{
  "id": "ireland",
  "title": "Ireland",
  "lang": "en",
  "source_lang": "en",
  "summary": "Ireland is an island in the North Atlantic off northwest Europe, known for its mild oceanic climate, low central plains ringed by coastal mountains, and division into two jurisdictions.",
  "category": "geography",
  "subcategory": "",
  "type": "place",
  "aliases": [
    "Éire",
    "Emerald Isle",
    "Island of Ireland"
  ],
  "generated_at": "2026-10-09",
  "model": "pro/claude-haiku-5-5",
  "url": "https://aiwiki.page/en/ireland/",
  "translations": {
    "zh-Hans": {
      "url": "https://aiwiki.page/zh/ireland/",
      "json": "https://aiwiki.page/zh/ireland.json"
    }
  },
  "sections": [
    {
      "heading": "",
      "text": "Ireland is an island in the North Atlantic Ocean, lying west of Great Britain and northwest of the European mainland, and it forms part of the British Isles. The island is divided between the Republic of Ireland, which covers most of its area, and Northern Ireland, which is part of the United Kingdom. Its physical geography is simple in outline but varied in detail: a broad interior of low plains and lakes, mostly underlain by limestone and covered in glacial deposits and peat, is surrounded by a ring of older upland and coastal mountains. Its rivers, most notably the Shannon, drain the centre of the island to the Atlantic, while its mild, wet climate, shaped by the Atlantic Ocean and prevailing westerly winds, supports lush vegetation and extensive pastoral farming.\n\nGeography explains much of Ireland's history, economy and environment. Its position on the Atlantic margin of Europe gives it a temperate oceanic climate that is milder than other places at similar latitudes, which in turn shapes land use, water availability and vulnerability to storms and flooding. Its bedrock and glacial history determine where bogs, lakes and fertile soils occur, and the country's mineral and energy resources, from peat to natural gas and wind, are tied to its landforms and coastline. The island's population, now more than five million in the Republic alone, is concentrated in and around Dublin and along the eastern seaboard, making settlement patterns another central theme.\n\nThis entry proceeds from the island's location and physical framework, through its geological origins, landforms, drainage, bogs and coasts, to its climate and weather hazards. It then covers soils, mineral resources, vegetation and ecosystems, population and settlement, land use and agriculture, and energy and water use. It closes with environmental pressures, the history of geographical knowledge about the island, and its regional context."
    },
    {
      "heading": "Location and political divisions",
      "text": "Ireland is an island in northwestern Europe, on the eastern edge of the North Atlantic Ocean. Its western coasts face open ocean, while the Irish Sea separates it from Great Britain to the east. To the south, the Celtic Sea opens onto the continental shelf that links the island to mainland Europe. The eastern neighbour is reached through St George's Channel in the southeast, the Irish Sea in the east and the North Channel in the northeast. The island's centre lies at approximately 53°N, 8°W, near the western margin of the European continental shelf, on the Eurasian Plate. Within the geographical grouping of the British Isles, Ireland is the second-largest island after Great Britain, lying to its west.\n\nThe island is divided between two jurisdictions. The Republic of Ireland is an independent sovereign state that occupies about five-sixths of the island, while Northern Ireland is a constituent country of the United Kingdom occupying the north-eastern remainder. This division is a matter of established administration and law: each jurisdiction has its own government, and each publishes its own official statistics. The Central Statistics Office in Ireland reports on the 26 counties of the Republic, and the Northern Ireland Statistics and Research Agency reports on the six counties within Northern Ireland. The boundary is therefore described here as a fact of governance and not as a subject of contention.\n\nArea figures\n\nThe whole island covers about 84,421 km², which is roughly 32,595 square miles. The Republic accounts for about 70,273 km², and Northern Ireland for about 14,130 km². On these figures the Republic holds roughly 83 per cent of the island and Northern Ireland roughly 17 per cent. Older reference works give slightly different values, such as 84,431 km² for the whole island and 14,148 km² for Northern Ireland. These variations stem from different measurement methods and dates, and the figures are close enough that they do not alter the overall picture.\n\nPopulation figures\n\nPopulation totals for the two jurisdictions come from different agencies and different reference dates, and this must be taken into account when comparing them. The Central Statistics Office's April 2026 estimate for the Republic is 5,525,600 usually resident persons, an increase of 66,900 over twelve months. A compilation with an earlier reference date gives 5,458,600 for April 2025, while the 2022 census recorded 5,149,139. The census is a count at a specific moment, whereas the Office's figures are estimates for a reference date. The difference between the April 2025 and April 2026 figures reflects growth over the intervening year, not conflicting data.\n\nFor Northern Ireland, the Northern Ireland Statistics and Research Agency estimated the population at 1.93 million on 30 June 2025. Growth between mid-2024 and mid-2025 was only around 600 people, the second consecutive year of slowing growth. The mid-2024 figure was 1,927,900. Adding the two most recent estimates gives a combined population of roughly 7.5 million, but this sum mixes an April estimate with a June estimate. Older encyclopaedic compilations list a figure of about 7.19 million for 2023, which predates the newest releases.\n\nWhen reading these numbers, three points are useful. First, the reference date (April, June or census day) must be matched before comparing totals. Second, \"usually resident\" definitions are used in the official estimates, which may differ from other measures of who is present. Third, rounding and revisions can shift published figures. Using the Office's and the agency's own tables, the Republic's population density is about 79 people per km², and Northern Ireland's is about 137 people per km², calculated from the figures above."
    },
    {
      "heading": "Area, boundaries and coastline",
      "text": "Measured as a whole, the island of Ireland has a total area of about 84,421 km², and land makes up 98.2% of that figure, with water at 1.8%. Official sources usually define total area as the sum of land and water inside international boundaries and coastlines, and land area as everything except inland water bodies such as lakes, reservoirs and rivers (total area = all land and water areas delimited by boundaries; land area excludes inland water; water area = inland water bodies such as lakes, reservoirs or rivers). Because inland water is counted within the boundary but ocean water is not, the figures for the sea-bounded island and its jurisdictions do not map neatly onto one another.\n\nThe division between jurisdictions shapes most of the published numbers. The Republic of Ireland's figures are commonly given as 70,273 km² total area, made up of 68,883 km² of land and 1,390 km² of inland water, which makes inland water roughly 2% of the Republic's area. Northern Ireland's six counties cover around 14,130 km², and the sum of the two is consistent with the island-wide total of roughly 84,400 km². Some compilations differ slightly; one reference gives 70,280 km² for the Republic, and another puts Northern Ireland at about 14,136 km². These differences reflect rounding, the year of the data and the measurement method rather than a disagreement about the boundary itself. The island is the third largest in Europe, after Great Britain and Iceland making it the third-largest island in Europe after Great Britain and Iceland.\n\nCoastline length is among the most variable figures in Irish geography. The CIA World Factbook gives a length of 1448 km for the Republic's coast, while the Ordnance Survey of Ireland reports a value of 3,171 km, and a World Resources Institute figure derived from older defence mapping data gives 6,347km. The gap arises because the island's bays, inlets, headlands and offshore islands are highly irregular. Measured with a divider of fixed length, the total grows as the divider shrinks: one analysis of the same map showed roughly 3,175 km at a 1 km step, 5,392 km at 100 metres and 15,550 km at 1 metre the value of 3,171 km given by the Ordnance Survey of Ireland corresponds to a step size of 1km. In other words, a shorter measuring unit follows more of the indentations, and no single figure is the \"true\" length. The western seaboard contributes most of this complexity: the western coastline is rugged, with many islands, peninsulas, headlands and bays, while the southern and northern coasts have a smaller number of substantial sea inlets. Of the island's counties, seventeen counties have an ocean/sea coastline: nine with a coastline on the Atlantic Ocean, seven with an Irish sea coastline and three with a coastline on the Celtic Sea.\n\nThe island measures roughly 480 km (300 mi) north-south, and 275 km (171 mi) east-west, though some sources give a north-south length of 486 kilometres long and 275 kilometres wide, depending on how the extreme points are defined. Its greatest breadth is found between two headlands: from Dundrum Head, Co. Down, to Annagh Head, Co. Mayo, a distance of 167km/104 miles. Because the island is compact, no part of the land is more than around 110 km (68 mi) from the sea.\n\nThe island's outer limits are defined by water on three sides. The Atlantic Ocean bounds the north and west, and the island is surrounded on all sides by the Atlantic and two of its local seas, the Celtic Sea off the island's south coast and the Irish Sea off its east coast. The Irish Sea lies between Britain and Ireland, while the Celtic Sea essentially the Western forecourt of the English Channel, separating Ireland from Brittany (Bretagne). The land boundary runs between the Republic and Northern Ireland, the only land border on the island; its course is treated in the political divisions section.\n\nThe island's extremes are at opposite ends of the relief scale. The highest point is Carrauntoohil, which is the highest mountain in Ireland at 1,038.6 metres (3,407 feet 6 inches). It is on the Iveragh Peninsula in County Kerry, close to the centre of Ireland's highest mountain range, MacGillycuddy's Reeks, and is the central peak of the MacGillycuddy's Reeks range, and has three major ridges. The lowest point is North Slob, which lies −3 metres (−10 ft) below sea level. It is an area of mudflats situated at the estuary of River Slaney at the Wexford Harbour in Ireland. The land was reclaimed in the 19th century when a sea wall was built and has an area of 1,000 hectares, and North Slob is the lowest point both in Ireland and in the British Isles."
    },
    {
      "heading": "Geological foundations",
      "text": "Ireland's bedrock records roughly 1.7 billion years of history. Dating places the oldest rock on Inishtrahull, a small uninhabited island off the Donegal coast, at about 1.7 billion years old, though some summaries round the figure to 1.8 billion. The oldest rocks in Ireland are 1.7 billion years old and are found on the island of Inishtrahull, Co. Donegal. The rock is about 1.8 billion years old in some accounts and is found on Inishtrahull Island off the north coast of Ulster. Its gneiss belongs to an ancient band that is part of the same ancient Rhinns complex exposed on Islay and Colonsay in Scotland, which suggests that this part of Donegal was once attached to a different landmass. Early rocks in Donegal also include deposits of glacial origin, so part of the future island was in the grip of an ice age at that time, although later upheavals make it almost impossible to sequence these early rock layers correctly.\n\nThe island's structural grain comes mainly from the Iapetus Ocean, which opened during the Cambrian and separated two continents, Laurentia and Gondwana. Its disappearance was a slow process of plate tectonic convergence. Subduction and continental collision closed the ocean and produced a mountain belt known as the Caledonide chain. The convergence took a long time: these two parts moved towards each other, eventually uniting about 440 million years ago. Final closure came later, as it was not until latest Silurian time that the Iapetus Ocean finally closed. The collision built mountains in the northwest and left granite bodies in places such as Donegal and Wicklow. Northern Ireland straddles three of the seven suspect terranes that together constitute the Caledonian Orogen in Ireland. Much of the assembly of these crustal blocks happened through large sinistral strike-slip movement on the terrane-bounding faults and along internal faults. The resulting suture line is visible in the landscape: in Ireland, this suture runs from the estuary of the River Shannon on the Atlantic coast, across the Irish Sea. The northwest-southeast alignment of these older blocks and faults is the main reason the island's rock units tend to run in parallel bands.\n\nThe most widespread younger bedrock is karst-forming Carboniferous limestone. During the Carboniferous Period (360 to 325 million years ago) much of Ireland was covered by a warm, tropical sea, the source of the widespread limestone which underlies much of the Central Plain. Almost a half of the Republic of Ireland is underlain by Carboniferous limestone, most of which is sufficiently pure to be karstified. Ireland possesses the largest continuous area of limestone in north-western Europe, covering approximately 30,000 km², and three-quarters of this limestone lies in a lowland central plain, which rarely rises above 100 m in elevation. Where the limestone is exposed, it develops underground drainage, and the exposure of limestone pavement, with its characteristic fissures known as 'clints' and 'grikes'. The Burren in County Clare is the best-known example of this landscape. Lowland limestone also produces turloughs, or transient lakes, which appear and disappear with the rise and fall of the water-table. Because the limestone is so widespread and porous, the lowland limestones are the principal source of groundwater in Ireland.\n\nGlaciation reshaped much of this bedrock. In most places the limestones are overlain by materials deposited during or after the last glaciation. That cover is why karst landscapes are limited in extent today, since the Carboniferous bedrock is usually overlain by glacial drift. Earlier in the Quaternary, when the land surface was exposed for longer, karstic conditions may then have been much more widespread, producing underground drainage and in places leading to the collapse of the overlying limestone. In the uplands, ice sheets and mountain glaciers carved cirques, steep hollows and sharp ridges, and the Macgillycuddy's Reeks in County Kerry show this sculpted form. Across several eastern counties, glacial till and related deposits blanket older rock, and the same ice produced the surface features of the lowlands. The last ice age left drumlins and glacial valleys across the country, and these landforms remain visible in the modern landscape."
