Alaska Physical Map

Prepared for educational and reference requirements, the Alaska Physical Map offers an easy-to-understand view of geographic boundaries and locations, useful for analyzing regional connections and planning activities. Offline usage of this Alaska Physical Map is supported through the Download Now option under the map.

Alaska Physical Map

About Alaska Physical Map

Explore physical map of Alaska state of United States showing geographical / physical features with rivers, landforms, mountains, plateau, peaks, lakes, etc.


Major Rivers of Alaska

Rank River Length (mi) Length (km) Source Mouth Drainage Area (sq mi) Drainage Area (sq km) Average Discharge (cfs) Notable Facts
1 Yukon River 1980 3187 Llewellyn Glacier, British Columbia Bering Sea 328000 849880 225000 Transboundary; Third longest in US; Major salmon run; Gold rush route
2 Kuskokwim River 702 1130 Confluence of East Fork and North Fork, Kuskokwim Mountains Kuskokwim Bay, Bering Sea 48000 124320 67000 Ninth largest by discharge in US; Seventeenth by basin area; Subsistence fishing
3 Porcupine River 569 916 Ogilvie Mountains, Yukon Territory Yukon River 45100 116809 23000 Transboundary; Twentieth largest basin in US; Tributary of Yukon
4 Tanana River 584 940 Confluence of Chisana and Nabesna Rivers Yukon River 44000 113960 41000 Sixteenth by discharge in US; Drains Alaska Interior; Tributary of Yukon
5 Innoko River 500 805 Cloudy Mountain, Innoko National Wildlife Refuge Yukon River 13000 33670 6800 Meandering wetlands; Tributary of Yukon; Remote wilderness
6 Noatak River 425 684 Mount Igikpak, Brooks Range Chukchi Sea 12600 32634 16700 Wild and Scenic River; Noatak National Preserve; Arctic ecosystem
7 Koyukuk River 425 684 Endicott Mountains, Brooks Range Yukon River 32000 82880 14500 Gates of the Arctic National Park; Tributary of Yukon; Indigenous lands
8 Colville River 350 563 De Long Mountains, Brooks Range Beaufort Sea 20700 53613 14000 North Slope Borough; Oil production region; Arctic tundra
9 Susitna River 313 504 Susitna Glacier, Alaska Range Cook Inlet 20000 51800 51000 Fifteenth largest by discharge in US; Glacial fed; Southcentral Alaska
10 Copper River 290 470 Copper Glacier, Wrangell Mountains Gulf of Alaska 24000 62160 57400 Tenth largest by discharge in US; World-class salmon fishery; Delta ecosystem
11 Kobuk River 280 451 Endicott Mountains, Brooks Range Chukchi Sea 12100 31339 13600 Kobuk Valley National Park; Caribou migration; Indigenous cultural sites
12 Nushagak River 242 389 Nushagak Lakes, Aleutian Range Bristol Bay, Bering Sea 13400 34706 36000 Major sockeye salmon producer; Bristol Bay watershed; Commercial fishing
13 Alsek River 240 386 Kluane National Park, Yukon Territory Dry Bay, Gulf of Alaska 10800 27972 64000 Transboundary; Glacier Bay National Park; Rafting destination
14 Stikine River 379 610 Stikine Plateau, British Columbia Eastern Passage, Alexander Archipelago 20000 51800 56000 Transboundary; Fourteenth largest by discharge; Salmon and wildlife habitat
15 Nowitna River 250 402 Kuskokwim Mountains Yukon River 4700 12173 2900 Nowitna National Wildlife Refuge; Clear water; Canoeing route


