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Wrangell–Saint Elias National Park and Preserve (fig. 6), the largest unit in the U.S. National Park System, encompasses nearly 13.2 million acres of geological won derments. Furthermore, its geologic makeup is shared with contiguous Tetlin National Wildlife Refuge in Alaska, Kluane National Park and Game Sanctuary in the Yukon Territory, the Alsek-Tatshenshini Provincial Park in British Columbia, the Cordova district of Chugach National Forest and the Yakutat district of Tongass National Forest, and Glacier Bay National Park and Preserve at the north end of Alaska’s panhan dle—shared landscapes of awesome dimensions and classic geologic features. In 1978, the United Nations recognized the global importance of Wrangell–Saint Elias and Kluane by designating them as “World Heritage” sites; Glacier Bay and Alsek-Tatshenshini were similarly designated in 1992, unify ing some 24 million acres of international parklands. The array of geologic features makes these parklands an impressive outdoor laboratory. Within Wrangell–Saint Elias are displayed features that indicate (1) how the southern Alaskan continental margin has more than doubled in size in approximately the past 200 million years by incremental addition of far-traveled geologic fragments; (2) how underthrusting by the Pacific oceanic plate6 has prompted rapid uplift, voluminous vol canism, and powerful earthquakes; and (3) how uplift of the coastal mountains adjacent to the storm-brewery of the Gulf of Alaska has engendered large and scenic systems of alpine, piedmont, and tidewater glaciers. In 1892, glaciologist Israel C. Russell, writing of one of the earliest scientific probes of the Wrangell–Saint Elias

A geologic guide to Wrangell-Saint Elias National Park and Preserve, Alaska: A tectonic collage of northbound terranes