    },
    {
      "heading": "Landform pattern: coastal mountains and central plain",
      "text": "Ireland's relief follows a simple overall pattern: a low interior basin surrounded by higher ground that rises toward the sea. The central lowland is built largely on limestone. Its average elevation is roughly 75 metres, and it is broken up by numerous lakes, bogs and low ridges. That lowland is encircled by coastal uplands whose rocks differ from one sector to another, so the rim is a patchwork of mountain groups rather than a uniform wall. Because no part of the land lies more than about 110 km from the sea, the upland rim is never far from the coast.\n\nSouthwest and west\n\nThe most dramatic relief is in the southwest. The MacGillycuddy's Reeks, on the Iveragh Peninsula in County Kerry, are mainly composed of old red sandstone. The range contains Carrauntoohil, the island's highest summit at about 1,040 metres (published figures range from 1,038 to 1,041 m), along with Beenkeragh and Caher, which also exceed 1,000 metres. Glaciation carved the range's steep corries, deep gullies and sharp ridges, which is why its peaks look so austere. The mountains in the west and southwest are similarly rugged, with ridges that drop abruptly into the Atlantic. The coast here is deeply indented: mountain spurs end in bold headlands and rocky islands, and the valleys between them have been flooded by the sea to form long, narrow inlets.\n\nNorth\n\nThe northern highlands are more varied in rock type. The Donegal Mountains are built of quartzite and form rugged peaks, and much of the interior of County Donegal consists of mountains, irregular highland groups, and extensive bog and moorland. Further east, the Antrim Plateau is a flat-topped expanse of basaltic lava. Its hard rock resists weathering, so the plateau's north and east cliffs fall almost directly into the sea.\n\nSouth and midlands\n\nThe south is distinguished by a series of east–west ridges and intervening valleys. Ancient sandstone and shale layers have been folded and eroded, leaving flat-topped mountains with steep scree slopes that are often capped by wind-swept bogs. Some ranges, such as the Galtee Mountains and Slieve Bloom, rise abruptly from the surrounding plains. Rivers such as the Suir, Lee and Blackwater flow through these valleys and cut through the ridges in narrow, gorge-like channels. In the north midlands, the relief is gentler: low, rounded foothills rise above patches of bog and wet, rushy ground.\n\nEast\n\nOn the east side, the Wicklow Mountains are formed from granite. Their rounded, peat-covered summits, such as Lugnaquilla at about 925 metres, have been sculpted by glacial cirques and penetrated by deep valleys, the best known being Glendalough. Between the Wicklow uplands and the Carlingford peninsula, the lowland opens to the Irish Sea over a stretch of about 90 km, which gives the east a comparatively easy approach from the sea.\n\nContrast between west and east\n\nThe overall contrast is between a rugged, remote western half and a more accessible, lower-lying eastern half. The west has high relief, indented coasts and sparse settlement, while the east has broader lowlands and a more uniform coastline with fewer natural harbours. This division shapes patterns of settlement and transport, with the more populous and accessible areas concentrated in the east."
    },
    {
      "heading": "Rivers, drainage basins and lakes",
      "text": "The Shannon and its basin\n\nThe River Shannon is Ireland's longest river. Its headwaters lie in County Cavan, at a small pool called the Shannon Pot on the slopes of Cuilcagh Mountain. The official Ordnance Survey Ireland length from the Shannon Pot is 360 km, made up of 102.2 km of tidal water and 258.3 km of freshwater. Other figures circulate because the measured length depends on the chosen source. One set of calculations shows that using a different headwater, the Boyle River, adds more than 30 km to the total making the Boyle-Shannon river the longest natural stream flow (source to sea) in Ireland. Older general references give shorter values, such as about 161 miles (259 km).\n\nThe river flows generally south and then turns west, reaching the Atlantic through the Shannon Estuary below Limerick. Limerick City stands where fresh river water meets the estuary's seawater. The river also acts as a provincial boundary: it forms the divide between Connacht to the west and Munster and Leinster to the south and east. Its tributaries include the Inny, Suck, Brosna, Fergus and Maigue.\n\nThe Shannon basin covers roughly a fifth of the island. One reference puts its area at 16,900 km2 (6,525 sq mi), approximately one fifth of the area of Ireland. Other calculations separate the main basin, with an area of 11,700 km2, from a total that includes the estuary and the River Feale, which gives 16,865 km2 (6,512 sq mi). In its course through the central lowlands, the river is surrounded by marshes and bogs for much of its course and widens at various points into lakes, many with islands. Its flow is substantial: its long-term average at Limerick is 208.1 m3/s (7,350 cu ft/s), which is double the flow rate of Ireland's second largest river, the River Corrib.\n\nCombined with the second-largest river system, the Shannon matters greatly for national hydrology. The Shannon and the Barrow-Nore-Suir river systems together drain over one third of the area of the country.\n\nOther major rivers\n\nThe Shannon is followed by the Barrow, Nore and Suir system, which is the second-largest. Among single rivers, the River Blackwater (Munster) flows through Kerry, Cork and Waterford, with a length of 168 km and a basin area of 3,324 km². The Liffey and the Lee are shorter, but they are important urban rivers that pass through Dublin and Cork respectively.\n\nThe northern drainage and Lough Neagh\n\nThe rivers of Northern Ireland largely drain into Lough Neagh, the largest lake on the island of Ireland and in the British Isles. The lake has a surface area that sources give as between about 383 and 392 km², and its average depth is 30 ft (9.1 m). Its primary inflows include the Upper Bann, Blackwater, Moyola, Ballinderry and River Main, while its single primary outflow is the Lower Bann. The Lower Bann flows from Lough Neagh for 60 km (35 miles), to the Barmouth between Castlerock and Portstewart, where it discharges into the sea. Lough Neagh's catchment area is 4,550 km², and it lies 91% in Northern Ireland and 9% in the Republic of Ireland. Its water is important for supply: it supplies 40.7% of Northern Ireland's drinking water.\n\nLakes and total water in the Republic\n\nWithin the Republic, Lough Corrib is the largest lake and contains around 800 billion litres of water. Lough Corrib is ranked second by area on the island, after Lough Neagh. In the Republic, the estimated lake count depends on the survey. According to the Environmental Protection Agency, there are an estimated 12,000 lakes in the Republic of Ireland, covering an area of more than 1,200 square kilometres. An older lake database instead reports over 4,000 lakes and ponds and their combined total area is approximately 2 per cent of the total country area. The difference reflects the criteria used. The EPA's monitoring focuses on lakes over 50 hectares and on those used for drinking water.\n\nLakes and reservoirs are also a major source of drinking water, the main sources of drinking water for two million people in Ireland. Estimates for the length of the river network are likewise uneven. One national figure is over 70,000 km of waterways in the Republic of Ireland contained in 3,192 river water bodies including rivers, streams, and tributaries. The EEA's surface water summary counts more than 13,000 km of major river channels and tributaries, so comparisons depend on which features are included."
    },
    {
      "heading": "Peatlands and bogs",
      "text": "Ireland's midland raised bogs took shape roughly 10,000 years ago, when the last glacial ice withdrew and left depressions in the central lowlands. Vast quantities of meltwater drained from the ice sheets and was trapped within these depressions, forming thousands of lakes across Ireland. The lakes did not stay open water for long. Over centuries and millennia, floating mats of vegetation spread toward the centre of these basins, eventually covering the water entirely. Plant matter that sank into the lake water did not fully break down, because the water was low in oxygen. Gradually, undecomposed plant material built up to form a layer of peat below the water level.\n\nAs the peat deepened, the lake surfaces were gradually filled in. The peat layers thickened and expanded, and the lakes contracted until a raised bog developed above the water level. This transition also changed the water supply. As the lake filled with peat, access to the nutrient rich groundwater was cut off. This meant that the only water supply came from the acidic and nutrient poor rainwater. The bog's surface then rose into a gentle dome, which is why the landform is called a raised bog. The name raised bog is derived from the elevated surface that develops as raised bogs grow upwards creating a slight dome-shaped surface above that of their immediate surrounding.\n\nThe central lowlands are suited to this development because their surface drains poorly. The landscape left by glacial deposits is uneven and hummocky, so water collects in the hollows. Over the centuries, poor drainage and the build up of dead plants created layer upon layer of peat. Thickness varies from place to place. One educational source gives an average depth of about 8 metres for the midland bogs of County Offaly, which are flat and deep, and these bogs provide a large-scale, commercial peat industry for the surrounding areas.\n\nPeat has been cut for fuel in Ireland for centuries. Rural households have long exercised turbary, the right to cut turf for domestic use. Since the 15th century traditional turbary has been responsible for the loss of 470,247ha of raised and blanket bogs or 40% of the original peatland area in the Republic of Ireland. Commercial extraction expanded sharply in the twentieth century. Bord na Móna, the state owned peat production company, was set-up in 1946 and in a relatively short period of time has been responsible for the development of 80,000ha of both raised and blanket bog. Taken together, hand cutting, mechanised turf cutting and industrial extraction account for a staggering loss of 47% of the original area of peatlands in Ireland. Peat-fired power generation has since been largely phased out, but peat still supplies domestic fuel and remains part of the rural economy and landscape.\n\nThe bogs are ecologically significant. The wettest, least-damaged part of a raised bog is the active bog, which keeps forming peat. There is a high proportion of cover by bog mosses or Sphagnum spp. Some typical features of active raised bogs occur here, including hummocks, pools, wet flats, Sphagnum lawns, flushes and/or soaks. Blanket bog is also valuable. Its pools support specialised mosses and plants and provide essential feeding habitats for wetland birds. Blanket bog is a globally restricted peatland habitat confined to cool, wet, typically oceanic climates. Ireland's share is significant. Ireland has 50% of the remaining blanket bogs of conservation importance within the Atlantic Biogeographic Region of Europe. Active blanket bog is also listed as a priority habitat under the EU Habitats Directive. Because of the relatively scarcity of the habitat in a European context, active blanket bog has been listed as a \"priority\" habitat for conservation in Annex 1 of the Habitats Directive.\n\nThese habitats are highly sensitive to change. Peatland habitats are particularly sensitive to hydrological changes brought about by drainage for agricultural improvement, forestry and peat extraction. Burning and overgrazing add further pressure. Of the original raised bog in the Republic, 64% have been lost to turbary, 24% to mechanical extraction and 2% to forestry, leaving 10% intact and worthy of conservation. For blanket bog, only 28% (216,599ha) of the blanket peatland resource remains in a relatively intact condition in the Republic of Ireland. The most recent national assessment under the Habitats Directive rated blanket bog as bad with a deteriorating trend. In the 2025 report, both Active and Inactive Blanket Bog were classified as one habitat, with the Status of Blanket Bogs being deemed as BAD, with a deteriorating Trend.\n\nFigures for the original extent of bog differ between sources. For the Republic, one source gives about 308,742 ha of raised bog and 774,367 ha of blanket bog, while a broader island-wide estimate for blanket bog reaches 908,117 ha. The differences reflect the boundaries and survey methods used, so the figures should be compared with care. Restoration is now part of management, and many degraded blanket peatlands have undergone restoration measures since the turn of the century."