Major Lakes of Alaska

Lake Name Surface Area (km²) Surface Area (mi²) Maximum Depth (m) Maximum Depth (ft) Elevation (m) Basin / Region Notable Feature / Use
Iliamna Lake 2,589 1,000 301 988 15 Bristol Bay / Alaska Peninsula Largest lake in Alaska; significant sockeye salmon fishery
Becharof Lake 1,186 458 ~88 ~289 4 Alaska Peninsula Second-largest lake; important for waterfowl and salmon
Teshekpuk Lake 826 319 ~6 ~20 3 North Slope (National Petroleum Reserve) Shallow coastal lake; major waterfowl molting area
Naknek Lake 617 238 ~110 ~360 11 Katmai National Park Deep glacial lake; famous for brown bear fishing at Brooks Falls
Clark Lake ~330 ~127 ~30 ~98 ~80 Interior Alaska Large interior lake; important for subsistence fisheries
Minchumina Lake ~300 ~116 ~18 ~59 ~210 Interior (Minto Flats) Shallow wetland lake complex; critical migratory bird habitat
Chalkyitsik Lake ~290 ~112 ~10 ~33 ~130 Yukon Flats Large shallow lake; key for waterfowl and fish
Crosswind Lake ~250 ~97 ~15 ~49 ~480 Copper River Basin Glacial lake; supports trout and grayling
Lake Clark ~260 ~100 ~314 ~1,030 76 Lake Clark National Park Deep fjord-like lake; sockeye salmon spawning grounds
Tustumena Lake ~245 ~95 ~290 ~950 77 Kenai Peninsula Deep glacial lake; significant salmon runs


Mountain Ranges in Alaska

Range Name Length (km) Highest Peak Elevation (m) Elevation (ft) Primary Location / Region Geologic Age (Ma) Key Characteristics / Significance
Alaska Range ~650 Denali (Mount McKinley) 6,190 20,310 South-central Alaska Cenozoic (ongoing uplift) Highest range in North America; Denali is continent’s tallest peak; major arc of Pacific Ring of Fire
Brooks Range ~1,100 Mount Chamberlin 2,749 9,020 Northern Alaska (Arctic) Devonian–Cretaceous Northernmost major range in North America; forms Arctic continental divide; Arctic National Wildlife Refuge
Aleutian Range ~1,000 Redoubt Volcano 3,108 10,197 Southwest Alaska / Alaska Peninsula Cenozoic (active volcanism) Active volcanic arc; part of Aleutian subduction zone; frequent eruptions and seismic activity
Chugach Mountains ~480 Mount Marcus Baker 4,016 13,176 South-central Alaska (Prince William Sound) Cretaceous–Paleogene Extensive icefields and glaciers; Prince William Sound maritime influence; high precipitation
Wrangell Mountains ~160 Mount Blackburn 4,996 16,391 Southeast interior (Wrangell–St. Elias) Cenozoic (volcanic) Largest contiguous wilderness in U.S.; massive volcanic shield; extensive ice cover
Saint Elias Mountains ~300 Mount Saint Elias 5,489 18,008 Southeast Alaska / Yukon border Cenozoic (rapid uplift) Second-highest peak in Canada & U.S.; extreme relief; massive icefields; tectonic collision zone
Talkeetna Mountains ~200 Sovereign Mountain 2,646 8,682 South-central Alaska Jurassic–Cretaceous Northern extension of Chugach; rugged alpine terrain; important moose and caribou habitat
Kuskokwim Mountains ~550 Unnamed peak near Nixon Fork ~1,950 ~6,400 Interior / Southwest Alaska Paleozoic–Mesozoic Low-elevation range; gold and mineral deposits; Yukon–Kuskokwim lowlands transition
Endicott Mountains ~320 Mount Isto 2,736 8,976 Brooks Range (Arctic) Devonian–Mississippian Highest section of Brooks Range; Gates of the Arctic National Park; remote Arctic wilderness
Kenai Mountains ~200 Truuli Peak 2,095 6,875 Kenai Peninsula Cretaceous–Tertiary Glacier-covered; Harding Icefield; significant coastal precipitation and fjord formation


