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The Irish countryside presents a remarkable tapestry of diverse landforms that have shaped both the physical landscape and the cultural identity of this island nation. From the fertile valleys carved by ancient rivers to the elevated plateaus that dominate certain regions, Ireland’s rural geography tells a story millions of years in the making. Understanding these landforms provides insight into the country’s agricultural heritage, settlement patterns, and the natural forces that continue to influence life across the Emerald Isle.
Understanding Ireland’s Geographical Framework
Ireland’s main geographical features include low central plains surrounded by coastal mountains, creating what geographers often describe as a bowl-shaped topography. The central limestone plain averages about 75 meters (246 feet) above sea level, interspersed with numerous lakes, bogs, and low ridges. This distinctive configuration has profoundly influenced how communities developed across the island and how land has been utilized for agriculture and settlement over millennia.
The geology of Ireland is diverse, with different regions containing rocks belonging to different geological periods, dating back almost 2 billion years. This geological diversity has created a landscape where ancient rock formations meet relatively recent glacial features, producing the varied terrain that characterizes modern Ireland.
The Formation of Irish Valleys
Valleys represent some of the most agriculturally productive and historically significant landforms in Ireland. These low-lying areas between hills or mountains have been carved primarily through fluvial erosion—the gradual wearing away of rock and soil by flowing water over countless millennia. The formation process continues today, though at an imperceptible pace compared to the dramatic reshaping that occurred during and after the last ice age.
Glacial Influence on Valley Development
The newer formations include drumlins and glacial valleys as a result of the last ice age, which ended approximately 10,000 years ago. Everywhere ice-smoothed rock, mountain lakes, glacial valleys, and deposits of sand, gravel and clay mark the passage of the ice. These glacial periods were instrumental in shaping the valleys we see today, with massive ice sheets grinding through existing river valleys and widening them considerably.
The glacial activity created two distinct types of valleys in Ireland: U-shaped valleys formed by glacial erosion, and V-shaped valleys carved primarily by river action. The U-shaped valleys, with their characteristic broad floors and steep sides, are particularly evident in mountainous regions where glaciers once flowed. Evidence of this is visible in the glacial valley of Glendalough, one of Ireland’s most famous glacial valleys located in County Wicklow.
River Valleys and Agricultural Significance
Rivers like the Shannon and the Boyne have created fertile floodplains, which are ideal for agriculture, supporting farming communities and contributing to Ireland’s economy. The periodic flooding of these valleys deposits nutrient-rich sediment across the floodplains, creating some of the most productive agricultural land in the country.
The mountain ridges of the south are composed of old, red sandstone separated by limestone river valleys, with the limestone valleys appearing as deep green grooves that tend to run in an east-west direction. This geological arrangement has created natural corridors for transportation and settlement, with many of Ireland’s historic towns and cities developing along these valley routes.
The Shannon Valley System
The River Shannon is the major river on the island of Ireland, and at 360 km (224 miles) in length, is the longest river in the British Isles, draining the Shannon River Basin, which has an area of 16,900 km² (6,525 sq mi) – approximately one fifth of the area of Ireland. The Shannon Valley represents Ireland’s most extensive valley system and has played a crucial role in the country’s development.
Shannon’s vast basin is dotted with lakes, wetlands, and towns that grew up around its fertile banks, making it a crucial artery for both nature and human settlement. The valley’s importance extends beyond agriculture; it has served as a major transportation corridor, a defensive boundary during various conflicts, and a source of hydroelectric power in modern times.
Along its course, the Shannon widens to form several large lakes. Along the river’s course, three lakes develop — Lough Allen, Lough Ree, and Lough Derg. These lakes are technically part of the river system but function as distinct geographical features, providing habitats for wildlife, recreational opportunities, and additional water resources for surrounding communities.
Notable Valley Regions
Beyond the Shannon, Ireland contains numerous other significant valleys that contribute to the country’s geographical diversity. The Boyne Valley in the east holds immense historical significance, being the site of ancient monuments and the famous Battle of the Boyne. Rivers like the Barrow, Suir, and Nore wind through the lush southeast, their waters feeding into the Celtic Sea and supporting rich farmlands and vibrant communities.
In the southwest, valleys cut through the mountainous terrain of Counties Kerry and Cork, creating dramatic landscapes where steep-sided valleys meet the Atlantic Ocean. These valleys often contain small farming communities that have adapted their agricultural practices to the challenging terrain, focusing on sheep grazing and specialized crops suited to the valley microclimates.