    },
    {
      "heading": "Coasts and nearshore seas",
      "text": "Western seaboard\n\nThe island's coastline is roughly 7,400 km long, and about 3,000 km of it is dominated by bedrock, mainly along the southwestern, western and northern shores. Along the Atlantic side, high sea cliffs and long headlands alternate with deep indentations. The Cliffs of Moher in County Clare are a typical case: their highest point rises about 214 m above the sea, and they extend for roughly 14 km. Because the bedrock is hard and poorly erodible, these cliffs keep their profile despite constant exposure to open-ocean waves. Large bays and estuaries, including the Shannon estuary and the Donegal, Clew, Tralee and Dingle bays, interrupt the rocky shore. Their soft, sedimentary floors contrast sharply with the adjacent headlands, and they are also among the places where sediment accumulates. Small islands lie off the same coast and face the full force of the swell.\n\nEastern shore\n\nThe east and southeast coasts are lower and largely composed of unconsolidated sediments deposited during the Quaternary period, with few rock exposures. Sandy beaches and marine gravel shores predominate, and these are highly erodible. Waves here are smaller than on the Atlantic side, typically between about 0.5 m and 2 m high. Much of their energy comes from local winds rather than from distant swell, because the Irish Sea is sheltered from the open ocean. This difference in wave climate explains why the west retains hard headlands while the east supports long strands and dune systems that can be quickly reshaped.\n\nWave exposure and sediment movement\n\nAtlantic swell, generated by distant North Atlantic storms, can break at heights of up to about 3 m along the west coast. Eastward-moving cyclones bring much of their energy to this seaboard, so exposure is greatest there. In the Irish Sea, however, tidal currents rather than waves are the dominant force that disturbs the seabed. Wave-induced stress mainly affects nearshore areas within about 10 km of the western Irish Sea coast and about 20 km of the eastern coast. Offshore sandbanks such as Kish and Codling act as sediment reservoirs. Sand moves from these banks toward the east coast, and soft sediment is replenished from deeper banks in the Celtic Sea, so that a tide-driven transport chain runs into and along the shoreline. Interference with this supply appears in the coastal record: sand has been noted to decline on the beaches at Bettystown and Portrane, north of Dublin, where it seems to have been deposited further north. Overall, about 20% of the coast is considered at risk of erosion, and average erosion rates on soft coasts are around 0.2–0.5 m per year, rising locally to 1–2 m per year. The predicted shift in North Atlantic storminess under climate warming is expected to affect coastal wetlands and soft sedimentary systems early, through storm-driven sea-level rise.\n\nMarine resources and aquaculture\n\nCoastal waters support fishing and aquaculture. Fish and shellfish are farmed in 14 coastal counties. A Bord Iascaigh Mhara report counted 278 aquaculture production units in 2019, which together produced about 38,000 tonnes of finfish and shellfish valued at €172 million. Mussels, oysters and salmon are the main farmed species. Open-net salmon farms are concentrated along the Atlantic coast from West Cork to Donegal, and the north region around Donegal generated the largest regional revenue in a later BIM assessment. An industry figure cited by the Irish Farmers' Association attributes around 1,833 direct jobs to aquaculture in remote rural areas, about 80% of them in the west, although this is based on older data. The industry's expansion is contested. Research has linked sea lice from open-net farms to declines in wild Atlantic salmon, and one 2025 study reports that wild salmon numbers fell by more than half between the early 1980s and 2023, before any fishing took place. Shellfish and other species introduced through aquaculture gear and stock have also been identified as a route for non-native species. Integrated multi-trophic systems, which grow seaweed and shellfish beside fish pens to take up waste nutrients, are being tested as a way to reduce the pollution and ecological pressure associated with finfish farming."
    },
    {
      "heading": "Climate type and its causes",
      "text": "Ireland's climate is classified as temperate oceanic, designated Cfb in the Köppen system, a category it shares with most of northwest Europe. In the Köppen scheme, this class requires the coldest month to average above 0 °C, the warmest month to stay below 22 °C, at least four months to average above 10 °C, and precipitation to exceed evaporation in every month. In practice, this produces a climate that is mild, humid and changeable, with plentiful rain and few temperature extremes. Frost and snow are infrequent in the lowlands, though not unknown.\n\nOcean heat and the atmospheric circulation\n\nThe main reason for this profile is the ocean that surrounds the island. The Atlantic Meridional Overturning Circulation (AMOC), a large system of currents that includes the North Atlantic Current and the Gulf Stream, moves warm water northward across the ocean. As that water cools, it releases heat into the air above the Atlantic. Prevailing winds from the southwest and west then carry this heat over Ireland. The effect is strongest in winter, when the warm ocean contrasts most sharply with the colder continental interior. For this reason, Dublin has a noticeably milder winter than other temperate oceanic locations at similar latitudes, and the island is often compared with places such as Newfoundland and Sakhalin, which lie at comparable latitudes but experience much harsher winters.\n\nThe same ocean moderates summers in a different way. Because the sea is slow to change temperature, it keeps the air cool in spring and holds it back in summer. Met Éireann notes that the sea near Ireland is at its coldest in February and March, which is why the rise in mean air temperature is gradual in spring, even though clear, calm afternoons in March can feel like summer. Summers are therefore mild rather than hot. The position of the storm track also matters: in summer, Atlantic depressions travel farther north and are generally less intense, while in winter they pass closer to the island and bring cool, windy weather.\n\nTemperature range and national averages\n\nThe annual temperature range is small. Mean daily temperatures in January and February generally fall between 4 and 7 °C, while July and August are typically between 14 and 16 °C. This gives a seasonal swing of roughly ten degrees Celsius, which is modest for a country at this latitude. Daily ranges are also narrow, so both sustained summer heat and hard winter frost are uncommon. The national average annual temperature is around 10 °C. Among the stations used in official climatologies, Valentia Island in County Kerry has one of the highest mean values, at about 10.9 °C, while the inland town of Mullingar in County Westmeath has one of the lowest, at about 9.3 °C.\n\nCoastal, inland and upland contrasts\n\nThe maritime effect weakens with distance from the sea. Its influence is strongest along the Atlantic coasts and fades progressively inland, so interior locations experience colder winters and warmer summers than coastal stations. Summer maximum temperatures near the coast are often around 17 to 18 °C, whereas inland they can reach 19 to 20 °C. The warmest districts tend to lie along the southwest coast, where the ocean exerts its greatest influence, and the coldest are found in the interior midlands.\n\nElevation adds another layer of variation. Higher ground is cooler and wetter, and the mountains that ring the island shelter lower land from the strongest winds while intercepting moist air from the west. Some upland areas that are too cold to meet the criteria for Cfb are classified as oceanic subpolar (Cfc), a category with cooler summers, typically fewer than four months averaging at least 10 °C, and relatively mild winters. The sensitivity of these patterns to the Atlantic is also a concern for future projections, since changes in the AMOC could alter the heat supply on which the present climate depends, a point taken up under climate change impacts."
    },
    {
      "heading": "Weather hazards and climate change impacts",
      "text": "Storms, floods and thunderstorms\n\nIreland sits in the path of Atlantic depressions, so its weather arrives in sequences of frontal systems. In 2025, five named storms directly affected Ireland, and during storm Éowyn two stations reached hurricane force 12 on the Beaufort wind scale. The 2023–24 season was more severe: the countries were affected by 13-14 severe storms, 11 of which were named by the Western Europe Storm Naming group, and storms Babet, Ciarán, Henk and Isha led to severe floods, severe damages to homes and infrastructure, power outages, travel cancellations, loss of crops and livestock.\n\nFlooding is often compounded by the sea. A Marine Institute oceanographer described a November flood in Galway in which a storm surge added roughly 1.6 metres to the expected tide. Thunderstorms are more localised but can be just as disruptive. Met Éireann warnings for them list surface water flooding, lightning damage and difficult travelling conditions, and intense downpours can flood roads and low-lying land quickly, with little warning. Occasional deep Atlantic lows bring the strongest winds, while thunderstorms tend to form in warm, humid spells when the air holds more energy.\n\nRainfall patterns\n\nRainfall is abundant and varies strongly with terrain. Average annual totals range from roughly 750 mm (30 in) in the eastern part of the country to over 2500 mm (100 in) in the western highlands. The west and high ground receive the most rain, and totals fall toward the northeast. Rain is also unevenly spread through the year: rainfall accumulation tends to be highest in winter and lowest in early summer, and April is generally the driest month. This regular, widespread wetting, together with the mild temperatures, underpins the island's green landscape and its grassland farming.\n\nProjected change\n\nNational and intergovernmental assessments point to a warmer, more variable climate. For Ireland, by 2050 (mid-century) mean annual temperatures are projected to increase by between 1 and 1.2℃, and between 1.3 and 1.6℃ depending on the emissions trajectory. The changes in rainfall are seasonal: significant decreases are projected for spring and summer and increases for winter. Extreme rainfall is also likely to become more frequent. The result is a double risk, since by mid-century there are projected increases in both dry periods and heavy precipitation events, so flood risk and drought frequency both rise. Storm behaviour may also shift. Average wind speeds may fall while the intensity of individual storms may increase. Warmer seas add moisture to the atmosphere, and Met Éireann notes that climate change is adding fuel to storms due to warmer ocean temperatures and more moisture in the atmosphere. A rapid attribution study by the World Weather Attribution group estimated that climate change has also increased the amount of rainfall of these storms, making them about 20% more intense.\n\nThe national assessment draws on the IPCC's global projections, and the EPA's Climate Ireland resources cite both the IPCC's 2021 report and Ireland's 2024 climate change assessment as sources for these figures.\n\nSea-level rise, coastal erosion and flood risk\n\nSea level is the most persistent long-term threat. Global mean sea level by 2100 is likely to be in the range of 0.29m to 1.10m (depending on the emissions scenario) and sea levels will continue to rise far beyond the year 2100. Around Ireland, satellite observations indicate that sea level around Ireland has risen by approximately 2-3mm per year since the early 1990s. Rates in Cork and Dublin appear to exceed the global average, although the reasons are still under investigation. Land movement complicates the local picture: glacial isostatic adjustment has left the north of the island rising relative to the sea, while parts of the south are sinking, so relative sea-level change differs from place to place.\n\nProjected additional rises by 2100 range from 0.32–0.6m under Early action to 0.63– 1.01m under Late action scenarios, with high uncertainty for the latter case whereby 2m rise could occur owing to highly uncertain ice sheet processes. Higher mean sea levels amplify the effect of changing storm surge and wave patterns in coastal areas. Exposure is high because most of Ireland's population and infrastructure are concentrated on the coast and in the coastal cities of Dublin, Cork, Limerick and Galway. The island's shores differ in their vulnerability. The Atlantic coast is dominated by high relief and rock cliffs interspersed with bays while the Irish sea coast is mainly low-lying. Flood risk is therefore concentrated on the lowlands, and currently, coastal flood risk is highest in low-lying areas along the east coast from Dundalk to Dublin and along the Wicklow to Wexford coast. Particularly at risk are soft sediment shorelines.\n\nVulnerable lowlands and peatlands\n\nThe eastern lowlands are doubly exposed: they receive the least rain, so they face more frequent drought, and they lie close to the sea, so they face rising water levels and surge flooding. Peatlands are sensitive to the same changes. Raised and blanket bogs depend on a high water table, so longer dry spells and lower summer rainfall can lower it, exposing peat to oxidation and releasing stored carbon. Heavier winter downpours, by contrast, can saturate bogs and overload the drainage of nearby farmland. Land-use change compounds the problem, since losses of natural grasses and woodlands can reduce soil drainage and increase the risk of flooding."
    },
    {
      "heading": "Soils and mineral resources",
      "text": "The soils of the central lowlands are closely tied to the rock beneath them and to the material glaciers left behind. The midlands sit on a broad plain of Carboniferous limestone that mostly lies below 150 metres above sea level. Where this limestone is covered by glacial drift, it produces calcium-rich soils. Ireland experienced at least two major glaciations, and each advance and retreat of the ice sheet reworked the surface, so the drift that forms the parent material of most Irish soils has a mixed origin and a complicated composition. Limestone-bearing drift tends to be fertile, whereas many older rock formations weather into thin, unproductive soils. Where drainage is poor, the same landscape gave rise to bogs and acidic, phosphate-poor soils, a topic treated in the peatlands section.\n\nThe limestone lowlands cover about 1.67 million hectares, almost a quarter of the national land area. Luvisols are the most common soil type within them, making up roughly 60 per cent, with brown earths, surface water gleys and small areas of humic rendzinas, the last mainly found in the Burren in County Clare. Under Irish rainfall, many of these soils have been leached of free carbonates, yet their base status and pH usually remain high. Because they are typically well drained, they support grass for grazing and can be used for tillage when managed carefully. Agricultural use of these soils is discussed in the land use section.\n\nIreland's mineral wealth is spread across several geological settings. The island has been divided into mineral provinces. Its Proterozoic and Lower Palaeozoic metasediments and metavolcanic rocks contain base-metal mineralisation, such as the copper at Avoca in County Wicklow, and gold-bearing quartz veins. The Carboniferous limestones of the central plain host a different family of deposits, known as \"Irish-type\" carbonate-hosted zinc–lead ores, which include Navan, Tynagh, Lisheen and Galmoy. Younger rocks contain industrial minerals, most notably the gypsum deposit near Knocknacran in County Monaghan, which lies in an outlier of Permian rocks. Metals recorded as mined or quarried in Ireland include copper, zinc, lead, silver, gold, iron and bauxite, along with antimony, barytes, cobalt, coal and salt.\n\nThe mining record is long. Bronze Age copper working in the southwest, at places such as Ross Island and Mount Gabriel, is documented, and alluvial gold was gathered from streams for ornaments. Iron works developed in the sixteenth and seventeenth centuries and expanded in the late eighteenth century as British industrialisation increased demand. A gold rush at the Gold Mines River in Wicklow between 1795 and 1830 yielded an estimated 7,000 to 9,000 ounces from alluvial gravels. Output of copper, lead and silver continued through much of the nineteenth century, but the industry contracted after metal prices fell from the 1860s, and depleted deposits and foreign competition kept activity low into the early twentieth century. From the 1960s, zinc and lead became the main focus. Two underground base-metal mines accounted for about 31 per cent of European zinc production and about 11 per cent of European lead in 2015, although sources differ on Ireland's ranking as a zinc producer in Europe.\n\nNon-metallic resources have been equally important for construction and industry. Gypsum is extracted in Counties Monaghan and Cavan for plasterboard. Irish Gypsum's operations near Knocknacran reported output of about 200,000 tonnes in 2019, and the company projected that its mine would reach depletion around 2030. Rock salt occurs at Kilroot in County Antrim. Limestone is quarried widely for construction and agriculture, while dolomite, silica sand, brick shale and fireclay have been mined in recent years, and marble has been quarried in County Galway. Exploration in the 2020s has also covered platinum-group metals, rare earths, lithium and other battery-related metals.\n\nExtraction is regulated in both jurisdictions. In the Republic, the Minerals Development Act 2017 governs exploration and mining and includes provisions on mine closure and on the social and environmental effects of mining. Operators must obtain planning permission and an environmental licence from the Environmental Protection Agency. Since 2006 a joint programme of the EPA and the Geological Survey of Ireland has inventoried historic mine sites and classified their risk, because many older workings were abandoned without remediation. Local controversies have accompanied several projects. In Monaghan, residents raised concerns about the handling of sulphate-laden water from a gypsum mine, and in Wicklow, proposed gold mining in the 2000s and later faced opposition over environmental impacts. Managing these legacies remains a central part of mineral policy."
