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Sitka National Historical Park is small — about 47 hectares (116 acres) — but it sits in one of the most tectonically active regions of North America, and all of the ground under it was left by ice and sea.

The park

WhereWestern shore of Baranof Island, Sitka Borough, southeastern Alaska — about 150 km (93 mi) southwest of Juneau
StatusProclaimed a national monument March 23, 1910; redesignated a national historical park October 18, 1972
HistoryThe site of the last major battle between invading Russian traders and the Tlingit
To seeTlingit and Haida totem poles along coastal trails; the Russian Bishop's House, built in 1842 and restored, a rare piece of Russian–American architecture from Russia's little-known colonial past in North America
To doExplore Tlingit culture and art, learn about the Russian colonial period, or walk the temperate rainforest on the Totem Trail and Russian Memorial Loop

A hiker on a mountain trail.

Harbor Mountain Trail. NPS photo by Weston Kessler.

What lies beneath

The Sitka area has mountains, dormant volcanoes and several faults. Repeated advances and retreats of Pleistocene glaciers carved deep bays, steep valley walls, jagged coastlines and sea cliffs, and left moraines nearby.

  • All of the park's geology is unconsolidated Quaternary deposits: glacial till, glacial gravels, glacial erratics (boulders carried in by ice that differ from the local rock) and coastal marine deposits.
  • About half of the park's resources are coastal or marine, including about 1.6 km (1 mi) of shoreline that waves and tides constantly rework.

The waterfront at Sitka Sound.

Sitka Sound. Image from the National Park Service's Geodiversity Atlas page on Sitka.

Maps and inventories

The Park Service's Geologic Resources Inventory makes digital geologic maps and reports for more than 270 natural resource parks; its products for Sitka — scoping summaries, GIS maps, reports and posters — are in the NPS DataStore. A Soil Resources Inventory for the park has also been completed.

Geodiversity is the full range of a park's geologic and soil resources and processes: rocks, minerals, sediments, fossils, landforms and the forces that shape them. The NPS Geodiversity Atlas gathers it park by park for education, geoconservation and management.

Sources

Based on "NPS Geodiversity Atlas—Sitka National Historical Park, Alaska," National Park Service; a work of the United States government in the public domain.

LanguagesEnglish

Licence: CC0 1.0 (public domain) · Adapted from www.nps.gov

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The runaway star that left the Tarantula Nebula
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The Blackwell School, where segregation had no law behind it
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The Eagle Nebula, seen in the infrared
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The house where the Equal Rights Amendment was written
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The Aleutians, the forgotten front of the Second World War
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The Cosmic Cliffs are not cliffs