Plateaus: Ireland’s Elevated Flatlands
Plateaus represent a distinctive category of Irish landforms—elevated areas with relatively flat surfaces that rise above the surrounding terrain. Unlike mountains, which feature peaked summits, plateaus maintain their flat or gently rolling character despite their elevation. These landforms have formed through various geological processes and serve important functions in Ireland’s rural landscape.
The Antrim Plateau
A basalt plateau covers much of the north-east of the country, representing one of Ireland’s most geologically distinctive features. This plateau originated in the lava flows that produced basalt rock in a great period of volcanic activity over fifty million years ago. The Antrim Plateau, also known as the Antrim Basalt Plateau, covers significant portions of County Antrim in Northern Ireland.
This volcanic plateau is famous for the Giant’s Causeway, a UNESCO World Heritage Site featuring approximately 40,000 interlocking basalt columns formed by ancient lava flows cooling and contracting. The plateau’s volcanic origin gives it distinct soil characteristics that differ from the limestone-based soils found in much of central Ireland, influencing both natural vegetation and agricultural practices in the region.
Limestone Plateaus and Karst Features
The Aran Islands (Inishmore, Inishmaan, and Inisheer) are limestone plateaus that rise directly from the Atlantic Ocean. These islands exemplify how plateau formations can occur in coastal settings, with their flat limestone surfaces creating unique ecosystems and challenging agricultural conditions.
The limestone composition of many Irish plateaus has led to the development of karst topography—landscapes characterized by underground drainage systems, caves, and sinkholes. Areas of limestone karst are widespread in Ireland, resulting in a large number of caves throughout the country. The Burren in County Clare represents perhaps the most famous example of a limestone plateau with extensive karst features, creating a stark, rocky landscape that supports unique flora and fauna.
Plateaus in the Irish Midlands
The Irish Midlands contain several plateau regions that, while less dramatic than coastal plateaus, play important roles in regional geography and land use. Plateaus are associated with areas where grit and shale rocks from the much older ‘Upper Carboniferous’ geological period overlie the more widespread limestones.
The Castlecomer plateau is a 30 km long, 22 km wide, basin-shaped upland wedged between the valleys of the Nore and Barrow rivers, located mainly in north Kilkenny and south Laois, rising steeply from the adjacent lowlands and mostly at a height of 200-300 metres, composed of sandstones, grits and coal measures from the Upper Carboniferous. This plateau has historical significance due to its coal deposits, which were mined from the seventeenth century onward.
Agricultural Use of Plateau Lands
Plateaus characterise other upland areas, usually with altitudes between 150 and 400 metres. These elevated flatlands are often used for grazing livestock, particularly sheep and cattle, as the terrain is too elevated or the soil too thin for intensive crop cultivation. The relatively flat surfaces of plateaus make them more accessible than steep mountainsides, allowing for easier movement of livestock and farm equipment.
The climate on plateaus tends to be cooler and wetter than in lowland areas, with increased exposure to wind. This creates challenges for agriculture but also opportunities for certain types of farming. Hardy grass species thrive on many plateau regions, providing natural pasture for grazing animals. Some plateau areas have been developed for forestry, with coniferous plantations established on land unsuitable for other agricultural uses.
The Central Lowlands: Ireland’s Agricultural Heartland
The heart of the country is a limestone-floored lowland bounded on the south by the Armorican ridges and on the north and west by the Caledonian mountains. This central lowland region represents the most extensive landform type in Ireland and has been fundamental to the country’s agricultural development.
The central plain, broken in places by low hills, is extensively covered with glacial deposits of clay and sand, and has considerable areas of bog and numerous lakes. The glacial deposits left behind after the last ice age created a varied landscape within the lowlands, with different soil types supporting different agricultural activities.
Peat Bogs: A Distinctive Lowland Feature
Peat bogs are swampy areas with partially decayed plant matter that can be dried for fuel, formed naturally about ten thousand years ago when glacier depressions formed and created thousands of tiny lakes, which eventually became bogs that developed in the basin of the River Shannon.