    },
    {
      "heading": "Vegetation, forests and ecosystems",
      "text": "Ireland's potential natural vegetation is woodland. Most of the Irish landscape was covered by trees following the last glaciation, around 10,000 years ago. Woodland dominated the landscape from about 8,500 years ago. Early forests were mixed: oak woodland in the lowlands and valleys, and pine forests on poorer soils. Popular accounts put the postglacial cover at up to 80 per cent of the island, though the exact figure is uncertain.\n\nClearance and the historical loss of woodland\n\nClearance began with farming. Shifting cultivation by Neolithic farmers from about 6,000 years ago produced temporary clearings that regrew once land was abandoned. By the end of the Bronze Age, most hills had been cleared of woodland by burning and cultivation, and blanket bogs had replaced the woodland on the summits.\n\nFrom the sixteenth century, clearance accelerated for political, military and commercial reasons. Shipbuilding and other timber-based trades drew on Irish wood, and large areas of land were allocated to English, Welsh and Scottish landlords during the plantations. The English military also cleared woodland to deny cover to rebels (a claim made in secondary accounts). A roughly fourfold population increase between 1700 and 1840 drove further clearance for food and shelter. The Civil Survey of 1654–56 is central to estimates of the period: it has been calculated that between two and 12 per cent of Ireland was afforested at this time. Historians disagree about the chronology. One scholar argued that the decline must be calculated in thousands of years, and not in three or four hundred, which indicates how contested the timing remains.\n\nLand transfer in the late nineteenth and early twentieth centuries accelerated the loss further. The 1903 Land Act increased woodland clearance as land transfer sped up, and woodland cover fell to an all-time low of 1.5%, with the remaining areas of very poor quality. Other sources give a lower figure, of under 1 per cent, for the start of the twentieth century.\n\nCurrent forest cover and composition\n\nThe National Forest Inventory (NFI) is the main official reference. Its 2022 cycle estimated the total forest area at 808,848 hectares, representing 11.6% of the land area. Figures in other sources are lower because they use different definitions or earlier surveys. The NFI counts land as forest when it has a minimum area of 0.1 hectare, a width of at least 20 metres, trees taller than 5 metres and a canopy cover above 20 per cent. Broadleaf species account for nearly one-third (30.6%) of the stocked forest area, while conifers dominate at 69.4%. Over three quarters (77%) of Ireland's forests have two or more tree species present. The forests also store large amounts of carbon: the national forest estate is an important sink for carbon, at 323.0 million tonnes of carbon.\n\nGovernment policy aims to increase forest cover. Sources give different target dates, with one citing a target of 18% of the land area by 2027 and another describing 18% as the target by 2050.\n\nNative woodland\n\nThe area of native woodland is much smaller than total forest cover. Just under 2% is native woodland, of which only tiny fragments are original ancient forests (c. 20,000 hectares). An earlier survey based on the Forest Inventory Planning System found not more than 77,047 ha of native woodland in the state, about 1% of the land area. The NFI's broader native and mixed category reached 206,540 ha, but this figure includes mixed stands, in which 20-80% of trees are native species, so it is not directly comparable to the stricter estimates. The term \"native\" usually refers to broadleaved woodlands, comprised of native species that are not intensively managed. Ireland has 33 native tree species, and the surviving woodland is largely modified by human activity, even in the oldest stands.\n\nHabitats and ecosystems\n\nWoodland is only one part of the island's vegetation. Clearance and grazing favoured open ground, including heathland. In some areas of intensive agriculture, heath land developed such as the great Heath of Maryborough. Peatlands form another major ecosystem. Blanket bogs contain pools whose mosses (especially species of Sphagnum) and plants provide feeding habitat for wetland birds, and oligotrophic lakes within blanket bog areas provide habitat for the rare and declining Arctic charr. Modern forests, both plantation and native, support biodiversity as well: the NFI reports over 10.2 million cubic metres of deadwood, which is an important habitat component.\n\nConservation status of key habitats\n\nPeatlands are the most conservation-critical habitats. Raised bogs originally covered about 308,742 ha in the Republic of Ireland. Of that original area, 64% has been lost to peat cutting, 24% to mechanical extraction and 2% to forestry, leaving 10% relatively intact and worthy of conservation. Ireland holds a large share of the Atlantic region's raised bog resource, and active raised bog is a priority habitat under the EU Habitats Directive. The 2025 assessment rated raised bogs as BAD, with drainage, peat extraction, afforestation and climate change listed as main pressures.\n\nBlanket bogs have suffered a similar decline. Their original extent in the Republic was more than 774,367 ha, but a 2009 assessment found only 28% (216,599ha) of the blanket peatland resource remains in a relatively intact condition. The 2025 report classed blanket bog as BAD with a deteriorating trend, and it identified peat extraction, overgrazing and agricultural activities as the main threats.\n\nBoth bog types are protected under national and European law, and representative samples have been designated as Special Areas of Conservation (SACs) under the EU Habitats Directive or as Natural Heritage Areas (NHAs) under the Wildlife Acts. Designation does not by itself reverse loss, however, and the protected network covers only a portion of the remaining bog and woodland."
    },
    {
      "heading": "Population and settlement",
      "text": "The Central Statistics Office (CSO) reported a usually resident population of 5,525,600 for the Republic in its April 2026 release, and the total grew by 66,900 over the preceding twelve months. Ireland's estimated Usually Resident Population is 5,525,600. Immigrants numbered 110,600 in the year to April 2026, while emigrants were estimated at 62,500, so net migration accounts for roughly 48,000 of the growth. The rest comes from natural increase, which was nearly 19,000 people. Migration is therefore the larger driver, and the balance has shifted toward it as births decline. Since 2010, the number of births continued to decline, with 55,000 people under the age of one year living in Ireland, a decrease of 19,900 people or 27% in 16 years. Immigration itself fell by 12% compared with the previous year, and emigration fell for a second consecutive year.\n\nThe age structure is changing noticeably. There were 992,400 people aged 0 to 14 in April 2026, the first time this age bracket fell under 1 million since 2014. At the other end, the share of people aged 65 and over rose from 14.4% in 2020 to 16.1% of the total. Citizenship is also mixed: the number of non-Irish citizens is 931,000, or 16.8%.\n\nOfficial and United Nations figures\n\nDifferent sources give different totals for the same country, and the differences reflect method and reference date rather than error. The United Nations' World Population Prospects 2024 revision estimates Ireland's population as of 1 July each year, and for forecasted years, the U.N. medium-fertility variant is used. Its figure for 2026 is 5,356,950, about 170,000 below the CSO's April 2026 count. For 2024 the UN gives 5,255,017. Readers should therefore check three things: the reference date (April for the CSO, 1 July for the UN), the definition (usually resident population in the CSO's case), and whether a figure is an observed estimate or a projection. For the current size of the Republic, the national office is the more appropriate source. For cross-country comparison, the UN series offers consistent methods across states, but it is a modelled series and should not be treated as an exact count. The 2022 census, which reported a total population of 5,149,139, is the benchmark against which later national estimates are compared.\n\nNorthern Ireland and the island as a whole\n\nNorthern Ireland's population is measured separately by the Northern Ireland Statistics and Research Agency, which counts usual residents on 30 June. The population there was estimated at 1.93 million on 30 June 2025. Growth has slowed sharply: annual population growth was 0.03%, or 600 people, from mid-2024, compared with 0.4% in mid-2024 and 0.5% in mid-2023. Migration has become the main component of change there, and net migration has remained positive since mid-2022.\n\nCombining the two jurisdictions gives an island total of roughly 7.5 million, although the components refer to different dates and are produced by different agencies. The population of Northern Ireland was 1.93m in 2024, meaning there are now around 7.5m people on the island of Ireland. The figure should be read as an approximation.\n\nDublin and the settlement hierarchy\n\nPopulation is concentrated heavily in the east. The proportion of the population living in Dublin rose from 28.3% of the total in 2020 to 28.9% of the total in 2026, standing at 1,597,700 people in April 2026. Dublin is therefore the dominant centre of the state, and its share has been increasing. The 2022 census had already placed the county as the most populous in the country, with 1,458,154 residents at that time.\n\nBelow Dublin, the principal urban centres are Cork, Limerick, Galway and Waterford. Cork is the second-largest city, followed by Limerick, Galway and Waterford, which act as regional hubs for their surrounding areas. The UN estimates that 62.0 % of the population lived in urban areas in 2024, which reflects the weight of these centres as well as Dublin. For the detailed ranking of these cities and their growth, see urbanization and city.\n\nFor background on the population measures used here, see demography."
    },
    {
      "heading": "Land use and agriculture",
      "text": "Agriculture is the dominant human use of land in the Republic. Official land-cover statistics show that grassland accounted for 59% of total land use in Ireland in 2021, down from 62% in 1990. The CORINE mapping for 2018 gives a different split, with just under 56% grassland, while croplands covered 12%, against an EU average of 37% for cropland. The two series use different classifications, so their figures should not be read as interchangeable.\n\nRoughly 64%, or 4.5 million hectares, is suitable for agriculture out of about 7 million hectares of land. Grass occupies 61 to 63% of utilisable land, while around 9.5% is used for arable crops, mainly wheat, barley and oats.\n\nPasture and livestock\n\nThe mild, wet climate favours grass growth, which is why pasture and grazing dominate. Ruminant livestock farming systems account for 87% of the utilised agricultural area, according to the CSO's 2016 Farm Structures Survey. Organic production remains a small component, reaching 179,400 hectares, or 3.8% of the total, in 2023. Common grazing is also significant. The 2013 Census of Agriculture recorded 10.8% of agricultural land as commonage, meaning land with multiple owners who hold rights to graze it, and two thirds of commonages are located in the Border, Midland and Western region.\n\nLowlands, soils and crops\n\nArable farming is concentrated in the south-east, where the climate is drier and the soils are lighter. Crop production is predominantly concentrated in the southeast, where annual rainfall is between 660 and 1000 mm, compared with 1000 to 2800 mm elsewhere, and where soils are light to medium textured and free-draining. The dominant establishment method in this region is plough-based tillage. Over the past half-century, cropping has moved from mixed grassland and spring-sown crops toward specialised cereal monocultures or rotations made up entirely of annual crops.\n\nFree-draining soils carry a management cost. Most free-draining soils are affected to varying degrees by leaching, and therefore require a continuous renewal of nutrients and lime beyond the amounts removed. That renewal relies on fertiliser inputs, which in turn feed the nutrient enrichment of waters discussed elsewhere. Trace-element shortages are also common, with zinc deficiency a major problem in many cereal-growing areas, particularly on continuous tillage soils. Soil physical condition matters too: one Irish study found that compaction that reduced the soil's pore space by 12% led to about a 20% drop in barley yields. Teagasc land-suitability figures suggest that land capacity is not the limiting factor for tillage. Of the total suitable tillage land in the country, 41% occurs in Leinster, 36% in Munster, 18% in Connacht and 6% in Ulster. Yet on a national basis, only 13% of the land suitable for tillage is used for that purpose annually.\n\nUplands and marginal land\n\nThe contrast with the uplands is sharp. In the same Teagasc assessment, marginal land occupies some 49% of the land area, almost matching the share classed as agricultural land. On thin, wet or acidic soils in the west and on the mountain margins, farming is largely extensive, with sheep and cattle grazing rough pasture, often on commonage. Intensive crop production and dairy-based systems are concentrated on the lowlands.\n\nForestry and peat cutting\n\nForestry is the other major land use, and its importance has grown. Forestry accounted for 11.6% of Ireland's total land area in 2022, the third lowest among EU Member States after Malta and the Netherlands. The island was far more wooded in prehistory. Woodland cover was 80 per cent at the start of the Neolithic, but accelerating clearance for agriculture reduced it to less than one per cent by the end of the 16th century. Modern planting began early in the twentieth century with North American conifers on land unsuited to farming. From the 1980s, the EU began funding private landowners to plant more broadleaf species on better land. Most planting is now undertaken by farmers, whereas in the past it was undertaken by the State. Native species remain a minority; including hedgerows, motorway plantations and birch monocultures, less than 2 per cent of the State is covered in native trees. The state company Coillte manages about 440,000 ha of Ireland's forests, or 7 per cent of total land area, and its estate includes 232,500 hectares of peatland, making it the largest single owner of peatland in the country. Government plans to increase cover to 17 per cent by 2030.\n\nPeat cutting has a longer and more varied history. Hand-cut turf for household fuel was once common across the midland bogs and remains part of rural life. Commercial extraction on industrial bogs, led largely by Bord na Móna, has been scaled back in recent years, and attention has shifted toward rehabilitation. This change is partly driven by policy. Under the EU's Nature Restoration Regulation, Ireland must restore 20 per cent of habitats in need of restoration by 2030 and all habitats by 2050."
