Английская Википедия:Glacial erratic boulders of King County, Washington
Шаблон:GeoGroup Glacial erratic boulders of King County are large glacial erratic boulders of rock which were moved into King County, Washington by glacial action during previous ice ages.
The Pleistocene ice age glaciation of Puget Sound created many of the geographical features of the region, including Puget Sound itself,Шаблон:Sfn and the erratics are one of the remnants of that age.Шаблон:Sfn According to Nick Zentner of Central Washington University Department of Geological Sciences, "Canadian rocks [are] strewn all over the Puget lowland, stretching from the Olympic Peninsula clear over to the Cascade Range."[1] Erratics can be found at altitudes up to about Шаблон:Convert in the Enumclaw area,Шаблон:Sfn along with kames, drumlins,Шаблон:Sfn and perhaps also the unique Mima mounds.[2] The soil of Seattle, the county's (and state's) largest city, is approximately 80% glacial drift, most of which is Vashon glacial deposits (till),Шаблон:Sfn and nearly all of the city's major named hills are characterized as drumlins (Beacon Hill, First Hill, Capitol Hill, Queen Anne Hill) or drift uplands (Magnolia, West Seattle).[1]Шаблон:Sfn Boulders greater than 3 meters in diameter are "rare" in the Vashon till,Шаблон:Sfn but can be found, as seen in the table below.
List of boulders
Name and description | Height | Image |
---|---|---|
Beaver Lake Preserve erratics are glacial erratics in and around protected space in Sammamish, weighing up to 100 tons.[3] The lake is a kettle lake also due to glaciation.[3] In the 1950s otters would reportedly rest on the large erratic at the north end of Beaver Lake.Шаблон:Sfn | Файл:No image.png | |
Big Rock is an Шаблон:Convert tall glacial erratic in the city of Duvall. A Duvall road, a park, and several businesses are named after it.[4][5] The rock, and two non-native sequoias adjacent to it probably planted by area pioneers, are a local landmark.[6] The erratic lies in what is said to be the smallest King County park, Шаблон:Convert in extent, that barely contains the rock and sequoias.[7] The two lanes of Big Rock Road used to split into a wye around the rock, until a shopping center was built nearby in the 1990s.[7][6] | Шаблон:Sort | Файл:Big Rock erratic in Duvall north face.JPG |
Big Rock Park erratic is a glacial erratic in the eponymous city park in Sammamish. Sammamish considered naming the park "Bigger Rock Park" to distinguish it from the identically named park in Duvall.[8] | Шаблон:Sort | Файл:Big rock at Big Rock Park 03.jpg |
Cascadia College erratic
Saved from destruction by sit-in conducted by Cascadia College environmental politics students, and relocated away from construction site.[9][10][11][12][13] The rock, which several students occupied during the sit-in, was about 2 meters across before being jackhammered to two thirds its original size.[12] |
Шаблон:Sort | Файл:Cascadia College erratic 3.jpg |
Des Moines Beach erratic near Des Moines Beach Park in Des Moines | Шаблон:Sort | Файл:Des Moines Beach erratic front.JPG |
Шаблон:AnchorDiscovery Park beach erratics
Four or more erratics on beach below Discovery Park. Largest is Шаблон:Convert high, Шаблон:Convert in circumference.[15] |
Шаблон:Sort | Файл:Eastern Discovery Park beach erratic, yardstick.jpg |
Шаблон:Vanchor is a glacial erratic in Cougar Mountain Regional Wildland Park near Bellevue. It is approximately the size of a two-car garage, and Шаблон:Convert high.[16]Шаблон:Sfn | Шаблон:Sort | Файл:Fantastic Erratic on Cougar Mountain.jpg |
Шаблон:Vanchor (also Fourmile Rock) is a round granite erratic, approximately Шаблон:Convert across, in the intertidal zone below Seattle's Magnolia Bluff and 60 yards offshore.Шаблон:Sfn It has had a navigational light placed on it and appears on nautical charts.[17]
Native Americans called the rock LE'plEpL, also written La'pub, and also called it Tele'tla (meaning "rock"). A legend says that a hero named Sta'kub could throw a giant cedar and hazel branch dragnet over the rock while standing at the beach.Шаблон:Sfn |
Шаблон:Sort | Файл:Fourmile Rock, Magnolia at low tide, with yardstick.JPG |
Unnamed erratic at Highline College. Granitic with "textbook en echelon dikes". Шаблон:Convert and Шаблон:Convert high.[19] | Шаблон:Sort | Файл:Highline CC erratic.jpg |
Homage artwork boulders, three locations in Bridle Trails neighborhood of Bellevue,[20] using "local granite boulders".[21] Exposed granitic bedrock does not occur in western King County.Шаблон:Sfn
Шаблон:Coord (NE 24th)
|
Файл:Bridle Trails boulders on 24th.jpg | |
Шаблон:Vanchor in Seattle's Leschi Park is a sandstone erratic with many embedded bivalve fossils. Analysis of the fossils and the rock's minerals shows it may have come from the Nooksack Group near Mount Baker, or from the Harrison Lake area of southern British Columbia.[22] | Шаблон:Sort | Файл:Leschi erratic east face, yardstick.JPG |
Lone Rock in Tiger Mountain State Forest on Tiger Mountain[23][24] | Шаблон:Sort | Файл:2020-06-08 Tiger Mtn Lone Rock Erratic - from side.jpg |
Шаблон:Vanchor in Ravenna Park in Seattle, a granodiorite stone three yards (2.75 meters) tall in Ravenna Creek with a wooden footbridge that wraps around it.Шаблон:Sfn[25] | c. Шаблон:Sort | Файл:Ravenna park erratic east face, yardstick.JPG |
Talus Rocks, a collection of piled erratics in Tiger Mountain State Forest on Tiger Mountain,Шаблон:SfnШаблон:Sfn[26] forming rock caves (called "Devil's Dens" in New England[27]) said to be among the largest in Washington.[28] | Шаблон:Sort | Файл:Talus Rocks, Tiger Mountain, Washington - round boulder with yardstick.JPG |
Шаблон:Vanchor near 17th Ave. NE and NE 104th St., in Seattle Parks' Kingfisher Natural Area. A local conservation group calls the area containing the boulder "Erratic Flats".[29] | c. Шаблон:Sort | Файл:Thornton Creek erratic with yardstick.JPG |
Wedgwood Rock is a glacial erratic (and known to geologists as the "Wedgwood Erratic") near the neighborhood of Wedgwood in Seattle, Washington. It is Шаблон:Convert in circumference and Шаблон:Convert or Шаблон:ConvertШаблон:Sfn in height. Since 1970 it has been an offense punishable by a $100 fine to climb the rock.[30] | Шаблон:Sort | Файл:Wedgwood Rock, yardstick.JPG |
Anonymous erratic in Wedgwood Square Park[31] | Шаблон:Sort | Файл:Wedgwood Square erratic, yardstick.JPG |
References
- Notes
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Further reading
External links
- Washington glacial erratics project at University of Washington dept. of earth and space sciences
- ↑ 1,0 1,1 Шаблон:YouTube, narrated by Nick Zentner (Central Washington University Department of Geological Sciences). Uploaded March 2, 2015 by Hugefloods.com (Nick Zentner and Tom Foster: Discover the Ice Age Floods).
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- ↑ Шаблон:Historylink
- ↑ http://wedgwoodinseattlehistory.com/2012/03/15/parks-in-wedgwood/