Northeast Greenland National Park | Exploring the World's Largest Protected Wilderness
Northeast Greenland National Park is a land of extremes — vast, silent, and overwhelmingly wild. Covering over 972,000 square kilometres, it is the largest national park in the world, a sanctuary of towering fjords, ancient glaciers, and fragile tundra ecosystems. Here, nature unfolds on a scale few places on Earth can match.
Yet despite its enormity, the park’s true power lies in its silence, its fragility, and the lessons it offers about resilience — both of the land and the Indigenous cultures who’ve called it home for millennia.
How big is Northeast Greenland National Park?
How big exactly is 972,000 square kilometres? Big enough to swallow entire countries. The Park is large enough to fit around 100 Yellowstone National Parks and is roughly the size of France and Spain combined.
Being the northernmost National Park in the world, it covers the entire north-eastern quarter of Greenland. The Greenland Ice Sheet covers around 80% of the Park’s area. Created in 1974 and designated a UNESCO Biosphere Reserve just three years later, this park isn’t just a sanctuary — it’s a scale of wilderness that’s hard to grasp.
Who lives in Northeast Greenland National Park?
Human presence in the Park is sparse, with only around 40 permanent residents. The number of sled dogs in it is more than the number of humans. There are around 400 sites in the Park that are used in summer by scientists and temporary researchers. Most of these are located on the ice-free coastal belt. Beyond that, there are a few weather stations, research stations, and military outposts.
Most winter residents in the Park are military personnel attached to the Sirius Dog Sled Patrol - a Danish naval unit responsible for maintaining Danish sovereignty over northern Greenland. Apart from them, sealers and hunters from Ittoqqortoormiit, a remote Inuit village with a population of around 450 residents, are the only people allowed to access and hunt inside the Park.
The Inuit have survived in this rugged terrain for thousands of years. As one of the few remaining subsistence hunting cultures on the planet, their way of life depends on free movement across land and sea ice to access essential resources. Their survival is closely tied to the rhythms of Arctic wildlife, and their knowledge of the environment has been shaped by generations of living off the land in harmony with its cycles.
Regions of the park
Northeast Greenland National Park spans the island’s entire northeastern corner, bordered by the Avannaata municipality to the west and Sermersooq to the south. Its coastline is long, jagged, and wild — carved by some of the Arctic’s most spectacular fjord systems.
While much of the park is dominated by ice and high plateaus, several key ice-free regions support unique landscapes and wildlife. These include Peary Land in the far north, Jameson Land in the southeast, and the narrow coastal belt where Arctic tundra meets the sea.
Rugged mountain ranges like the Roosevelt Range, Stauning Alps, and Halle Range rise near the coast, framing deep fjords such as Scoresbysund, Kong Oscar Fjord, and Kejser Franz Joseph Fjord. Glaciers flow from the interior toward the ocean, including the fast-moving Northeast Greenland Ice Stream (NEGIS) and frequently calving glaciers like The Gully, Sefstrøm, and Hamberg Glacier.
Peary Land: Arctic desert and polar legend
Peary Land is one of the northernmost land areas on Earth - a remote Arctic desert marked by deep fjords and rugged mountains that rise as high as 1,950 meters. Located in the far north of the park, it covers around 57,000 square kilometres, and is crossed by the largest river in Greenland, the Børglum River.
The area was named after American explorer Robert E. Peary, who traversed the region during his 1891–1892 Greenland expedition in search of the North Pole. At the time, it was believed that Peary Land was an island. Knud Rasmussen's 1912 expedition established the fact that it is a peninsula connected to the mainland.
Though uninhabited today, Peary Land holds evidence of early human presence. Archaeological finds — including boat frames and hunting tools discovered along Herlufsholm Strand — suggest it was once a migration route for Inuit ancestors. One of the most significant sites is Deltaterrasserne, a terraced stone structure near Jørgen Brønlund Fjord dating back to 2,050–1,750 BC.
In the 1990s, the region also gained attention for its mineral resources, with the discovery of large zinc and lead deposits near Citronen and Navarana fjords — the northernmost such reserves on the planet.
Jameson Land: Fossils, wildlife and gateway to the Eastern Arctic
Jameson Land is a strikingly diverse region in the southeastern corner of the park. Bordered by the towering Stauning Alps to the north and the vast Scoresbysund fjord system to the south, it transitions from rugged mountains to broad lowland tundra.
This varied landscape supports one of the richest concentrations of wildlife in East Greenland, particularly musk oxen, which thrive in its open terrain. It’s also home to Arctic foxes, hares, and a variety of tundra birds (Snow Bunting, Red Knot, Dunlin, Rock Ptarmigan just to name a few) during the summer months.