    },
    {
      "heading": "Energy and water resources",
      "text": "Energy sources\n\nIreland has little domestic fossil fuel, and as an island nation with no large fossil fuel reserves such as oil or coal, Ireland is highly dependent on imports. Gas is the largest single input to power generation. Almost half of electricity is generated from natural-gas-fuelled power stations, while about a third comes from indigenous sources such as wind, peat and hydro-electricity. Gas reaches the island by a subsea pipeline from Scotland, and the Corrib field off County Mayo supplies a growing share. Corrib is expected to account for up to 56% of gas needs at its peak.\n\nWind is now the main renewable source. In 2023, 40.7% of Ireland's electricity supply came from renewable energy, and just over a third (33.7%) of electricity came from wind. Most wind capacity is onshore, while offshore development has lagged; one recent assessment judges that the national target of 80% renewable electricity by 2030 will likely be missed. Solar photovoltaic capacity has grown quickly, but the country's heating sector remains the hardest to decarbonise, because heating remains heavily dependent on imported fossil fuels, particularly oil and natural gas.\n\nHydropower was the first renewable electricity source to be developed. The Ardnacrusha power station on the River Shannon, built in 1929, was a landmark in the country's electrification and remains operational today. Its contribution is small, and new large schemes face limits because of environmental constraints and the relatively flat topography of much of the country. Hydro's share of electricity is only a few per cent, so it functions mainly as a source of reliable, flexible power.\n\nThe peat transition\n\nPeat was once central to electricity supply. The oil crises of 1956 (Suez) and of 1973 were to cement the rationale for the development of peat-powered plants to diversify the Irish electricity system and avoid the risk of blackouts and rationing. Of the ten peat-burning plants built, six have closed, and the rest closed in turn as carbon pricing and climate policy made peat uneconomic. The West Offaly station was refused permission to continue burning peat for electricity and closed in December 2020. The last peat-fired plant, Edenderry, was to deliver 118MW of renewable electricity for the national grid after a €100m conversion to 100% biomass. The plant's peat use ended around the turn of 2023–2024, and Ireland is among the first EU member states to cease its use of an indigenous fossil fuel for climate action goals, rather than economic reasons. The shift has raised questions about biomass supply, since some fuel had to be sourced from abroad, even as far as Brazil.\n\nFreshwater resources\n\nPublic drinking water is drawn from several sources. Drinking water is sourced from rivers, lakes, springs and groundwater and must be treated to make it clean and safe to drink before it is supplied to consumers. Most public supply relies on surface water, with lakes and reservoirs playing a large role. Groundwater is stored in rock: when enough water is held in the pores or cracks in the rock, it is referred to as an aquifer. Estimates of groundwater's share vary by method. One national estimate gives between 20 and 25 per cent of drinking water, and the share is far higher locally, with the proportion much greater in certain midland counties. In rural areas, groundwater is usually the only source of supply for households outside public and group schemes.\n\nWater use is dominated by households, followed by industry and agriculture. An earlier European Environment Agency assessment reported that water is mostly consumed in households (431.5 mio m³/year), followed by industry (249.7 mio m³/year) and finally agriculture (129.6 mio m³/year). Demand is rising with population growth and per-capita consumption, and the projected changes in water availability pose potential problems for the dilution of waterborne effluent, particularly in dry years.\n\nManagement, quality and links to land use\n\nWater services are governed mainly by the Water Services Acts 2007 to 2014 and regulated by the Commission for Energy Regulation. Irish Water took over responsibility from 34 Local Authorities in 2015, although the change was phased in over several years. The EPA's 2025 report found that water from 99.8% of Ireland's public supplies complied with bacterial and chemical standards and was therefore safe to drink. Vulnerabilities remain at a number of plants: the EPA has identified 35 water treatment plants where supplies could be disrupted because of disinfection and other failures.\n\nPollution from agriculture and towns is the main pressure on water quality, and it is linked to land use through nutrient inputs such as fertiliser and manure. The national indicators show a mixed record. Nitrates in groundwater have shown significant improvement over time, but river quality has not kept pace: in the 2022-2024 period, 18% of rivers and streams were of bad or poor quality, compared with 25% between 1987-1990. Nutrient enrichment in rivers and lakes is discussed further under eutrophication."
    },
    {
      "heading": "Environmental pressures and management",
      "text": "Water pollution and nutrient leaching\n\nNutrient pollution is the most widely documented pressure on Ireland's freshwater and coastal systems. The Environmental Protection Agency (EPA) identifies farm runoff, poorly treated wastewater, and residues of fertiliser and pesticides as the main sources of excess nitrogen and phosphorus. Excess nutrients, particularly nitrogen and phosphorus, from farming, poorly treated wastewater discharge and chemicals from fertiliser and pesticides are the main culprits. Once these nutrients reach rivers, lakes and coastal waters, they promote algal overgrowth that consumes oxygen and degrades habitat for other organisms. Phosphorus is largely linked to sewage plants and surface runoff, while nitrogen leaching from intensive farming is a particular concern for groundwater and the estuaries that receive it.\n\nAgriculture is the largest single contributor. One estimate attributes about 85 per cent of nitrogen loadings in rural catchments to farming. Agriculture remains the main driver of nutrient pollution, accounting for 85 per cent of nitrogen loadings in rural catchments. The effects are spatially uneven. The 2025 assessment found that a large proportion of river sites (43 per cent) have elevated nitrogen levels, many of which are found in the south and east of the country. Phosphorus shows a different pattern: in the EPA's 2023 indicators, over one quarter (27 per cent) of rivers and one third (35 per cent) of lakes had levels that were too high, with lakes in the north and northeast most affected.\n\nThe condition of the water itself has changed little. The EPA's latest report, based on 2025 monitoring, found no major change in water quality in 2025. The biological health of our rivers and lakes has shown little change with slightly more than half (54%) in good or better biological quality. The agency has also flagged the loss of high-status sites as a warning sign, and it reports \"no clear evidence that nutrient levels are falling in the long term\".\n\nWaste disposal and its geographic challenges\n\nWaste management in Ireland is shaped by distance, limited landfill space, and reliance on exports. Irish municipal waste shipped abroad totalled about 1.2 million tonnes, and roughly 38 per cent of that was burned overseas. A lot of that \"recovery\" happens outside Ireland as the country exported 1.2 million tonnes of municipal waste, 38 per cent of which was incinerated. Because the country depends on external treatment capacity, its recycling and recovery figures are sensitive to shipping and to the policies of receiving states.\n\nDomestic practice has changed considerably. Landfill was once dominant, but there has been a steep decline in Ireland's landfill rate for municipal waste from over 80% in 2001. In 2023 the municipal recycling rate was 42 per cent, while the landfill share was 14 per cent. Ireland must reduce municipal landfilling to 10 per cent or less by 2035, a target that the EPA considers challenging. The recycling targets are also demanding: the 55 per cent municipal recycling target set for 2025 was not met. Construction and demolition waste is the largest stream by volume, and soil and stone make up most of it. Soil and stone is the largest waste fraction of this stream, accounting for 82% of the stream.\n\nNorthern Ireland faces a similar set of problems with different timing. This is particularly important due to the expectation that infrastructure capacity could be reached by 2028 or soon after. In 2022–23, about 1.29 million tonnes of waste went to landfill there. Current national responses, including the circular-economy waste plan that succeeded the earlier regional plans, aim to move waste from disposal toward prevention and reuse. The national strategy, the Waste Action Plan for a Circular Economy, charts a pathway away from simply disposing of waste towards a resource-efficient, circular economy model.\n\nInvasive species, habitat loss and cross-cutting pressures\n\nInvasive species and habitat loss are interlinked pressures. Most non-native species introduced to Ireland since 1500 have increased, and although most are harmless, \"some have become invasive, notably Himalayan balsam, Japanese knotweed and rhododendron, with negative impacts on native flora and fauna\". The mechanisms are mainly direct competition with native species, habitat alteration, and the spread of parasites and pathogens. Freshwater rivers, ponds, native woodland, lowland heath, and coastal saltmarsh and dune systems are among the habitats under threat, and native animals such as red squirrels and white-clawed crayfish are also affected.\n\nHabitat loss has other drivers. The national biodiversity plan lists agriculture, forestry, invasive species, resource extraction and development as the main pressures on biodiversity. Losses are concentrated in species associated with grasslands, wetlands and hedgerow margins – habitats that have been most heavily affected by agricultural intensification. Climate change acts as an additional, cross-cutting pressure, since shifts in rainfall and temperature affect river flows, nutrient transport and the hydrology of wetlands and peatlands.\n\nPolicy responses and monitoring\n\nPolicy operates at national, EU and international levels. The revised national biodiversity plan sets out 194 actions and, for the first time, is backed by statutory powers. The plan requires Government departments, State agencies and local authorities to integrate biodiversity into plans and policies – and to report on progress to the Minister. Under EU law, Ireland must restore all water bodies to satisfactory ecological condition by 2027, a deadline the EPA considers unrealistic. Water-quality measures so far include mercury limits, nutrient controls and bans on certain flame retardants. Ireland also operates under a derogation from the Nitrates Directive, which is subject to an interim review. On invasive species, the National Parks and Wildlife Service and the National Biodiversity Data Centre announced in May 2026 a partnership that will establish an Invasive Species Bureau to support EU regulations and coordinate monitoring. Monitoring itself is continuous: the EPA publishes annual water-quality indicators, and the Data Centre issues species alerts after expert verification of new sightings. The EPA has stated that the pace and scale of restoration measures must be increased if the trend is to change."