Ireland’s peat bogs represent a unique type of wetland ecosystem that has shaped both the landscape and human culture. There are two main types: raised bogs, which form in lowland areas where water accumulates, and blanket bogs, which develop in areas of high rainfall, typically on hillsides and plateaus. The central lowlands contain extensive raised bog systems, though many have been harvested for fuel over centuries.
These bogs serve multiple ecological functions beyond their historical use as fuel sources. They act as carbon sinks, storing vast amounts of carbon that would otherwise be released into the atmosphere. They also provide habitat for specialized plant species, including various mosses, sedges, and carnivorous plants adapted to the nutrient-poor, acidic conditions. Additionally, bogs preserve archaeological artifacts and even human remains, offering invaluable insights into Ireland’s past.
Drumlins: Glacial Legacy in the Landscape
There are gentle hills called drumlins created by glacial deposits in the northernmost section of the lowlands. Drumlins represent one of the most distinctive glacial landforms in Ireland, particularly abundant in counties such as Monaghan, Cavan, Leitrim, and Down.
These elongated, oval-shaped hills were formed beneath moving glacial ice sheets. As glaciers advanced across the landscape, they deposited sediment in streamlined mounds aligned with the direction of ice flow. The result is a characteristic “basket of eggs” topography, with numerous small hills creating an undulating landscape. Individual drumlins typically measure between 250 and 1,000 meters in length and rise 5 to 50 meters above the surrounding terrain.
Drumlin Fields and Land Use
The drumlin fields of Ireland create both challenges and opportunities for agriculture and settlement. The irregular terrain makes large-scale mechanized farming difficult, as fields must conform to the drumlin shapes. However, the well-drained slopes of drumlins provide good grazing land, and many drumlin areas have traditionally supported pastoral farming.
Settlement patterns in drumlin regions often reflect the topography, with farmsteads typically located on drumlin summits or upper slopes to avoid the wetter, poorly drained areas between drumlins. Roads wind through drumlin fields, following the natural contours rather than running in straight lines. This creates the characteristic winding road networks found in counties like Monaghan.
This drowned drumlin landscape was created by glacial action and subsequent sea level rise, as seen in Clew Bay, County Mayo, where drumlins were partially submerged as sea levels rose after the last ice age, creating a bay dotted with hundreds of small islands—each one a drumlin summit rising above the water.
Eskers: Ancient River Channels in Stone
Eskers represent another fascinating glacial landform found throughout Ireland’s countryside. These long, winding ridges of sand and gravel were deposited by meltwater streams flowing within or beneath glacial ice. As the ice melted away, these sediment deposits remained as elevated ridges snaking across the landscape.
Evidence of glacial activity is visible in the Esker Riada, one of Ireland’s most significant esker systems. The Esker Riada runs roughly east-west across the central lowlands, and historically served as an important routeway across the boggy midlands. In ancient times, when much of the central plain was difficult to traverse due to bogs and wetlands, the well-drained esker ridges provided natural highways.
Characteristics and Formation
Eskers typically range from a few meters to over 30 meters in height and can extend for many kilometers. Their composition of sand and gravel makes them well-drained and stable, contrasting sharply with the surrounding boggy terrain. This excellent drainage has made eskers valuable for various human uses throughout history.
The formation process began as meltwater streams carved tunnels through or beneath glacial ice, depositing sediment along their courses. As the climate warmed and glaciers retreated, these sediment-filled tunnels were left behind as ridges. The sinuous, winding nature of eskers reflects the meandering courses of the meltwater streams that created them.
Modern Uses of Esker Landforms
Today, eskers continue to serve important functions in the Irish landscape. Their well-drained gravel composition makes them valuable sources of aggregate for construction. Many eskers have been quarried for sand and gravel, though this has raised conservation concerns as eskers represent important geological heritage sites and unique ecosystems.
The natural drainage and elevation of eskers have made them preferred locations for roads, railways, and settlements in areas where the surrounding land is wet or boggy. Some modern roads follow ancient routes along esker ridges, maintaining transportation corridors that have been in use for thousands of years.
Mountain Ranges and Coastal Highlands
While not typically classified as rural landforms in the same sense as valleys and plateaus, Ireland’s mountain ranges form the dramatic backdrop to much of the countryside and significantly influence rural land use patterns. Ireland’s main geographical features include low central plains surrounded by coastal mountains, creating distinct regional characteristics.