Mountain Peaks in Alaska

Peak Name Elevation (m) Elevation (ft) Prominence (m) Prominence (ft) Mountain Range Coordinates (Lat, Long) First Ascent Year Notable Feature / Status
Denali (Mount McKinley) 6,190 20,310 6,144 20,156 Alaska Range 63.0690°N 151.0074°W 1913 Highest peak in North America; active tectonic uplift; sacred to Indigenous peoples
Mount Saint Elias 5,489 18,008 3,429 11,250 Saint Elias Mountains 60.5025°N 140.9069°W 1897 Second-highest in both Canada and United States; extreme coastal relief; massive icefields
Mount Blackburn 4,996 16,391 3,539 11,613 Wrangell Mountains 61.7333°N 143.4333°W 1912 Highest volcanic peak in Wrangell–St. Elias; shield volcano with extensive glaciers
Mount Sanford 4,949 16,237 2,329 7,641 Wrangell Mountains 62.2167°N 144.1333°W 1939 Prominent volcanic summit; remote and heavily glaciated
Mount Marcus Baker 4,016 13,176 3,280 10,761 Chugach Mountains 61.8333°N 147.7167°W 1938 Highest peak in Chugach Mountains; extensive icefield source
Mount Bona 5,044 16,550 2,104 6,906 Saint Elias Mountains 61.3833°N 141.7500°W 1930 Fourth-highest in United States; massive ice-covered massif
Mount Lucania 5,226 17,146 3,046 9,993 Saint Elias Mountains 60.8667°N 140.6833°W 1937 Highest peak entirely in Canada; extreme isolation
Mount Fairweather 4,671 15,325 3,956 12,979 Fairweather Range 58.9167°N 137.5333°W 1931 Highest coastal peak in North America; extreme precipitation and glaciation
Mount Hubbard 4,577 15,015 2,437 7,995 Saint Elias Mountains 60.3167°N 139.6833°W 1891 Straddles Alaska–Yukon border; massive ice plateau
Mount Chamberlin 2,749 9,020 1,329 4,360 Brooks Range 69.2833°N 144.9167°W 1960s Highest peak in Brooks Range; Arctic wilderness


Plateau in Alaska

Plateau Name Approximate Area (km²) Average Elevation (m) Maximum Elevation (m) Primary Location / Region Geologic Age (Ma) Dominant Rock Type Key Characteristics / Significance
Yukon–Tanana Upland ~150,000 600–1,200 ~1,950 Interior Alaska (Yukon–Tanana region) Paleozoic–Mesozoic Metamorphic (schist, gneiss); intrusive granitic Largest upland plateau in Alaska; extensive gold placer deposits; dissected by Yukon and Tanana rivers
Arctic Foothills (Arctic Coastal Plain margin) ~80,000 150–600 ~1,200 North Slope (Brooks Range northern flank) Cretaceous–Tertiary Sedimentary (sandstone, shale); permafrost-dominated Transitional plateau between Brooks Range and Arctic Coastal Plain; critical caribou calving grounds; National Petroleum Reserve–Alaska
Kuskokwim Mountains Plateau ~60,000 400–1,000 ~1,950 Southwest Interior (Kuskokwim River basin) Paleozoic–Mesozoic Metamorphic and volcanic; intrusive plutons Low-relief dissected upland; significant mercury, antimony, and gold mineralization
Seward Peninsula Upland ~40,000 200–600 ~1,300 Western Alaska (Seward Peninsula) Paleozoic–Mesozoic Metamorphic (schist, marble); granitic intrusions Low-elevation plateau; Bering Land Bridge remnant; rich in placer gold and tin deposits
Interior Alaska Plateau (Tanana–Koyukuk Lowland margin) ~120,000 100–400 ~800 Central Interior (Tanana and Koyukuk basins) Cenozoic (alluvial fill) Unconsolidated sediment overlying older bedrock Broad lowland plateau; extensive permafrost and wetlands; major subsistence fisheries
Ray Mountains Plateau ~25,000 500–1,200 ~1,600 Interior (Dall River to Ray River) Paleozoic–Mesozoic Metamorphic and granitic Dissected upland; transitional between Yukon–Tanana and Brooks Range
Kilbuck Mountains Plateau ~18,000 400–900 ~1,200 Southwest Alaska (Kuskokwim Bay area) Mesozoic Volcanic and sedimentary Low-relief plateau; important salmon spawning rivers