But Jameson Land’s importance lies below the surface as well. Its sedimentary rock formations are a treasure trove for paleontologists. Fossils of small and medium-sized vertebrates from the late Triassic period have been found here, offering a window into a prehistoric ecosystem more than 200 million years old. The region is considered one of the most fossiliferous areas in Greenland.
Today, Jameson Land is also the most accessible part of Northeast Greenland National Park. The Constable Point (Nerlerit Inaat) airstrip, just 40 kilometres from Ittoqqortoormiit, serves as the main gateway for researchers and expedition travellers arriving by air before joining vessels that explore Scoresbysund and the broader national park.
Scoresbysund: The world’s largest fjord system
Scoresbysund, or Scoresby Sund, forms the southeastern boundary of Northeast Greenland National Park — and stands as one of the most awe-inspiring natural features in the Arctic. Stretching across 38,000 square kilometres, Scoresbysund is the planet’s largest fjord system, with branching waterways that reach deep into Greenland’s mountainous interior.
Despite its remote location, Scoresbysund is the most accessible part of the park for expedition travellers. The nearby Inuit settlement of Ittoqqortoormiit, perched near the fjord’s mouth, offers the only permanent human presence in the region. Most visitors arrive by ice-strengthened ship during the brief Arctic summer, exploring this landscape of ice and stone under the midnight sun.
Scoresbysund is also a hotspot for Greenland wildlife. Musk oxen graze along the tundra slopes, Arctic foxes dart between rocks, and bird cliffs host nesting kittiwakes, fulmars, and little auks. In the fjord’s deep waters, visitors may glimpse narwhals, belugas, or even the elusive bowhead whale, which relies on the region’s seasonal polynyas for open water access.
Geologically, the fjord system is a showcase of Earth's deep time — with exposed basalt cliffs, ancient gneiss formations, and sedimentary layers that preserve traces of long-extinct ecosystems. For scientists, photographers, and explorers alike, Scoresbysund offers one of the most breathtaking and revealing windows into Greenland’s eastern wilderness.
Scattered across Northeast Greenland National Park are numerous sites of geological, historical, or ecological significance — many of which are accessible only by expedition vessel and visited by a fortunate few. These places offer glimpses into the park’s human history, unique geology, and vibrant yet fragile ecosystems.
Explore the many regions on Northeast Greenland National Park on an Expedition Micro Cruise
Photogenic Fjords and Scenic Highlights
Ofjord
Located deep inside the Scoresbysund system, Ofjord or Øfjord, which means 'Island Fjord', is a spectacular fjord. It is a paradise for photographers and presents dramatic views of icebergs and towering cliffs.
Segelsällskapet Fjord
This is a fjord in the King Christian X Land and was named by Alfred Gabriel Nathorst in 1899. The fjord is bordered by steep peaks that rise to around 2,000 metres above the water. One striking feature in the fjord is the striped cliffs made of layered sedimentary rocks. Multiple glaciers, including the Sedgwick Glacier, terminate here.
Wildlife Viewing and Landing Sites
Bear Islands
Bear Islands or Bjørne Øer are a cluster of rocky islands at the northern end of Scoresbysund and the mouth of Ofjord. The islands are not named but are marked by numbers from I to XI.
Sydkap
Sydkap is a low-lying landing area in the Scoresbysund system. Short hiking trails around the area lead to some stunning viewpoints and allow you to observe a variety of tundra flora. The area offers stunning views of the mirror-like blue waters and icebergs of Hall Bredning, a wide portion of Scoresbysund. There is also a high chance of observing Arctic wildlife in the area.
Blomsterbugt
The Blomsterbugt, often called the ‘flower bay’, is a landing site known for its Arctic flora and striking geological formations. It is a part of the King Oscar Fjord system and has a beautiful lake offering fantastic views of the surrounding area.
Historic Outposts and Cultural Traces
Antarctic Havn
Antarctic Havn is a landing site in a natural harbour that was also a Norwegian hunting station in the 1930s. The remains of the older station are still seen lying around. A memorial to Norwegian explorer Helge Ingstad also stands close to the building.
Holm Bugt
Holm Bugt is a picturesque bay with a sandy beach in the Kong Oscar Fjord area. It has an old trapper's cabin and some archaeological remains of Thule culture.
Glacier-Studded Fjords and Peaks
Kong Oscar Fjord
King Oscar Fjord is a major fjord on the northern border of Scoresbysund and presents a grand view of mountains and glaciers. The fjord is one of the best places to observe giant icebergs from up close.