The MacGillycuddy’s Reeks
The MacGillycuddy’s Reeks, composed of old red sandstone, include Carrauntoohil, Ireland’s highest peak at 1,038 meters (3,406 feet). Located in County Kerry, this mountain range represents Ireland’s most dramatic upland terrain. The sandstone composition creates distinctive reddish-brown peaks that contrast with the green valleys below.
The steep slopes and high elevation of the MacGillycuddy’s Reeks limit agricultural use, though lower slopes support sheep grazing. The mountains attract significant tourism, with hillwalking and mountaineering being popular activities. The surrounding valleys benefit from the mountains’ influence on local climate and water resources, with numerous streams flowing down from the peaks to support agriculture in the lowlands.
The Wicklow Mountains
The Wicklow Mountains to the east are primarily granite formations, with Lugnaquilla reaching 925 meters (3,035 feet). This mountain range extends south from Dublin, creating a significant upland area on Ireland’s east coast. The granite bedrock creates distinctive rounded peaks and has weathered to produce acidic soils that support heathland vegetation.
The Wicklow Mountains have long served as a refuge and wilderness area close to Ireland’s capital city. The uplands contain important water catchment areas that supply Dublin with drinking water. Forestry plantations cover significant portions of the lower slopes, while the higher elevations remain as open moorland grazed by sheep.
The Donegal Highlands
The north features the basaltic Antrim Plateau and the rugged quartzite peaks of the Donegal Mountains. The Donegal highlands represent some of Ireland’s most remote and rugged terrain, with quartzite peaks creating sharp, angular mountain profiles. The isolation and challenging terrain have preserved traditional land use patterns in many areas, with small-scale farming and sheep grazing remaining important activities.
Hills and Upland Areas
Between the dramatic mountain ranges and the flat lowlands lie numerous hill regions that contribute significantly to Ireland’s rural character. These areas typically range from 150 to 500 meters in elevation and support a mix of agricultural activities.
Less than 5% of the island lies above 500 metres, and well over 80% is below 200 metres, therefore in many parts of the country, relief is quite subdued. This relatively gentle topography has facilitated agricultural development across much of the country, with even upland areas remaining accessible for farming activities.
Hill regions often mark transitions between different geological zones, with varied rock types creating diverse soil conditions. This geological diversity supports different vegetation types and agricultural uses. Some hill areas have been developed for forestry, while others remain as improved pasture or rough grazing land.
Coastal Landforms and Their Rural Connections
The coastline is notably rugged and heavily indented along the south and west, where mountain ranges terminate in bold headlands and rocky islands, forming long, narrow fjord-like inlets and wide-mouthed bays. These coastal features create unique rural landscapes where farming communities have adapted to challenging conditions.
Peninsulas and Coastal Valleys
Ireland’s western and southern coasts feature numerous peninsulas where mountain ranges extend into the Atlantic Ocean. The Dingle Peninsula, Iveragh Peninsula, and Beara Peninsula in the southwest create dramatic landscapes where steep-sided valleys run perpendicular to the coast, creating sheltered harbors and fertile pockets of agricultural land.
These coastal valleys often have milder climates than inland areas due to the moderating influence of the ocean. This allows for specialized agriculture, including early potato production and, in some areas, subtropical plant species that cannot survive in colder inland regions. The combination of mountains, valleys, and coastline creates spectacular scenery that supports tourism alongside traditional farming.
Coastal Plains and Machair
In contrast to the rugged western peninsulas, some coastal areas feature flat or gently sloping plains. The eastern coast, in particular, has more uniform terrain with fewer dramatic features. These coastal plains have been important agricultural areas, with fertile soils supporting crop production and dairy farming.
In the northwest, particularly in Donegal and parts of the west coast, machair landscapes occur—low-lying fertile plains formed from shell sand blown inland from beaches. These unique coastal grasslands support distinctive plant communities and have been used for centuries for grazing and cultivation using traditional methods.
The Influence of Geology on Landform Development
Ireland’s geological history includes a wide range of elements, from volcanism and tropical seas to the last glacial period. Understanding this geological history is essential to comprehending the diverse landforms visible in the Irish countryside today.
Ancient Geological Foundations
Ireland was formed in two distinct parts, which slowly joined, uniting about 440 million years ago. This ancient collision created fundamental geological structures that still influence the landscape. The joining of these two landmasses created zones of weakness and folding in the rock that later erosion would exploit, helping to shape valleys and other features.