Principal Lowland and Plain Regions in Alaska

Plain / Lowland Name Approximate Area (km²) Average Elevation (m) Maximum Elevation (m) Primary Location / Region Dominant Surface Deposit Geologic Age (Ma) Key Characteristics / Significance
Arctic Coastal Plain ~90,000 0–150 ~300 North Slope (Beaufort Sea coast) Alluvial, deltaic, permafrost, tundra Cenozoic (Quaternary) Largest continuous coastal plain in Alaska; extensive permafrost; major oil fields (Prudhoe Bay); critical caribou calving and waterfowl habitat
Yukon–Kuskokwim Lowland ~130,000 0–300 ~400 Southwest Interior (Yukon and Kuskokwim deltas) Alluvial, deltaic, floodplain, permafrost Cenozoic (Quaternary) Vast wetland complex; largest river deltas in Alaska; globally significant waterfowl staging and breeding area; subsistence fisheries
Tanana Valley Lowland ~45,000 100–400 ~600 Interior Alaska (Tanana River basin) Alluvial, glacial outwash, loess, permafrost Cenozoic (Quaternary) Broad river valley plain; major agricultural region (Delta Junction); extensive permafrost and thermokarst features
Koyukuk Lowland ~35,000 100–300 ~500 Interior Alaska (Koyukuk River basin) Alluvial, floodplain, permafrost Cenozoic (Quaternary) Extensive wetlands and meander belts; important moose and waterfowl habitat; remote wilderness
Copper River Basin Lowland ~25,000 300–600 ~800 South-central Interior (Copper River watershed) Glacial, alluvial, lacustrine, permafrost Cenozoic (Quaternary) Intermontane basin; glacial lake remnants; significant salmon runs and waterfowl staging
Susitna River Lowland ~20,000 50–400 ~600 South-central Alaska (Susitna River valley) Alluvial, glacial outwash, permafrost Cenozoic (Quaternary) Broad river floodplain; important salmon spawning and moose habitat; Matanuska–Susitna Valley agricultural area
Minto Flats Lowland ~15,000 100–200 ~300 Interior Alaska (Tanana River floodplain) Alluvial, wetland, permafrost Cenozoic (Quaternary) Large wetland complex; globally significant migratory bird habitat; subsistence hunting and fishing


Deserts and Arid Regions of Alaska

Region / Desert Name Approximate Area (km²) Average Annual Precipitation (mm) Average Elevation (m) Primary Location / Physiographic Province Dominant Vegetation Type Geologic Surface Material Notable Climatic / Ecological Feature
Arctic Coastal Plain Desert (Polar Desert) ~90,000 100–250 0–150 North Slope (Beaufort Sea coast) Tundra (graminoid, moss, lichen) Alluvial, deltaic, permafrost, loess Extreme cold desert; continuous permafrost; lowest precipitation in Alaska; major oil fields
Interior Alaska Dry Zone (Rain Shadow) ~80,000 250–350 100–400 Tanana and Yukon Flats (Interior lowlands) Boreal forest, shrub tundra, grassland patches Alluvial, loess, glacial outwash Continental rain shadow; warmest summers in Alaska; frequent wildfires; agricultural potential (Delta Junction)
Koyukuk–Yukon Flats Semi-Arid Zone ~50,000 200–300 100–300 Interior (Koyukuk and Yukon river confluence) Boreal forest, wetland mosaic Alluvial floodplain, permafrost Low precipitation interior basin; extensive wetlands; subsistence fisheries and moose habitat
North Slope Foothills Semi-Desert Transition ~40,000 150–300 150–600 Brooks Range northern flank Dwarf shrub tundra, graminoid Sedimentary, colluvial, permafrost Transitional polar semi-desert; critical caribou migration corridor; National Petroleum Reserve
Upper Copper River Basin Arid Pocket ~15,000 250–350 300–600 South-central Interior (Copper River basin) Boreal forest, steppe-like patches Glacial, alluvial, loess Rain shadow from Chugach Mountains; relatively warm and dry interior valley; salmon spawning grounds


Alaska's Physical Geography

Biggest U.S. state? That’d be Alaska - covering 665,384 square miles. Think bigger than Texas, California, and Montana piled together. Land like this makes up just a fifth of America’s total ground. Shaped by deep shifts beneath the surface, not to mention ice and wild weather, what you see here is raw natural change. High mountains rise sharp; wide basins stretch flat. Forces tugging at rock and air feed life unlike anywhere else. Creatures thrive in numbers seen few places elsewhere. People live within these shifting rhythms, part observer, part partaker. Out near Alaska's northwest tip, its landscape shifts across Arctic waters - the Arctic Ocean, Beaufort Sea, Bering Sea, then the Pacific - while Canada lies just to the east. This stretch of land keeps to itself, marked by lakes that number beyond three million and rivers stretching past twelve thousand in length. Glaciers take up nearly thirty-nine thousand square miles, silent under gray skies. Through such spaces, lives unfold without city sounds, shaped by space and survival rather than schedules or roads. The vastness here doesn’t whisper; it announces itself through rivers cutting through valleys, through snow lingering long after winter ends.

