Английская Википедия:Glacial erratic boulders of Kitsap County, Washington

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Шаблон:Short description Шаблон:GeoGroup Glacial erratic boulders of Kitsap County are large glacial erratic boulders of rock which were moved into Kitsap County, Washington by glacial action during previous ice ages.

Kitsap County was so extensively formed by glaciation that according to J Harlen Bretz almost any east-west traverse across the Kitsap Peninsula (shared with two other counties) will describe an ascending and descending profile across till ridges.[1]

List of boulders

Frog Rock, dynamited, moved off the road, and stacked in 20th century

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Файл:Bainbridge Island Frog Rock.jpg
Haleets, at Agate Point on Bainbridge Island, has petroglyphs said to be from before 400 CE

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Файл:Haleets petroglyph rock.JPG
Illahee Preserve erratic

At Illahee Preserve Almira parking lot[2]

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Файл:No image.png
Illahee Road erratic, an "extremely large erratic of volcanic rock"[3]

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Файл:No image.png
Lone Rock, the namesake landmark of the unincorporated community of Lone Rock, located on the Hood Canal tidal flat about 400 feet off shore. At least Шаблон:Convert across.[4]

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Файл:Lone-Rock-Hood-Canal-Washington-18-Aug-2017.jpg

References

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External links

Шаблон:Washington erratics


Шаблон:KitsapCountyWA-geo-stub