Alaska isn't just America's largest state—it's a geological and ecological universe unto itself. From North America's highest peak to the planet's most extensive tidewater glaciers, from boreal forests stretching to the horizon to tundra that blooms briefly under midnight sun, Alaska's landscapes defy superlatives.
The Alaska Range arcs 400+ miles across southcentral Alaska, crowned by Denali (20,310 ft / 6,190 m)—the highest summit in North America and one of Earth's greatest vertical reliefs (18,000 ft from base to peak). Other major ranges:
Nearly 50% of Alaska is forested, dominated by the boreal forest (taiga)—a circumpolar band of white/black spruce, paper birch, aspen, and balsam poplar adapted to permafrost, extreme seasons, and fire cycles. In the southeast panhandle and coastal southcentral, temperate rainforests flourish: Sitka spruce, western hemlock, yellow/red cedar draped in mosses and epiphytes, fed by 200+ inches of annual rain. The Tongass National Forest (16.7 million acres) is the U.S.'s largest national forest and the world's largest intact temperate rainforest.
Covering ~one-third of Alaska, tundra prevails where permafrost and short growing seasons exclude trees. Two types:
Thousands of thermokarst lakes dot the coastal plain—critical waterfowl breeding habitat. The Arctic National Wildlife Refuge protects 19 million acres of this ecosystem.
Alaska holds ~100,000 glaciers—more than the rest of the U.S. combined. Key facts:
Glacial melt drives sea-level rise, alters ocean circulation, and reshapes coastlines in real time.
33,904 miles (54,563 km) of coastline—more than the rest of the U.S. combined. Features:
Alaska's landscapes aren't static scenery—they're active planetary systems: carbon storage in permafrost and forests, freshwater reservoirs in glaciers, climate regulation via sea ice, and biodiversity refugia for species losing habitat elsewhere. Understanding them is essential for global climate science, Indigenous sovereignty, and the future of the Arctic.