Greenland is a place of stark visual contrasts: a vast white ice sheet covering most of the interior, ringed by rocky coastlines cut with deep fjords, clusters of brightly painted houses, and patches of low-growing tundra that turn green and purple in summer. It looks nothing like the featureless white expanse most people imagine. The ice is real and enormous, but the 20 percent of land not buried under it holds some of the most dramatic scenery on Earth.
The Ice Sheet Dominates the Interior
About 80 percent of Greenland sits beneath a single continuous ice sheet stretching across 1.7 million square kilometers, an area roughly three times the size of Texas. At its thickest point, the ice is over 3 kilometers (1.9 miles) deep. From above, the interior looks like an endless white plateau, gently domed in the center and sloping toward the edges. The surface isn’t smooth. Wind sculpts it into ridges and ripples, and in summer, vivid blue meltwater rivers and lakes appear on top of the ice, snaking across the white surface before plunging into deep vertical shafts called moulins.
At the edges, the ice sheet breaks apart dramatically. Glaciers flow outward through mountain gaps and pour into fjords, where enormous chunks calve off into the sea as icebergs. The Ilulissat Icefjord on the west coast is one of the most visually striking places on the planet: a river of broken ice stretching to the horizon, with icebergs the size of apartment buildings drifting slowly toward open water. The ice itself ranges from brilliant white to deep blue, depending on how compressed and air-free it is.
Fjords, Mountains, and Rocky Coastline
Greenland’s coastline is one of the most deeply carved on Earth. Hundreds of fjords slice inland, flanked by sheer rock walls that rise hundreds or thousands of feet from dark water. The Scoresby Sund system on the east coast is among the largest fjord systems in the world, a sprawling network of deep channels and branching inlets surrounded by jagged peaks. In winter, sea ice fills many of these fjords, turning them into flat white corridors between dark cliffs.
The tallest mountains cluster along the east coast in the Watkins Range, where Gunnbjørn Fjeld reaches about 3,700 meters (12,139 feet), the highest point in the Arctic. Climbers who have approached these peaks describe massive basalt cliffs, knife-edged snow ridges, and unstable icefalls. The mountains are raw and angular, shaped by glaciers rather than smoothed by time. Along the west and southwest coasts, the terrain is gentler: rolling hills, exposed bedrock polished by ancient ice, and wide valleys that open to the sea.
Colorful Towns With No Roads Between Them
Greenland’s settlements are small and visually distinctive. Houses are painted in bold reds, yellows, blues, greens, and blacks, scattered across rocky hillsides overlooking the water. This color-coding dates to the 18th century colonial period, when wooden houses arrived from Scandinavia as timber kits. With no street names or house numbers, each color identified a building’s purpose: red for churches, schools, and ministers’ houses; yellow for hospitals and doctors; blue for fish factories; green for telecommunications; black for police stations. The system is no longer strictly followed, but the tradition stuck, and today the clusters of bright houses against grey rock and white snow are one of Greenland’s most recognizable visual features.
There are virtually no roads connecting one town to another. Until 2025, there was no land-based route between any two settlements capable of handling vehicles. That year, a 130-kilometer track opened between Sisimiut and Kangerlussuaq, passable only by all-terrain vehicles. Otherwise, people travel between towns by helicopter, small plane, or boat. In the north and east, dog sleds are still used in winter. This isolation means each town sits alone in the landscape, a small patch of color surrounded by wilderness.
Tundra That Blooms in Summer
The ice-free coastal margins are covered in Arctic tundra, and in summer they’re surprisingly green. The most common plant community is dwarf shrub heath: low carpets of crowberry, Arctic blueberry, dwarf birch, willow, and heather that grow between 10 and 50 centimeters tall. These plants hug the ground to survive the wind, creating a dense, textured mat that shifts from bright green to deep red and orange in autumn. Mosses, lichens, and fungi fill the gaps between shrubs, and wildflowers appear in brief, vivid bursts during the long summer days.
In sheltered valleys in the south, vegetation grows thick enough to resemble subarctic meadows. A few areas even support small farms with sheep grazing on green hillsides, a scene that looks more like Iceland or Norway than the frozen wasteland people expect. The contrast between these lush pockets and the ice sheet visible on the horizon is one of the most striking things about Greenland’s appearance.
Light That Changes Everything
What Greenland looks like depends enormously on when you see it. In the far north, the midnight sun is visible from late April through late August, meaning the landscape is bathed in continuous golden light for months. Near the Arctic Circle, the sun stays above the horizon from early June to mid-July. During these weeks, shadows stretch endlessly across the ice, fjord water glows in shades of pink and orange, and the sky never fully darkens.
In winter, the opposite happens. The polar night brings weeks of near-total darkness, and the landscape is visible mainly by moonlight reflecting off snow and ice. From late August through April, the northern lights are frequently visible, painting the sky in green, purple, and blue. East Greenland, where jagged peaks and fjords frame the sky, is considered one of the best places in the world to watch the aurora. The combination of dark mountains, ice-filled fjords, and rippling light overhead creates scenes that look almost surreal.
A Landscape That Is Visibly Changing
Greenland has been losing ice every year since the late 1990s. In 2025, the ice sheet lost an estimated 129 billion metric tons of ice, less than the recent annual average of about 219 billion tons but still a continuation of the long-term trend. Glaciers are retreating, exposing rock that hasn’t been visible for thousands of years. New patches of brown and grey bedrock are appearing at the ice sheet margins, and coastal areas are seeing changes in shoreline shape as meltwater runoff increases.
If you visited certain fjords a decade ago and returned today, you’d notice the glaciers have pulled back, leaving fresh rubble and sediment where ice used to be. The visual transformation is slow on a human timescale but unmistakable over years. Greenland still looks overwhelmingly like a world of ice, rock, and water, but the balance between those elements is shifting in real time.