Kejser Franz Josephs Fjord
This is the world’s northernmost fjord system and has a length of around 200 kilometres. It has branches like the Dusénfjord, Nordfjord, Moskusoksefjord, and Geologfjord, and the total system covers around 500 kilometres. The views are spectacular, and this is also a great place for observing Greenlandic wildlife.
Teufelsschloss
Teufelsschloss, or the Devil’s Castle, is a prominent mountain that rises to a height of 1,500 metres above the Kaiser Franz Joseph Fjord. It was named by the second German North Polar Expedition in 1869–70.
Raffles
Raffles Island (Danish name Raffles Ø) is an uninhabited island in the Scoresbysund area. Arctic explorer William Scoresby, during his Greenland voyage of 1822, named the island after the British minister Thomas Raffles.
Wildlife of Greenland National Park
Despite its harsh climate and extreme isolation, Northeast Greenland National Park is home to a remarkable diversity of wildlife. These remote ecosystems remain largely undisturbed, providing refuge for iconic Arctic species and a critical stronghold for Greenland’s terrestrial and marine life.
Land Mammals
The park hosts around 40% of the world’s musk oxen, making it one of the best places to observe these shaggy Ice Age survivors in their natural habitat. Other land mammals include Arctic foxes, Arctic hares, Arctic wolves, collared lemmings, and ermines. Reindeer were introduced in Greenland in 1952, and the Park has a sizable reindeer population at present.
Birdlife
The cliffs and mountains in the Park host large bird colonies, even though they are smaller than the colonies in West Greenland. Common seabirds that form colonies are the Arctic tern, glaucous gull, ivory gull, black-legged kittiwake, fulmar and large colonies of the little auk.
In the tundra zones, species like the ruddy turnstone, red knot, dunlin and sanderling are common sights. Rock ptarmigan and ravens are among the few birds that remain year-round.
Marine Mammals
The icy waters along the park’s coastlines and fjords support all nine Arctic marine mammals, including: the walrus, polar bear, bearded seal, bowhead whale, beluga, narwhal, harp seal, ringed seal, and hooded seal. Polynyas in northeast Greenland, which are areas of open water surrounded by sea ice, are important habitats for the marine mammals, especially the walrus and bowhead whale.
Geology and legacy of the Lauge Koch
Beneath the ice and tundra of Northeast Greenland lies one of the oldest and most revealing geological records on the planet. The park showcases a timeline stretching back nearly 4 billion years, with ancient gneissic rocks exposed in its interior and fjord systems — some of them among the oldest formations ever found on Earth.
Layered on top of this ancient bedrock are younger sedimentary rocks, many of which date back to the Paleozoic and Mesozoic eras. These layers preserve a rich fossil record, including marine invertebrates, plant imprints, and even vertebrate remains in areas like Jameson Land. The result is a rare, nearly continuous window into Earth's geologic evolution, from the early formation of the continents to the rise of complex life.
Much of what we know about this landscape comes from the work of Lauge Koch, a Danish geologist and Arctic explorer whose career spanned from the 1920s to the 1950s. Through extensive mapping expeditions — often under brutal conditions — Koch helped chart the topography and rock formations of East Greenland with an unmatched level of detail for the time. His surveys laid the foundation for modern geological understanding of the region and produced some of the first accurate topographic maps of the Arctic.
To this day, geologists continue to build on Koch’s legacy. The park remains a focus for research on everything from plate tectonics and glacial history to the potential for rare earth mineral deposits.
Human history in the park: Inuit presence and cultural legacy
While Northeast Greenland National Park is almost entirely uninhabited today, archaeological discoveries reveal that it has been part of human life and movement for thousands of years. Sites in areas like Peary Land and Deltaterrasserne preserve the remnants of Paleo-Inuit migrations, including ancient hunting tools, tent rings, and boat frames — signs of a culture that adapted ingeniously to the Arctic’s unforgiving extremes.
These early traces connect the park to the broader story of Greenland’s Indigenous peoples. Skills honed over millennia — from hunting and navigation to clothing and shelter — remain essential for survival in the high Arctic and continue to shape life in nearby communities like Ittoqqortoormiit.
The Greenlandic-Danish explorer Knud Rasmussen helped preserve this cultural knowledge. Through his Thule Expeditions in the early 20th century, Rasmussen recorded oral histories, spiritual beliefs, and practical traditions from Inuit communities across the Arctic, many of whom had ancestral links to Northeast Greenland. His work offers a rare window into how people not only survived in the region, but thrived through close relationships with land, sea, and ice.