Relief and Landforms

From sea to sky, Alaska’s relief swings hard - its shores sit low while towering peaks rise near 20,000 feet at Denali, the continent’s tallest summit. Five broad zones make up the land: the Far North, Interior, Southwest, South Central, and Southeast - each shaped by its own set of elevations and features. Shaped by glaciers and deep forces beneath the ground, rock walls stretch high above wide basins, river paths, and saltwater channels carved through millions of years. People tend to live close together where ground stays flat, tucked behind natural walls that loom vertical and vast.

Mountain Ranges

Running across southern central areas, the Alaska Range covers about 650 kilometers. It holds Denali at an elevation of 6,190 meters - also home to seventeen of the twenty tallest peaks within the U.S. During the Cenozoic period, its shape took form due to persistent tectonic movement. This curved line splits the state's water flow patterns. Farther north lies the Brooks Range, stretching more than 1,100 kilometers into Arctic terrain. At 2,749 meters tall, Mount Chamberlin stands as the region's highest point near the Arctic circle. That range represents the most northern significant mountain range in North America. Its rocks date back to the Devonian through Cretaceous ages. Running over a thousand kilometers across the peninsula, the Aleutian Range hums with ongoing volcanic activity. Rising sharply near the coast, Redoubt Volcano reaches nearly three thousand eight hundred feet above sea level. Down in the southeastern corner, a different chain marks the boundary with Canada - the Saint Elias Mountains stand tall. Among them, Mount Saint Elias claims an impressive five-thousand-four-hundred-eighty-nine-foot height, known too for swift geological shifts and vast glaciers. Altogether, these two mountain zones make up thirty-nine separate units, which quietly highlights Alaska’s position within the seismic zone stretching along the Pacific.

Plateaus

Above lies the Yukon-Tanana Upland - roughly 150,000 square kilometers inside the territory. Height ranges between 600 and 1,200 meters. Underfoot sit ancient metamorphic stones from Paleozoic through Mesozoic eras. A highland shaped by erosion hosts gold sites across its surface. Flowing through it, large rivers cut deep paths. Far north stretches another landform, the Arctic Foothills plateau. Its base covers near 80,000 square kilometers on the slope that leads to the Arctic. Elevation often stays within 150 to 600 meters. Layers laid down in the Cretaceous and Tertiary periods make up much of its bedrock. Frozen ground stays present throughout the year. Above frozen tundras, the Kuskokwim Mountains rise into a flat expanse some sixty thousand square kilometers large. Here heights climb between four hundred and one thousand meters, holding veins of mercury beneath the soil. Elsewhere stands the Seward Peninsula Upland, covering about forty thousand square kilometers while lifting land from two hundred up to six hundred meters. These forms - distinct yet spread across the land - show how Alaska carries many kinds of low-relief hills within its vast sweep.

Plains

Stretching from the Beaufort Sea, the Arctic Coastal Plain covers roughly 90,000 square kilometers - its ground sits between zero and 150 meters above sea level, built mostly of recent glacier deposits locked in year-round frozen soil. Here lies active drilling for oil, along with herds of caribou making seasonal moves across the tundra. Down south, the Yukon-Kuskokwim Lowland takes up nearly twice as much space on Earth’s surface, spanning around 130,000 square kilometers; it rises slightly from sea level up to three hundred meters high, soaked in part by vast marshes that matter greatly for migratory birds worldwide. A wide space - Tanana Valley Lowland covers about 45,000 square kilometers - lies between one hundred and four hundred meters above sea level, making it Alaska’s main spot for growing food. Found within massive wild zones, these flats tend to rest on frozen ground, known as permafrost. Still, people live here because the land allows work and survival without disappearing into silence.

Deserts

Dry lands in Alaska are scarce yet contain the Arctic Coastal Plain Desert - about 90,000 square kilometers wide - with rainfall between 100 and 250 millimeters each year. Here, ground stays frozen much of the time, covered in tundra grasses. Moving south, the Interior Alaska Dry Zone covers around 80,000 square kilometers, shaped by as little as 250 but often up to 350 millimeters annual rain after crossing mountains nearby. Wildfires occasionally spark here under thickets of boreal forest. Farther west, the Koyukuk-Yukon Flats Semi-Arid Zone measures some fifty thousand square kilometers, seeing two hundred to three hundred millimeters precipitation on average while wetlands blend into the landscape. From north to south, each zone shows how weather shifts across Alaska. Cold stays strong where rain hardly falls at all. This mix shapes special landscapes unlike farther south.