Different rock types weather and erode at different rates, creating varied topography. Resistant rocks like granite and quartzite form uplands and mountains, while softer rocks like limestone erode more easily, creating lowlands and valleys. This differential erosion has been fundamental in creating Ireland’s bowl-shaped topography, with resistant rocks forming the coastal mountains and softer limestone creating the central lowlands.
Glacial Reshaping
The island has seen at least two general glaciations, with the most recent ending approximately 10,000 years ago. These glacial periods fundamentally reshaped the Irish landscape, smoothing some features while accentuating others. Glaciers deepened existing valleys, deposited vast quantities of sediment, and created entirely new landforms like drumlins and eskers.
The legacy of glaciation is visible throughout the Irish countryside. Erratic boulders—large rocks transported far from their source by glacial ice—dot the landscape. Glacial till—unsorted sediment deposited directly by ice—covers much of the lowlands, creating the parent material for many Irish soils. Glacial meltwater carved channels and deposited sorted sediments, creating features like eskers and kames.
Climate and Its Influence on Landforms
The influence of the North Atlantic Current ensures the coastline of Ireland remains ice-free throughout the winter. Ireland’s temperate oceanic climate, moderated by the Atlantic Ocean and the North Atlantic Current, creates conditions that continue to shape landforms through weathering and erosion.
Rainfall is a particularly prominent part of western Irish life, with Valentia Island, off the west coast of County Kerry, getting over twice as much annual rainfall as Dublin on the east (1,557 mm or 61.3 in vs. 714 mm or 28.1 in). This high rainfall, particularly in western and upland areas, drives ongoing erosion and weathering processes. Rivers continue to deepen their valleys, though at imperceptible rates compared to glacial erosion. Chemical weathering of limestone creates karst features, while physical weathering breaks down exposed rock on mountain summits.
The mild, wet climate also supports the development and maintenance of peat bogs, which continue to grow slowly in areas where conditions remain suitable. However, climate change and human activities are altering these processes, with some bogs drying out while others remain active.
Human Modification of Rural Landforms
While natural processes created Ireland’s fundamental landforms, human activity has significantly modified the rural landscape over thousands of years of settlement and agriculture. Understanding these modifications provides insight into the interaction between people and landscape in rural Ireland.
Agricultural Terracing and Field Systems
In hilly and mountainous areas, farmers have created terraces and modified slopes to make land more suitable for cultivation and grazing. Ancient field systems, some dating back thousands of years, remain visible in upland areas, showing how communities adapted to challenging terrain. Stone walls built from cleared field stones create the characteristic patchwork of small fields that defines much of the Irish countryside.
Drainage systems have been installed across lowland areas to make boggy land suitable for agriculture. Networks of ditches and drains lower water tables, converting wetlands into productive farmland. While this has increased agricultural productivity, it has also led to the loss of significant bog areas and altered natural drainage patterns.
Peat Extraction and Landscape Change
Centuries of peat cutting for fuel have dramatically altered bog landscapes in many areas. Traditional hand-cutting created distinctive patterns of trenches and banks, while modern industrial peat extraction has removed entire bog systems, leaving behind flat, bare landscapes. Some cutaway bogs are being rehabilitated for conservation or alternative uses, including forestry and renewable energy production.
Quarrying and Mining
Extraction of stone, gravel, and minerals has created artificial landforms throughout rural Ireland. Quarries excavated into hillsides and eskers have removed natural features while creating new topography. Some abandoned quarries have been repurposed as lakes or wildlife habitats, while others remain as scars on the landscape.
Ecological Significance of Rural Landforms
Ireland’s diverse landforms support varied ecosystems, each with characteristic plant and animal communities adapted to specific conditions. Understanding these ecological relationships helps explain the importance of preserving landform diversity.
Upland Ecosystems
Mountain and hill areas support heathland and moorland ecosystems dominated by heather, gorse, and grasses adapted to acidic soils and exposed conditions. These uplands provide habitat for birds like red grouse, meadow pipits, and skylarks, as well as mammals including Irish hares and, in some areas, red deer. The open character of upland landscapes makes them important for species that require extensive territories.
Wetland and Bog Ecosystems
Peat bogs and other wetlands support specialized plant communities including sphagnum mosses, cotton grass, and carnivorous plants like sundews and butterworts. These nutrient-poor environments have selected for species with unique adaptations. Bogs provide important habitat for breeding birds including curlews, golden plovers, and snipe, as well as insects like dragonflies and damselflies.