    },
    {
      "heading": "Geographical knowledge and naming",
      "text": "Classical and medieval descriptions\n\nIreland entered written geography through Greek and Roman sources. The explorer Pytheas of Massilia, writing around 320 BC, called the island Ierne during his voyages in northwest Europe. The Greek form later gave rise to the Latin Hibernia, which Julius Caesar used in the 1st century BC and which became the standard Latin name. Roman writers also used forms such as Iuverna, and the Latin name may have been reinterpreted in association with hibernus, \"wintry,\" although its root is a Celtic name meaning something like \"fertile land.\"\n\nThe most detailed classical account is Ptolemy's Geography, compiled in the 2nd century AD. It gives the coordinates of six promontories, fifteen river mouths, ten settlements, nine islands and sixteen population groups, and it calls the island Iouernia. Ptolemy almost certainly never visited Ireland. His map drew on reports from soldiers, traders and travellers, combined with his own mathematical calculations, and modern scholars regard it as remarkably accurate for its time and sources. Because Ireland was never conquered by Rome, Roman knowledge of the island stayed fragmentary, and Ptolemy's material survived mainly through manuscript copies made during the Middle Ages.\n\nSurveys and the development of modern mapping\n\nThe first detailed land survey of Ireland was the Down Survey, carried out under the English scientist William Petty in the mid-1650s. Its teams measured each townland, and the resulting cadastral maps were designed to support the redistribution of land confiscated from Irish owners. Petty later drew on this material for Hiberniae Delineatio (1685), the first printed atlas of Ireland. The Down Survey's areas and valuations were later judged unreliable, which became a reason for a new survey.\n\nThe Ordnance Survey of Ireland began in 1824, with fieldwork carried out from 1824 and the six-inch-to-the-mile maps produced in the following decades. By 1830 the survey employed nearly 2,000 people, and it worked from north to south. Its fieldwork was largely complete by 1842, and the engraving of the six-inch maps was finished in 1846. Alongside the maps, officers wrote memoirs and name books describing local economy, language and environment, which make the survey a valuable record of pre-Famine Ireland. The Ordnance Survey of Northern Ireland was established in 1922, and the Republic's mapping is now handled by Ordnance Survey Ireland. Digitisation of historical maps began in the 2000s, and modern mapping now relies on geographic information systems and map projections that allow old and new surveys to be compared.\n\nGeological mapping followed a similar path of systematic national survey, which is covered in the geology article. Later survey methods, including aerial photography and satellite imagery, have added remote sensing to field observation, allowing changes in land cover, coastlines and water bodies to be tracked over time. Digital databases now combine these sources, so that geographical knowledge of Ireland is held in layered, regularly updated datasets rather than in single printed maps.\n\nNaming the island: Éire, Ireland and the Emerald Isle\n\nThe Irish name Éire derives from Ériu, a goddess associated with sovereignty and the land in Irish mythology, who was traditionally linked with her sisters Banba and Fódla. The English name Ireland combines Ire, a form of Éire, with the word land. The poetic form Erin comes from the dative case Éirinn. Under the Irish Free State, the state adopted the name Éire in its 1937 Constitution, and the state became the Republic of Ireland in 1949. Éire now appears on coins, stamps and official documents.\n\nThe nickname Emerald Isle is generally traced to William Drennan, a Belfast-born physician and United Irishmen activist, whose poem about Erin is usually dated to 1795. Some later printings and commentaries give 1800 for the same poem, so the exact date varies by source. Drennan's poem used the island's green landscape as a symbol while also addressing political struggles against British rule, a context that is often left out of tourism usage. The nickname spread through literature and song in the 19th century and remains widely used in tourism, although it is less common in everyday speech."
    },
    {
      "heading": "Regional context and comparison",
      "text": "Rank among North Atlantic islands\n\nThe island lies off the northwestern edge of the European continent, with the Atlantic on its western side and the Celtic Sea to its south Ireland is located off the north western coastline of European continent. ... Ireland is bounded by the Atlantic Ocean – by the Celtic Sea in the south. By size, the island holds second place among the islands of the British Isles and third place in Europe, and it ranks around twentieth in the world second-largest island of the British Isles, the third-largest in Europe, and the twentieth-largest in the world. Within Europe, only Great Britain and Iceland are larger; Iceland's area is listed at 101,826 km² Iceland | 101,826 | 39,315 | Iceland.\n\nComparison with Great Britain\n\nGreat Britain is the largest island of the archipelago, but published figures for its area disagree. One list gives 218,634.50 km², while another gives 229,848 km2 and a population of about 61 million people. The difference probably reflects differing coastline treatment and data sources, so comparisons should use a single dataset. Ireland's all-island population is far smaller. The 2022 joint census recorded the island at 7.1 million, with Ireland now accounts for 73% of the all-island population with 5.15 million residents, while Northern Ireland makes up 27% with 1.91 million people.\n\nThe two islands also differ in relief. Ireland's uplands are comparatively modest, comprising relatively low-lying mountains surrounding a central plain. Its highest summit, Carrauntoohil, reaches 1,041 m (3415 ft), whereas Ben Nevis in Scotland, on Great Britain, rises to about 1,345 m. Both islands share the moderating influence of the Atlantic, so their climatic contrasts are mainly regional, with the western and upland areas of each being wetter and cooler than the lowlands of the east and south.\n\nRelation to continental Europe\n\nIreland is separated from Great Britain by the North Channel, the Irish Sea, and St George's Channel, so its links with the continent run mainly across open water rather than by land. Its western seaboard faces the Atlantic, and the broader Atlantic weather systems that cross Europe shape its climate. In that sense, the island is part of the North Atlantic maritime setting that also connects Great Britain, Iceland and the Scandinavian coasts.\n\nComparison with other European island nations\n\nFive of Europe's sovereign states are islands or island groups. Two of them, Iceland and the Republic of Ireland, are comparable in size. The other three (Cyprus at 9,251 km², Iceland at 103,000 km², and the Republic of Ireland at 70,273 km²) sit between those extremes. Among the large Mediterranean islands, Sicily covers 25,662 km², so the whole island of Ireland is more than three times the size of Sicily. Iceland is far more sparsely settled: Iceland is the most sparsely populated country in Europe, with about 400,000 people across 103,000 square kilometers (roughly 3.9 people per square kilometer). By contrast, the Republic's density is Ireland (73 people per km²).\n\nIn terms of population, the island ranks second-most populous island in Europe after Great Britain. Its coastline of 7,527 km (4677.1 mi) is long for an island of its area, a result of indented shores and headlands, although the total depends heavily on the measurement scale used."
    }
  ],
  "links": [
    "united-kingdom",
    "ocean",
    "europe",
    "plate-tectonics",
    "geography",
    "karst",
    "river",
    "estuary",
    "climate-change",
    "storm-surge",
    "sea-level-rise",
    "species",
    "invasive-species",
    "biodiversity",
    "urbanization",
    "city",
    "demography",
    "fertilizer",
    "eutrophication",
    "nitrogen-cycle",
    "groundwater",
    "wetland",
    "geographic-information-system",
    "geology",
    "remote-sensing"
  ],
  "sources": [
    {
      "title": "Ireland",
      "url": "https://en.wikipedia.org/wiki/Ireland"
    },
    {
      "title": "Geography of Ireland",
      "url": "https://en.wikipedia.org/wiki/Geography_of_Ireland"
    },
    {
      "title": "Relative Size of Ireland - Ireland's History in Maps",
      "url": "https://sites.rootsweb.com/~irlkik/ihm/rel_size.htm"
    },
    {
      "title": "The Shannon-Erne Waterway",
      "url": "https://derosia.com/old/ireland/geography.html"
    },
    {
      "title": "Republic of Ireland",
      "url": "https://en.wikipedia.org/wiki/Republic_of_Ireland"
    },
    {
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    {
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    },
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    },
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    },
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    },
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    },
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      "title": "Untitled",
      "url": "https://www.ucd.ie/wac-6/text11.html"
    },
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    },
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    },
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    },
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    },
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      "url": "https://trips.ie/inishtrahull/"
    },
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      "url": "https://www.britannica.com/place/Iapetus-Ocean"
    },
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      "title": "Basement structure and the terrane model of Northern Ireland - MediaWiki",
      "url": "https://earthwise.bgs.ac.uk/index.php/Basement_structure_and_the_terrane_model_of_Northern_Ireland"
    },
    {
      "title": "Caledonian orogeny facts for kids",
      "url": "https://kids.kiddle.co/Caledonian_orogeny"
    },
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      "url": "https://ougs.org/ireland/local-geology/"
    },
    {
      "title": "(PDF) Hydrogeology of lowland karst in Ireland",
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    },
    {
      "title": "(PDF) The Use of Multiple Techniques for Conceptualisation of Lowland Karst, a case study from County Roscommon, Ireland",
      "url": "https://www.researchgate.net/publication/285731536_The_Use_of_Multiple_Techniques_for_Conceptualisation_of_Lowland_Karst_a_case_study_from_County_Roscommon_Ireland"
    },
    {
      "title": "Carboniferous limestone",
      "url": "https://www.askaboutireland.ie/reading-room/environment-geography/physical-landscape/Irelands-physical-landsca/the-formation-of-the-phys/carboniferous-limestone/"
    },
    {
      "title": "Ireland topographic map, elevation, terrain",
      "url": "https://en-ie.topographic-map.com/map-rgp/Ireland/"
    },
    {
      "title": "Ireland's Geography",
      "url": "https://www.askaboutireland.ie/learning-zone/secondary-students/cspe/geography-of-ireland/"
    },
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    },
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    },
    {
      "title": "MacGillycuddy's Reeks - Wikishire",
      "url": "https://wikishire.co.uk/wiki/MacGuillycuddy's_Reeks"
    },
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      "url": "https://www.ireland-information.com/reference/geog.html"
    },
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    },
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    },
    {
      "title": "Coastal landforms of Ireland",
      "url": "https://en.wikipedia.org/wiki/Coastal_landforms_of_Ireland"
    },
    {
      "title": "Shannon River Basin",
      "url": "https://en.wikipedia.org/wiki/Shannon_River_Basin"
    },
    {
      "title": "Rivers of Ireland",
      "url": "https://en.wikipedia.org/wiki/Rivers_of_Ireland"
    },
    {
      "title": "River Shannon",
      "url": "https://www.britannica.com/place/River-Shannon"
    },
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      "url": "https://en.wikipedia.org/wiki/River_Shannon"
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      "url": "https://en.wikipedia.org/wiki/List_of_rivers_of_Ireland"
    },
    {
      "title": "Lough Neagh",
      "url": "https://en.wikipedia.org/wiki/Lough_Neagh"
    },
    {
      "title": "Bann drainage",
      "url": "https://en.wikipedia.org/wiki/Bann_drainage"
    },
    {
      "title": "Lough Neagh: Ireland’s Vast Lake of Legends and Leisure",
      "url": "https://lakehub.com/lake-info/lough-neagh-irelands-vast-lake-of-legends-and-leisure/"
    },
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    },
    {
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    },
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    },
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    },
    {
      "title": "ISSN 1393",
      "url": "https://www.npws.ie/sites/default/files/publications/pdf/IWM99_RB_Restoration_Best%20Practice%20Guidance.pdf"