Alfred Wegener - shaping the science of ice and earth in Northeast Greenland
Northeast Greenland has long been a proving ground for polar science — and few figures shaped its legacy more than Alfred Wegener. Known today as the father of continental drift theory, Wegener proposed in 1912 that Earth’s continents were once joined in a supercontinent — which he called Pangaea — and had since drifted apart. At the time, the idea was radical and widely dismissed, but it later became the foundation of modern plate tectonics, transforming our understanding of Earth’s geology.
Before this theory gained recognition, Wegener had already made a name for himself through his polar fieldwork. During a series of expeditions to East Greenland in the early 20th century, he conducted pioneering studies of the Greenland Ice Sheet — collecting data on snowfall, temperature, ice thickness, and glacier flow. His goal was to understand the structure and behaviour of the ice, and how it interacted with the atmosphere and global systems.
Much of this work took place in areas that now lie within Northeast Greenland National Park. Wegener and his team faced brutal Arctic conditions to establish meteorological stations and carry out long-distance sledge journeys. These expeditions helped lay the groundwork for modern glaciology and cryospheric science, setting new standards for how researchers conduct science in extreme environments.
Today, the region continues to play a vital role in climate research. The park includes part of the Northeast Greenland Ice Stream (NEGIS) — one of the main outlets carrying ice from the interior to the North Atlantic. Monitoring this system is crucial for understanding glacier retreat, sea-level rise, and the global implications of a warming Arctic.
Wegener’s legacy is not only etched into scientific theory but also into the very ice and stone of Northeast Greenland — a landscape he helped decode and one that continues to shape our understanding of the planet.
Greenland’s minerals and the protected status of the National Park
Greenland has attracted increasing global interest in recent years for its strategic mineral resources, including rare earth elements, zinc, copper, and hydrocarbons. As global demand grows for critical minerals used in clean energy, defense, and electronics, Greenland’s largely untapped reserves have drawn attention from major powers — including past proposals from the United States to increase political influence in the region.
While most active exploration occurs in southern and western Greenland, parts of the northeastern region — including Jameson Land and Citronen Fjord in Peary Land — contain known deposits of zinc, lead, and other industrial minerals. The Citronen project, in particular, represents one of the northernmost base metal deposits on Earth.
However, much of this mineral-rich terrain falls within the boundaries of Northeast Greenland National Park — the largest protected area in the world. As a UNESCO Biosphere Reserve, the park is governed by strict environmental regulations, and any commercial exploitation is subject to rigorous assessments, if permitted at all.
For now, this region remains a rare example of Arctic territory where scientific research and environmental protection take priority over resource development — offering a case study in how to balance national interests with ecological preservation in a changing geopolitical climate.
Accessing Northeast Greenland National Park
Access to Northeast Greenland National Park is extremely limited due to its size, isolation, and lack of infrastructure. There are no roads, harbours, or settlements within the park’s interior, and the region remains ice-covered or inaccessible for most of the year.
For scientific expeditions, small aircraft and helicopter support are occasionally used to reach inland research stations during summer, using gravel airstrips such as the one at Constable Point (Nerlerit Inaat) in Jameson Land — the closest public airfield to the park.
For most travellers, the park is accessed via ice-strengthened expedition vessels during the short Arctic summer, when sea ice conditions allow safe navigation. While some ships depart directly from Iceland, Secret Atlas offers a faster route via charter flights to Constable Point (Nerlerit Inaat) in Jameson Land — the closest public airfield to the park. From there, guests board the ship and begin their voyage into the remote fjords of Northeast Greenland.
Visits are strictly regulated. The park is classified as a ‘remote part of Greenland’, and entry requires a permit from the Greenland government. All expeditions must adhere to environmental guidelines and travel with experienced guides familiar with local conditions.
While reaching the park is a challenge, the reward is profound: access to one of the last truly wild regions on Earth, where landscapes remain unmarked by roads, buildings, or modern infrastructure — and the journey is part of the experience.
When to visit
The best time to visit the world’s largest National Park is during the Arctic summer, between the months of late June and early September. The summers are warmer, and the 24-hour daylight makes it the ideal time for exploration. This is also the period when the Arctic wildlife, migratory birds and whales remain the most active.
By late September, the first signs of sea ice begin to return — transforming the landscape into a shifting mosaic of water, light, and frost. Days grow shorter, sunsets stretch longer, and the Northern Lights may begin to dance across the night sky. While conditions can become more challenging for navigation, this time of year offers a uniquely dramatic and photogenic Arctic experience — quieter, colder, and full of contrast.
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