West Coast of the United States
Coastline in the United States / From Wikipedia, the free encyclopedia
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The West Coast of the United States – also known as the Pacific Coast, the Pacific Seaboard, and the Western Seaboard – is the coastline along which the Western United States meets the North Pacific Ocean. The term typically refers to the contiguous U.S. states of California, Oregon, and Washington, but sometimes includes Alaska and Hawaii, especially by the United States Census Bureau as a U.S. geographic division.
West Coast of the United States | |
---|---|
Country | United States |
Principal cities | Los Angeles San Diego San Jose San Francisco Sacramento Portland Seattle Anchorage Honolulu |
Largest city | Los Angeles |
Largest metropolitan area | Greater Los Angeles |
Area | |
• Total | 1,009,688 sq mi (2,615,080 km2) |
• Land | 895,287 sq mi (2,318,780 km2) |
• Water | 21,433 sq mi (55,510 km2) |
• Coastal | 28,913 sq mi (74,880 km2) |
Highest elevation (Denali) | 20,310 ft (6,190.5 m) |
Lowest elevation | −282 ft (−86 m) |
Population (2020) | |
• Total | 53,669,422[lower-alpha 1] |
Time zone | |
Mountain | UTC−7:00 |
• Summer (DST) | UTC−6:00 |
Pacific | UTC−8:00 |
• Summer (DST) | UTC−7:00 |
Alaska | UTC−9:00 |
• Summer (DST) | UTC−8:00 |
Hawaii | UTC−10:00 |
There are conflicting definitions of which states comprise the West Coast of the United States, but the West Coast always includes California, Oregon, and Washington as part of that definition. Under most circumstances, however, the term encompasses the three contiguous states and Alaska, as they are all located in North America. For census purposes, Hawaii is part of the West Coast, along with the other four states.[3] Encyclopædia Britannica refers to the North American region as part of the Pacific Coast, including Alaska and British Columbia. Although the encyclopedia acknowledges the inclusion of Hawaii in some capacity as part of the region, the editors wrote that "it has little in common geologically with the mainland states."[4]
Several dictionaries offer different definitions of the West Coast. Lexico restricts the West Coast's definition to "the western seaboard of the U.S. from Washington to California."[5] However, Macmillan Dictionary provides a less specific definition as "the western coast of the U.S., along the Pacific Ocean."[6] As for the Cambridge Dictionary, the West Coast is "the area of the Pacific coast in the U.S. that includes California."[7]
The history of the West Coast begins with the arrival of the earliest known humans of the Americas, Paleo-Indians, crossing the Bering Strait from Eurasia into North America over a land bridge, Beringia, that existed between 45,000 BCE and 12,000 BCE (47,000–14,000 years ago). Small isolated groups of hunter-gatherers migrated alongside herds of large herbivores far into Alaska. Between 16,500 BCE and 13,500 BCE (18,500–15,500 years ago), ice-free corridors developed along the Pacific coast and valleys of North America and possibly by sea.[8]
Alaska Natives, indigenous peoples of the Pacific Northwest Coast, and California indigenous peoples eventually descended from the Paleo-Indians. They developed various languages and established trade routes.[citation needed]
Later, Spanish, British, French, Russian, and American explorers and settlers began colonizing the area.[citation needed]
On May 10, 1869, the first transcontinental railroad was completed joining the West Coast to the East of the United States.
The West Coast of the United States has an oceanic climate in its Northwestern, Northern, and Eastern edge towards the U.S.-Canada border, but from Northern California, towards the U.S.-Mexico border the climate is mediterranean. While the northern half of the west coast, particularly coastal Washington and Oregon has moderate rainfall, particularly during the winter months, much of coastal California is drier year-round. The coastline sees significantly milder temperatures compared to inland areas during summer. In far Northern California there is a difference of 17 °C (30 °F) between Eureka and Willow Creek in spite of only 25 miles (40 km) separating the locations and Willow Creek being located at a 500 metres (1,600 ft) elevation. Slightly narrower fluctuations can be seen all through the coastline, and could partially be explained by the cold currents in the Pacific Ocean moderating coastal temperatures and the mountain ranges blocking the maritime air from moving farther inland than its foothills during summer. Coastal fog is also prevalent in keeping shoreline temperatures cool. While famous in the San Francisco Bay Area, coastal fog also affects Santa Monica in Los Angeles, Southern California, leading to May gray and June gloom conditions. Coastal California has very little yearly temperature differences with cool summers similar to those expected in parts of Northern Europe in San Francisco but warmer temperatures year-round further south. A short journey inland and summer temperatures are comparable with the rest of the United States on the same latitudes, sometimes warmer due to prevailing winds from the Nevada and Arizona hot desert climate. [citation needed]