    },
    {
      "title": "Boglands",
      "url": "https://www.askaboutireland.ie/learning-zone/primary-students/looking-at-places/offaly/aspects-of-offaly/boglands/"
    },
    {
      "title": "Over-Exploitation of Peatlands for Peat - Irish Peatland Conservation CouncilIrish Peatland Conservation Council",
      "url": "https://www.ipcc.ie/a-to-z-peatlands/irelands-peatland-conservation-action-plan/peatland-action-plan/over-exploitation-of-peatlands-for-peat/"
    },
    {
      "title": "Bellanagare Bog",
      "url": "https://en.wikipedia.org/wiki/Bellanagare_Bog"
    },
    {
      "title": "Blanket Bogs of Ireland FactsheetIrish Peatland Conservation Council",
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    },
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    },
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    },
    {
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    },
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    },
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    },
    {
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      "url": "https://www.sciencedirect.com/science/article/abs/pii/S0301479795901345"
    },
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    },
    {
      "title": "EPA Climate Ireland",
      "url": "https://www.climateireland.ie/impact-on-ireland/climate-hazards/coastal-erosion/"
    },
    {
      "title": "Coastal erosion - ClimateChangePost",
      "url": "https://www.climatechangepost.com/countries/ireland/coastal-erosion/"
    },
    {
      "title": "A coastal exposure index for Ireland: relative hazard exposure and the protective role of coastal habitats",
      "url": "https://link.springer.com/article/10.1007/s11069-026-08361-w"
    },
    {
      "title": "A new seabed mobility index for the Irish Sea: Modelling seabed shear stress and classifying sediment mobilisation to help predict erosion, deposition, and sediment distribution - ScienceDirect",
      "url": "https://www.sciencedirect.com/science/article/pii/S0278434321002302"
    },
    {
      "title": "(PDF) Benthic surveys of sandbanks in the Irish Sea",
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    },
    {
      "title": "Vulnerable Coastal \"Hotspots\" Identified in UCC Study - Afloat",
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    },
    {
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    },
    {
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    },
    {
      "title": "Salmon Farming in Ireland - Salmon Watch Ireland",
      "url": "https://salmonwatchireland.ie/salmon-farming-ireland/"
    },
    {
      "title": "Aqua Facts - Irish Farmers' Association",
      "url": "https://www.ifa.ie/aqua-facts/"
    },
    {
      "title": "Irish Aquaculture \"Resilient\" In Spite of Challenging 2023, BIM Report Says",
      "url": "https://afloat.ie/port-news/fishing/aquaculture/item/65155-irish-aquaculture-resilient-in-spite-of-challenging-2023-bim-report-says"
    },
    {
      "title": "Climate of Ireland",
      "url": "https://en.wikipedia.org/wiki/Climate_of_Ireland"
    },
    {
      "title": "Ireland's climate",
      "url": "https://storymaps.arcgis.com/stories/e452f01dfb86418c9cdaf318cc0d81d3"
    },
    {
      "title": "Climate of Ireland - Met Éireann - The Irish Meteorological Service",
      "url": "https://www.met.ie/climate/climate-of-ireland"
    },
    {
      "title": "Met Éireann warns of potential gulf stream collapse - Agriland.ie",
      "url": "https://www.agriland.ie/farming-news/met-eireann-warns-of-potential-gulf-stream-collapse/"
    },
    {
      "title": "Climate of Ireland — Grokipedia",
      "url": "https://grokipedia.com/page/Climate_of_Ireland"
    },
    {
      "title": "Oceanic climate",
      "url": "https://www.classicistranieri.com/wikipediaforschools/wp/o/Oceanic_climate.htm"
    },
    {
      "title": "Ireland Weather by Month: A Traveller's Guide - Approach Tours",
      "url": "https://approachtours.com/ireland-weather-by-month/"
    },
    {
      "title": "Blue Green Atlas - The Climate of Ireland",
      "url": "https://bluegreenatlas.com/climate/ireland_climate.html"
    },
    {
      "title": "Annual Climate Statement for 2025 - Met Éireann - The Irish Meteorological Service",
      "url": "https://www.met.ie/annual-climate-statement-for-2025"
    },
    {
      "title": "Human-caused Climate Change Brings Increased Storm Rainfall - Met Éireann - The Irish Meteorological Service",
      "url": "https://www.met.ie/human-caused-climate-change-brings-increased-storm-rainfall"
    },
    {
      "title": "Ireland weather: Thunderstorms and heavy rain expected as Met Éireann issues weather warning",
      "url": "https://www.irishtimes.com/ireland/2025/07/14/thunderstorms-and-heavy-rain-expected-as-met-eireann-issues-weather-warning/"
    },
    {
      "title": "The Irish Climate",
      "url": "https://www.croancottages.com/weather.htm"
    },
    {
      "title": "Climate change",
      "url": "https://www.epa.ie/environment-and-you/climate-change/"
    },
    {
      "title": "EPA Climate Ireland",
      "url": "https://www.climateireland.ie/impact-on-ireland/future-climate-of-ireland/"
    },
    {
      "title": "Storm Centre - Met &Eacuteireann - The Irish Meteorological Service",
      "url": "https://cli.fusio.net/cli/stormcenter/index.html"
    },
    {
      "title": "EPA Climate Ireland",
      "url": "https://www.climateireland.ie/impact-on-ireland/future-climate-of-ireland/sea-level-rise/"
    },
    {
      "title": "EPA Climate Ireland",
      "url": "https://www.climateireland.ie/impact-on-ireland/climate-hazards/coastal-flooding/"
    },
    {
      "title": "Coastal floods - ClimateChangePost",
      "url": "https://www.climatechangepost.com/ireland/coastal-floods/"
    },
    {
      "title": "Meteorologist's Commentary - Met Éireann - The Irish Meteorological Service",
      "url": "https://www.met.ie/forecasts/meteorologists-commentary"
    },
    {
      "title": "CLIMATOLOGICAL NOTE NO.14 A SUMMARY OF CLIMATE AVERAGES FOR IRELAND 1981-2010",
      "url": "https://www.fruitandnut.ie/climate.Ireland.pdf"
    },
    {
      "title": "www.pressreader.com",
      "url": "https://www.pressreader.com/ireland/irish-daily-star/20240509/283326117440806"
    },
    {
      "title": "Rolling Lowlands",
      "url": "https://link.springer.com/chapter/10.1007/978-3-319-71189-8_10"
    },
    {
      "title": "Limestone Lowland Landscapes",
      "url": "https://www.askaboutireland.ie/learning-zone/secondary-students/geography/physical-environment/soil-types-in-ireland/limestone-lowland-landsca/"
    },
    {
      "title": "The Soils of Ireland By PIERCE RYAN, B.Agr.Sc., M.Sc.,",
      "url": "https://scispace.com/pdf/the-soils-of-ireland-56qunkosx2.pdf"
    },
    {
      "title": "Topography of Ireland",
      "url": "https://earthobservatory.nasa.gov/images/5343/topography-of-ireland"
    },
    {
      "title": "Previous Page Table of Contents Next Page",
      "url": "https://fao.org/fishery/docs/CDrom/aquaculture/a0844t/docrep/009/T0377E/T0377E15.htm"
    },
    {
      "title": "Ireland Mining History",
      "url": "https://www.askaboutireland.ie/enfo/irelands-environment/mineral-extraction/ireland-mining-history/"
    },
    {
      "title": "Mineral Extraction",
      "url": "https://www.askaboutireland.ie/enfo/irelands-environment/mineral-extraction/"
    },
    {
      "title": "Mining in Ireland - MMTA",
      "url": "https://mmta.co.uk/mining-in-ireland/"
    },
    {
      "title": "Minerals from Ireland",
      "url": "https://albionfireandice.co.uk/localities/ireland/"
    },
    {
      "title": "Forgotten industrial relations",
      "url": "https://www.irishtimes.com/news/forgotten-industrial-relations-1.349867"
    },
    {
      "title": "Ireland Locality Guide",
      "url": "https://earthwonders.com/guides/ireland_81"
    },
    {
      "title": "Mining in Ireland: Best Rich Heritage Guide",
      "url": "https://www.connollycove.com/rich-heritage-of-mining-in-ireland/"
    },
    {
      "title": "Minerals",
      "url": "https://www.gov.ie/en/department-of-climate-energy-and-the-environment/policy-information/minerals/"
    },
    {
      "title": "irish minerals - Rock n Gem Magazine",
      "url": "https://www.rockngem-magazine.co.uk/index.php/content/minerals-in-rockngem-magazine/188-irish-minerals"
    },
    {
      "title": "1 Saint-Gobain Mining (Ireland) Ltd., Dublin Road, Kingscourt, Co. Cavan",
      "url": "https://epawebapp.epa.ie/licences/lic_eDMS/090151b2806fdcfa.pdf"
    },
    {
      "title": "2019 Minerals Yearbook U.S. Department of the Interior U.S. Geological Survey",
      "url": "https://pubs.usgs.gov/myb/vol3/2019/myb3-2019-ireland.pdf"
    },
    {
      "title": "Monaghan sinkholes: ‘The mining is a cancer in our parish’",
      "url": "https://www.irishtimes.com/news/environment/monaghan-sinkholes-the-mining-is-a-cancer-in-our-parish-1.3754925"
    },
    {
      "title": "Mining in Ireland",
      "url": "https://www.conroygoldandnaturalresources.com/projects/mining-ireland"
    },
    {
      "title": "Name of Lead Investigator Mark Holdstock Email mholdstock@aurumexploration.com",
      "url": "https://www.imcexploration.com/media/attachments/2017/12/07/mine_waste_aurum_final_report.pdf"
    },
    {
      "title": "Geology of Ireland facts for kids",
      "url": "https://kids.kiddle.co/Geology_of_Ireland"
    },
    {
      "title": "NATIONAL SURVEY OF NATIVE WOODLAND IN IRELAND",
      "url": "https://www.npws.ie/sites/default/files/publications/pdf/Higgins_et_al_2004_Woodland_Interim_Report.pdf"
    },
    {
      "title": "History of Forestry in Ireland - Forestry Services Limited",
      "url": "https://forestryservices.ie/history-of-forestry-in-ireland/"
    },
    {
      "title": "A brief history of Ireland's native woodlands - Coillte",
      "url": "https://www.coillte.ie/a-brief-history-of-irelands-native-woodlands/"
    },
    {
      "title": "Memories of Early Modern Deforestation and Modern Irish Forest Policy",
      "url": "https://www.nacbs.org/post/memories-of-early-modern-deforestation-and-modern-irish-forest-policy"
    },
    {
      "title": "Forestry since Tudor Times - Forestry Focus",
      "url": "https://www.forestryfocus.ie/forests-woodland/history-of-irish-forestry/forestry-since-tudor-times/"
    },
    {
      "title": "Does Ireland Have Trees? Its Forest History & Future - Biology Insights",
      "url": "https://biologyinsights.com/does-ireland-have-trees-its-forest-history-future/"
    },
    {
      "title": "0b1fafb5-9475-4955-bbbc-26bd9effb509.pdf",
      "url": "https://assets.gov.ie/246991/0b1fafb5-9475-4955-bbbc-26bd9effb509.pdf"
    },
    {
      "title": "List of forests in Ireland — Grokipedia",
      "url": "https://grokipedia.com/page/List_of_forests_in_Ireland"
    },
    {
      "title": "Area forested with native species",
      "url": "https://irishriverproject.com/2021/12/14/area-forested-with-native-species/"
    },
    {
      "title": "A Historical View of Woodlands in Ireland - Teagasc",
      "url": "https://teagasc.ie/news--events/daily/a-historical-view-of-woodlands-in-ireland/"
    },
    {
      "title": "Raised Bogs in Ireland FactsheetIrish Peatland Conservation Council",
      "url": "https://www.ipcc.ie/a-to-z-peatlands/peatland-habitat-types/raised-bogs/"
    },
    {
      "title": "Conservation and Management of Raised Bogs in Ireland",
      "url": "https://peatlands.org/assets/uploads/2019/06/OConnell-165.pdf"
    },
    {
      "title": "Peatland Conservation - Clara Bog Nature Reserve",
      "url": "https://www.clarabognaturereserve.ie/article-conservation-management/article-peatland-conservation/"
    },
    {
      "title": "National National Survey Survey of Native of Native Woodlands Woodlands 2003",
      "url": "https://www.npws.ie/sites/default/files/general/nsnw-vol-1.pdf"
    },
    {
      "title": "Forestry Facts and News",
      "url": "https://www.gov.ie/en/department-of-agriculture-food-and-the-marine/publications/forestry-facts-and-news/"
    },
    {
      "title": "Raised Bog",
      "url": "https://www.askaboutireland.ie/enfo/irelands-environment/peatlands/peatlands-in-ireland/raised-bog/"
    },
    {
      "title": "Ardgraigue Bog",
      "url": "https://en.wikipedia.org/wiki/Ardgraigue_Bog"
    },
    {
      "title": "Ireland Population (2026) - Worldometer",
      "url": "https://www.worldometers.info/world-population/ireland-population/"
    },
    {
      "title": "Migration fuels Northern Ireland’s population growth to 1.93 million",
      "url": "https://www.loveballymena.online/post/migration-fuels-northern-ireland-s-population-growth-to-1-93-million"
    },
    {
      "title": "Ireland Demographics 2024 (Population, Age, Sex, Trends) - Worldometer",
      "url": "https://srv1.worldometers.info/demographics/ireland-demographics/"
    },
    {
      "title": "CSO data shows a 12% decrease in immigration to Ireland in the year to April 2026 - The European Migration Network",
      "url": "https://emn.ie/cso-pop-est-2026/"
    },
    {
      "title": "Ireland Population (2026) - Worldometer",
      "url": "https://ipv6.worldometers.info/world-population/ireland-population/"
