Indigenous people have lived in Alaska for thousands of years, and it is widely believed that the region served as the entry point for the initial settlement of North America by way of the Bering land bridge. The Russian Empire was the first to actively colonize the area beginning in the 18th century, eventually establishing Russian America, which spanned most of the current state, and promoted and maintained a native Alaskan Creole population. The expense and logistical difficulty of maintaining this distant possession prompted its sale to the U.S. in 1867 for US$7.2 million (equivalent to $157 million in 2023). The area went through several administrative changes before becoming organized as a territory on May 11, 1912. It was admitted as the 49th state of the U.S. on January 3, 1959.
Amchitka was populated for more than 2,500 years by the Aleut people, but has had no permanent population since 1832. The island has been part of the United States since the Alaska Purchase of 1867. During World War II, it was used as an airfield by US forces in the Aleutian Islands Campaign.
Köppen climate types of Alaska, using 1981-2010 climate normals.
The climate of Alaska is determined by average temperatures and precipitation received statewide over many years. The extratropical storm track runs along the Aleutian Island chain, across the Alaska Peninsula, and along the coastal area of the Gulf of Alaska which exposes these parts of the state to a large majority of the storms crossing the North Pacific. The climate in Juneau and the southeast panhandle is a mid-latitude oceanic climate (similar to Scotland, or Haida Gwaii), (KöppenCfb) in the southern sections and a subarctic oceanic climate (Köppen Cfc) in the northern parts. The climate in Southcentral Alaska is a subarctic climate (Köppen Dfc) due to its short, cool summers. The climate of the interior of Alaska is best described as extreme and is the best example of a true subarctic climate, as the highest and lowest recorded temperatures in Alaska have both occurred in the interior. The climate in the extreme north of Alaska is an Arctic climate (Köppen ET) with long, cold winters, and cool summers where snow is possible year-round. (Full article...)
Image 15Oil pooled on rocks on the shore of Prince William Sound after the oil spill. (from History of Alaska)
Image 16Alaska's area compared to the 48 contiguous states (from Geography of Alaska)
Image 17St. Michael's Cathedral in Sitka. The original structure, built in 1848, burned down in a fire on January 2, 1966. The cathedral was rebuilt from plans of the original structure and contains artifacts rescued from the fire. (from History of Alaska)
This is a list of recognized content, updated weekly by JL-Bot (talk·contribs) (typically on Saturdays). There is no need to edit the list yourself. If an article is missing from the list, make sure it is tagged (e.g. {{WikiProject Alaska}}) or categorized correctly and wait for the next update. See WP:RECOG for configuration options.
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Knik, Alaska, the ghost town, and Knik River, Alaska, the CDP, are not the same place. In fact, they are approximately an hour's drive away from each other.
Despite its name of "City and Borough of Yakutat," this entity is a borough, not a consolidated city-borough.
See the talk page (or archives of same) of WP:ALASKA, or of the articles in question, for more information.
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