Lake_Minchin_deposits_above_deposits_left_by_Lake_Ballivian.png (417 × 360 pixels, file size: 131 KB, MIME type: image/png)
Description |
Finely laminated clays, silts, and sands of Lake Minchin above (north) Fairweather Gap. Their visible portion is here 30 feet thick and in places have as high as 15 to 30 thin, and about 7 thicker laminations to the inch. They are in strong contrast to the thick-bedded deposits of Lake Ballivian. They lie only on the valley floor, whereas the deposits of Lake Ballivian are now in most places eroded back some distance from the river. |
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Source | |
Date |
Published in 1914 and created before 1914 |
Author |
Unknown |
Permission (Reusing this file) |
See below.
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![]() | This image is in the public domain in the United States because it was first published outside the United States prior to January 1, 1929. Other jurisdictions have other rules. Also note that this image may not be in the public domain in the 9th Circuit if it was first published on or after July 1, 1909 in noncompliance with US formalities, unless the author is known to have died in 1953 or earlier (more than 70 years ago) or the work was created in 1903 or earlier (more than 120 years ago.)[1] | ![]() |
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current | 13:39, 15 October 2016 | ![]() | 417 × 360 (131 KB) | Jo-Jo Eumerus (talk | contribs) | {{Information |description=Finely laminated clays, silts, and sands of Lake Minchin above (north) Fairweather Gap. Their visible portion is here 30 feet thick and in places have as high as 15 to 30 thin, and about 7 thicker laminations to the inch. The... |
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