    },
    {
      "title": "Ireland Population Pyramid 2026",
      "url": "https://www.populationpyramid.net/ireland/2026/"
    },
    {
      "title": "www.cso.ie",
      "url": "https://www.cso.ie/en/releasesandpublications/ep/p-eii/environmentalindicatorsireland2023/landuse"
    },
    {
      "title": "Extent Ecosystem Accounts - Grasslands and Croplands 2018 - Central Statistics Office",
      "url": "https://www.cso.ie/en/releasesandpublications/fp/fp-eagac/ecosystemaccounts-grasslandsandcroplands2018/extent/"
    },
    {
      "title": "Land Use in Ireland",
      "url": "https://www.askaboutireland.ie/enfo/sustainable-living/farming-in-ireland-overvi/land-use-in-ireland/"
    },
    {
      "title": "Profile of Irish Agriculture & Food using CSO, EStat and ...",
      "url": "https://www.climatecouncil.ie/media/climatechangeadvisorycouncil/contentassets/documents/presentations/14.06.2021%20Profile%20of%20Irish%20Agriculture%20&%20Food%20%20using%20CSO,%20EStat%20and%20Teagasc%20NFS%20economic%20data.pdf"
    },
    {
      "title": "www.cso.ie",
      "url": "https://www.cso.ie/en/releasesandpublications/ep/p-eii/environmentalindicatorsireland2024/landuse"
    },
    {
      "title": "Frontiersin",
      "url": "https://www.frontiersin.org/journals/agronomy/articles/10.3389/fagro.2022.1063773/xml"
    },
    {
      "title": "Teagasc",
      "url": "https://teagasc.ie/wp-content/uploads/2025/05/General-1.pdf"
    },
    {
      "title": "Tillage Crops - Teagasc",
      "url": "https://teagasc.ie/crops/soil-soil-fertility/trace-elements/tillage-crops/"
    },
    {
      "title": "Farming for Soil Health Best practices for managing Irish agricultural soils",
      "url": "https://teagasc.ie/wp-content/uploads/uploads/media/website/publications/2025/Farming-for-Soil-Health-Web.pdf"
    },
    {
      "title": "www.cso.ie",
      "url": "https://www.cso.ie/en/releasesandpublications/ep/p-eiigcc/environmentalindicatorsireland2025-globalcontextandclimate/landuse"
    },
    {
      "title": "New standard promotes stewardship of woodlands in Ireland",
      "url": "https://fsc.org/en/newscentre/general-news/new-standard-promotes-stewardship-of-woodlands-in-ireland"
    },
    {
      "title": "Native trees cover just 2% of Ireland. How can this be increased?",
      "url": "https://www.irishtimes.com/culture/heritage/native-trees-cover-just-2-of-ireland-how-can-this-be-increased-1.3553824"
    },
    {
      "title": "Does Ireland have the will to undo the disaster of plantation forestry?",
      "url": "https://www.irishtimes.com/environment/2026/10/01/does-ireland-have-the-will-to-undo-the-disaster-of-plantation-forestry/"
    },
    {
      "title": "Ireland's Energy Sources - Where Do We Get Our Electricity From?",
      "url": "https://selectra.ie/energy/guides/energy-market/ireland-energy-sources"
    },
    {
      "title": "Oil and gas",
      "url": "https://irelandenergy2050.ie/present/oil-and-gas/?q=where-does-ireland-get-its-electricity"
    },
    {
      "title": "Renewable Energy in Ireland",
      "url": "https://www.seai.ie/data-and-insights/seai-statistics/key-publications/renewable-energy-in-ireland"
    },
    {
      "title": "Renewable Energy Ireland 2026",
      "url": "https://climatejargonbuster.ie/renewable-energy-ireland/"
    },
    {
      "title": "Peat",
      "url": "https://irelandenergy2050.ie/past/peat/"
    },
    {
      "title": "Energy in Ireland",
      "url": "https://en.wikipedia.org/wiki/Energy_in_Ireland"
    },
    {
      "title": "Peat used for final time this weekend in power station",
      "url": "https://www.offalyindependent.ie/2024/01/01/peat-used-for-final-time-this-weekend-in-power-station/"
    },
    {
      "title": "Last of the peat-fired electricity power plants in Ireland switches to biomass",
      "url": "https://thedirt.news/last-of-the-peat-fired-electricity-power-plants-in-ireland-switches-to-biomass/"
    },
    {
      "title": "Irish drinking water meets \"very high standards\" - EPA",
      "url": "https://www.rte.ie/news/2026/0701/1581181-irish-drinking-water/"
    },
    {
      "title": "Water Pollution",
      "url": "https://www.askaboutireland.ie/enfo/irelands-environment/water/water-pollution/"
    },
    {
      "title": "EPA DriNkiNG WAtEr ADViCE NOtE Advice Note No. 7:",
      "url": "https://www.epa.ie/publications/compliance--enforcement/drinking-water/advice--guidance/Advice-Note-No7.pdf"
    },
    {
      "title": "2.9. Republic of Ireland — European Environment Agency",
      "url": "https://www.eea.europa.eu/publications/92-9167-032-4/page011.html"
    },
    {
      "title": "Fresh water resources - Ireland",
      "url": "https://www.climatechangepost.com/countries/ireland/fresh-water-resources/"
    },
    {
      "title": "www.cso.ie",
      "url": "https://www.cso.ie/en/releasesandpublications/ep/p-eiigcc/environmentalindicatorsireland2025-globalcontextandclimate/water"
    },
    {
      "title": "Renewable Energy in Ireland",
      "url": "https://www.askaboutireland.ie/enfo/irelands-environment/energy/re/"
    },
    {
      "title": "West Offaly Power Station",
      "url": "https://en.wikipedia.org/wiki/West_Offaly_Power_Station"
    },
    {
      "title": "Edenderry Power Station",
      "url": "https://en.wikipedia.org/wiki/Edenderry_Power_Station"
    },
    {
      "title": "Water In Ireland",
      "url": "https://www.askaboutireland.ie/learning-zone/secondary-students/cspe/stewardship/water/water-in-ireland/"
    },
    {
      "title": "Water",
      "url": "https://www.gsi.ie/en-ie/education/our-water/Pages/default.aspx"
    },
    {
      "title": "Pollution from farms and wastewater keep Ireland's water quality so poor, watchdog says",
      "url": "https://www.thejournal.ie/poor-water-quality-epa-report-ireland-7072856-Jun2026/"
    },
    {
      "title": "Irish Waters in Trouble: What’s Really in Our Rivers?",
      "url": "https://universitytimes.ie/2025/11/irish-waters-in-trouble-whats-really-in-our-rivers/"
    },
    {
      "title": "Decline in Ireland's highest quality water bodies 'a serious warning sign', EPA says",
      "url": "https://www.echolive.ie/nationalnews/arid-41864151.html"
    },
    {
      "title": "There are no signs yet of an improvement in water quality and more action is needed, says EPA",
      "url": "https://www.epa.ie/news-releases/news-releases-2024/there-are-no-signs-yet-of-an-improvement-in-water-quality-and-more-action-is-needed-says-epa.php"
    },
    {
      "title": "Faster action is needed, as water quality shows little overall improvement in 2025, says EPA",
      "url": "https://www.epa.ie/news-releases/news-releases-2026/faster-action-is-needed-as-water-quality-shows-little-overall-improvement-in-2025-says-epa-.php"
    },
    {
      "title": "More than half of daily waste generated in Ireland burned or sent to landfill, EPA says",
      "url": "https://www.irishtimes.com/environment/2025/09/23/more-than-half-of-daily-waste-generated-in-ireland-burned-or-sent-to-landfill-epa-says/"
    },
    {
      "title": "Municipal Waste Statistics for Ireland",
      "url": "https://www.epa.ie/our-services/monitoring--assessment/waste/national-waste-statistics/municipal/"
    },
    {
      "title": "Ireland faces challenges in meeting waste targets",
      "url": "https://www.socialjustice.ie/article/ireland-faces-challenges-meeting-waste-targets"
    },
    {
      "title": "OFFICIAL OFFICIAL Waste management and illegal disposal in Northern Ireland",
      "url": "https://www.theoep.org.uk/sites/default/files/reports-files/Resource%20Futures_%20Waste%20management%20and%20illegal%20dumping%20-%20an%20evidence%20baseline%20assessment%20(October%202023).pdf"
    },
    {
      "title": "Ireland’s Waste Action Plan: Benefits & Prevention",
      "url": "https://www.allirelandsustainability.com/irelands-waste-action-plan/"
    },
    {
      "title": "Revised national biodiversity plan backed by new powers to protect and restore declining nature across Ireland",
      "url": "https://www.irishtimes.com/environment/2024/01/25/revised-national-biodiversity-plan-backed-by-new-powers-to-protect-and-restore-declining-nature-across-ireland/"
    },
    {
      "title": "Biodiversity in Ireland",
      "url": "https://enable-research.ie/biodiversity-ireland/"
    },
    {
      "title": "No improvement to water quality standards in 2025 - EPA",
      "url": "https://www.rte.ie/news/environment/2026/0617/1578808-water-quality-report/"
    },
    {
      "title": "Review of Waste Management in Northern Ireland",
      "url": "https://www.niauditoffice.gov.uk/files/niauditoffice/documents/2024-07/NI%20Audit%20Office%20Report%20-%20Review%20of%20Waste%20Management%20in%20Northern%20Ireland.pdf"
    },
    {
      "title": "INVASIVE SPECIES IN IRELAND Prepared for Environment & Heritage Service and",
      "url": "https://www.npws.ie/sites/default/files/publications/pdf/Stokes_et_al_2004_IAS_Ireland.pdf"
    },
    {
      "title": "Minister O’Sullivan announces new approach to tackling invasive species in Ireland",
      "url": "https://www.npws.ie/news/minister-o%E2%80%99sullivan-announces-new-approach-tackling-invasive-species-ireland"
    },
    {
      "title": "EU biodiversity strategy to 2020",
      "url": "https://biodiversity.europa.eu/countries/ireland/eu-biodiversity-strategy-to-2020"
    },
    {
      "title": "How Ireland Got Its Name: Éire, Ériu & the Goddess Origin",
      "url": "https://www.theirishjewelrycompany.com/blog/post/learn-how-ireland-got-its-name"
    },
    {
      "title": "10 Nicknames for Ireland and the History Behind Them",
      "url": "https://www.destguides.com/ireland/ireland-nicknames"
    },
    {
      "title": "Ireland’s many names and their meanings",
      "url": "https://www.irishpost.com/life-style/irelands-many-names-and-their-meanings-90875"
    },
    {
      "title": "How Ireland got its name and where the 'Emerald Isle' nickname came from",
      "url": "https://www.irishstar.com/culture/nostalgia/how-ireland-name-emerald-isle-30866311"
    },
    {
      "title": "Hibernia",
      "url": "https://en.wikipedia.org/wiki/Hibernia"
    },
    {
      "title": "Protohistory of Ireland",
      "url": "https://en.wikipedia.org/wiki/Protohistory_of_Ireland"
    },
    {
      "title": "Ptolemy%27s map of Ireland",
      "url": "https://en.wikipedia.org/wiki/Ptolemy%27s_map_of_Ireland"
    },
    {
      "title": "What is a Hibernian? - Ancient Order of Hibernians",
      "url": "https://www.louisvilleirish.com/about/what-is-a-hibernian/"
    },
    {
      "title": "Hibernia (personification)",
      "url": "https://en.wikipedia.org/wiki/Hibernia_(personification)"
    },
    {
      "title": "Nagnata",
      "url": "https://en.wikipedia.org/wiki/Nagnata"
    },
    {
      "title": "Down Survey",
      "url": "https://en.wikipedia.org/wiki/Down_Survey"
    },
    {
      "title": "Historic Maps - All Island Ireland - Map Collections at UCD and on the Web - LibGuides at UCD Library",
      "url": "https://libguides.ucd.ie/findingmaps/mapshistIreland"
    },
    {
      "title": "Online Resources for Irish Mapping Ordnance Survey maps",
      "url": "https://www.tcd.ie/library/map-library/assets/pdf/Online%20Resources%20for%20Irish%20Mapping.pdf"
    },
    {
      "title": "THE ORIGIN OF IRELAND’S ORDNANCE SURVEY - History Ireland",
      "url": "https://historyireland.com/the-origin-of-irelands-ordnance-survey/"
    },
    {
      "title": "The Ordnance Survey of Ireland",
      "url": "https://www.historicalballinrobe.org/places/mayo-and-irish-history/the_ordnance_survey_of_ireland"
    },
    {
      "title": "‘That's a powerful map’: Shared authority, public engagement, and the archives of the first Ordnance Survey of Ireland - ScienceDirect",
      "url": "https://www.sciencedirect.com/science/article/abs/pii/S030574882400152X"
    },
    {
      "title": "Ordnance Survey of Northern Ireland",
      "url": "https://en.wikipedia.org/wiki/Ordnance_Survey_of_Northern_Ireland"
    },
    {
      "title": "200 Years of Irish Maps",
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    },
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      "url": "https://www.worldatlas.com/maps/ireland"
    },
    {
      "title": "List of European islands by area",
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    },
    {
      "title": "List of islands by area",
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    },
    {
      "title": "Largest Islands Of Europe By Area",
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    },
    {
      "title": "ireland and northern ireland joint census publication 2021 2022 released",
      "url": "https://www.nisra.gov.uk/news/ireland-and-northern-ireland-joint-census-publication-2021-2022-released"
    },
    {
      "title": "graphsearch.epfl.ch",
      "url": "https://graphsearch.epfl.ch/en/concept/42677/concepts"
    },
    {
      "title": "Which European Countries Are Islands?",
      "url": "https://www.worldatlas.com/articles/island-countries-of-europe.html"
    },
    {
      "title": "ireland and northern ireland",
      "url": "https://www.nisra.gov.uk/statistics/census-2021-results/ireland-and-northern-ireland"
    }
  ],
  "license": "https://creativecommons.org/licenses/by/4.0/"
}