Limestone Landscapes
Areas with limestone bedrock, including the Burren and limestone plateaus, support distinctive flora adapted to alkaline soils and, in some cases, exposed rock surfaces. The Burren is particularly famous for its unusual combination of Arctic-alpine plants, Mediterranean species, and typical Irish flora growing in close proximity—a result of the unique microhabitats created by the limestone pavement topography.
Conservation and Management of Rural Landforms
Recognizing the importance of Ireland’s diverse landforms for ecology, heritage, and landscape character has led to various conservation initiatives. Many significant landforms are protected within national parks, nature reserves, and designated conservation areas.
The Wicklow Mountains National Park protects upland landscapes including glacial valleys, mountain peaks, and blanket bogs. The Burren and Cliffs of Moher UNESCO Global Geopark recognizes the geological and geomorphological significance of the Burren’s limestone landscape. Numerous Special Areas of Conservation (SACs) protect specific landforms and their associated ecosystems, including raised bogs, limestone pavements, and coastal features.
Sustainable management of rural landforms requires balancing conservation with continued agricultural use and other human activities. Agri-environment schemes encourage farmers to manage land in ways that protect landscape features, maintain traditional field patterns, and preserve important habitats. These programs recognize that many of Ireland’s valued landscapes result from centuries of human interaction with natural landforms.
Tourism and Recreation on Rural Landforms
Ireland’s diverse landforms attract visitors seeking outdoor recreation and scenic beauty. Walking and hiking trails traverse mountains, valleys, and coastal areas, providing access to spectacular landscapes. The Wild Atlantic Way, a coastal touring route, showcases the dramatic interaction between land and sea along Ireland’s western coast, highlighting cliffs, headlands, bays, and islands.
Mountain ranges like the MacGillycuddy’s Reeks and the Wicklow Mountains attract hillwalkers and climbers. Valleys like Glendalough combine natural beauty with historical sites, drawing visitors interested in both landscape and heritage. The unique landscapes of the Burren and the Giant’s Causeway have become iconic tourist destinations, contributing significantly to local economies.
Recreational use of rural landforms must be managed to prevent damage to sensitive environments. Popular walking routes can suffer from erosion, requiring path maintenance and visitor management. Balancing public access with conservation remains an ongoing challenge in many areas.
The Future of Ireland’s Rural Landforms
Ireland’s rural landforms continue to evolve through natural processes and human influences. Climate change is altering precipitation patterns, potentially affecting erosion rates, bog development, and vegetation patterns. Rising sea levels threaten coastal landforms, particularly low-lying areas and coastal wetlands.
Land use changes, including agricultural intensification in some areas and abandonment in others, are reshaping rural landscapes. Forestry expansion is changing the character of upland areas, while renewable energy development, particularly wind farms, is creating new features in the landscape. Urban expansion continues to consume agricultural land around growing towns and cities.
Understanding and appreciating Ireland’s diverse rural landforms—from fertile valleys to elevated plateaus, from glacial drumlins to ancient eskers—provides insight into the forces that have shaped this island and continue to influence it today. These landforms are not merely scenic backdrops but active components of functioning ecosystems, productive agricultural landscapes, and cultural heritage that connects present communities to thousands of years of human interaction with the Irish countryside.
For those interested in learning more about Ireland’s geography and landforms, resources such as the Ordnance Survey Ireland provide detailed mapping and geographical information, while the Geological Survey Ireland offers insights into the geological processes that created these features. The National Parks and Wildlife Service manages many protected areas that showcase Ireland’s landform diversity, and organizations like Heritage Ireland interpret the cultural significance of these landscapes. Academic institutions including Trinity College Dublin’s Department of Geography conduct ongoing research into Irish geomorphology and landscape evolution, contributing to our understanding of these remarkable landforms.
The Irish countryside’s valleys, plateaus, drumlins, eskers, and other landforms represent a geological and geographical heritage millions of years in the making. They provide the foundation for agriculture, shape patterns of settlement, support diverse ecosystems, and create the distinctive landscapes that define Ireland’s character. Preserving and sustainably managing these landforms ensures that future generations can continue to benefit from and appreciate the remarkable diversity of Ireland’s rural geography.