Hydrography

Out here, Alaska holds more than three million lakes. Among them, Iliamna Lake stands tallest - measuring 2,589 square kilometers. Across five percent of the land area, wetlands stretch through 188,320 square kilometers. Life thrives because moisture lingers so long. Flowing across the terrain, twelve thousand rivers join together along 365,000 miles. One of the longest? The Yukon River runs 1,875 miles just inside Alaska's borders. Flowing through them are rivers fed by glaciers, where fishing and shipping exist alongside unique ecosystems. Scattered across the region are over one hundred thousand glaciers, making up five percent of terrain - their slow movement shapes river flow plus ocean height.

Rivers

Flowing 1,875 miles across Alaska, the Yukon River stands as the nation’s third-longest stream. Its path supports both salmon populations and inland travel. Near the southern edge of the state, the Kuskokwim River measures 702 nautical miles in length - its waters key to local food sources. Running shorter but just as intense, the Copper River covers 286 miles; cold glaciers feed its runoff while large fish runs thrive there. Scattered across the terrain, more than 3,000 rivers carve paths with constant flow. Erosion marks their trail, dropping sand and pebbles along the way. Life thrives where water meets land, feeding plants and animals alike. People draw sustenance too, built close to these winding routes.

Lakes

Buried deep inside Alaska, Iliamna Lake holds the title of biggest freshwater lake - measuring 2,589 square kilometers. Its floor dips nearly three hundred meters below the surface, reaching 301 meters down. Farther north, another giant appears: Becharof Lake covers more than a thousand one hundred square kilometers, feeding flocks of waterbirds. Not far off, Teshekpuk Lake spreads across eight hundred twenty-six square kilometers, its shallow depths quietly nurturing vast numbers of avian travelers. With ninety-four lakes bigger than 10 square miles, Alaska shows how much water can live among frozen ground. These spots become homes while surrounding landscapes stay locked in ice.

Coastline and Islands

Along Alaska's edge, more than 6,640 miles stretch when measured straight - this number climbs to 33,904 if you count every inlet and island. Compared to every coastline elsewhere in the United States, it covers far more ground. Shoreline shaped by tides adds up to 47,300 miles. Glaciers have carved deep channels into rock, making some areas feel like inside a glacier. There are 1,800 islands officially listed. Kodiak stands tallest among them, measuring 3,588 square kilometers across its surface. Running over 1,100 miles, the Aleutian Chain includes fourteen big islands along with fifty-five smaller ones - all shaped by volcanoes and marked by frequent earthquakes. Life thrives at sea here, while humans have lived along harsh coastlines for thousands of years, shaped by nature's strength.

Climate and Ecosystems

From warm coastlines to freezing tundras, Alaska’s weather shifts dramatically across its land. In the southern edges, more than two and a half meters of rain falls each year. Up toward the Arctic circle, less than quarter of that reaches the ground. Eight out of ten places here stay frozen underground forever. Because of this deep freeze, plants adapt - not just anywhere, but exactly what grows where. Toward the western tip, thick woods soak up moisture year after year. Beyond them stretches endless grassland, stretching vast and endless. This soggy world attracts countless winged travelers every season, drawn by hidden ponds and silent marshes. Life thrives here - more than 400 birds, countless large animals live among forests that shift like ice in spring. People move through these spaces, bound to nature’s rhythm, where cold gives way to warmth each year without fail.

Geology and Resources

Beneath Alaska, forces stir - the Pacific Ring of Fire still pulses. More than 130 volcanoes hum, spewing ash into skies; earthquakes rattle ground often, most famously in 1964 when it struck with magnitude 9.2 power. From deep pressure, rocks lift upward - seen in peaks such as the Alaska Range - all rising during the Cenozoic age. Buried deep, oil pools fill the northern tundra; while gold glimmers within the Yukon-Tanana Upland’s stone. Elsewhere, scattered minerals mark rocky plateaus under sunlight. Rocky features shape how the state makes money, because glaciers keep shrinking - this shift affects people living there along with the land itself.