VOLCANIC AND ASSOCIATED ROCKS (WRANGELL LAVA)
Alluvium along streams and in fans (Holocene)—Mainly in active flood plains and lowermost terraces of major and some minor streams and in larger active fans. Larger fan margins are outlined by fine dots. Chiefly stratified silt, sand, gravel, and boulders Older alluvium (Holocene and Pleistocene)—Ma...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.688.5560 2023-05-15T15:41:08+02:00 VOLCANIC AND ASSOCIATED ROCKS (WRANGELL LAVA) Sonya Creek Shield Volcano The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.688.5560 http://pubs.usgs.gov/imap/i-2695/i-2695so.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.688.5560 http://pubs.usgs.gov/imap/i-2695/i-2695so.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.usgs.gov/imap/i-2695/i-2695so.pdf text ftciteseerx 2016-01-08T18:14:35Z Alluvium along streams and in fans (Holocene)—Mainly in active flood plains and lowermost terraces of major and some minor streams and in larger active fans. Larger fan margins are outlined by fine dots. Chiefly stratified silt, sand, gravel, and boulders Older alluvium (Holocene and Pleistocene)—Mainly outwash related to Alaskan glaciation and possibly younger phase of Wisconsin glaciation. Chiefly stratified silt, sand, gravel, and boulders Colluvium, undifferentiated (Holocene and Pleistocene)—Chiefly talus, but also includes deposits of small landslides, rock glaciers, other products of mass-wasting processes, and alluvium in small fans and cones. Chiefly poorly sorted silt, sand, gravel, and boulders Landslide deposits (Holocene and Pleistocene)—Includes large slump and debris avalanche deposits. Particularly common along steep north flank of mountain escarpment south of Beaver Creek. Slump deposits consist chiefly of masses of volcanic rock as much as hundreds of meters wide; debris deposits are chiefly diamicton and rubble Solifluction deposits (Holocene and Pleistocene)—Deposits on low-angle, low-relief slopes at relatively high elevations. Mostly bedrock rubble but may include some Wisconsin and older glacial drift Rock glacier deposits (Holocene)—Deposits of active rock glaciers exhibiting well-defined lobate forms. Chiefly angular blocks and diamicton Alaskan glaciation deposits (Holocene)—Terminal and lateral moraine at base of small ice field in sec. 34, T. 2 N., R. 22 E. Chiefly diamicton Younger Wisconsin glaciation deposits (Pleistocene)—Terminal and lateral moraines of late(?) phase of Wisconsin glaciation. Chiefly diamicton and rubble Older Wisconsin glaciation deposits (Pleistocene)—Chiefly ground moraine of main(?) phase of Wisconsin glaciation. Diamicton, local gravel and sand Fluvio-glacial deposits (Pleistocene)—Chiefly outwash related to main(?) phase of Wisconsin glaciation. Silt, sand, gravel, and boulders Text Beaver Creek Unknown |
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English |
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Alluvium along streams and in fans (Holocene)—Mainly in active flood plains and lowermost terraces of major and some minor streams and in larger active fans. Larger fan margins are outlined by fine dots. Chiefly stratified silt, sand, gravel, and boulders Older alluvium (Holocene and Pleistocene)—Mainly outwash related to Alaskan glaciation and possibly younger phase of Wisconsin glaciation. Chiefly stratified silt, sand, gravel, and boulders Colluvium, undifferentiated (Holocene and Pleistocene)—Chiefly talus, but also includes deposits of small landslides, rock glaciers, other products of mass-wasting processes, and alluvium in small fans and cones. Chiefly poorly sorted silt, sand, gravel, and boulders Landslide deposits (Holocene and Pleistocene)—Includes large slump and debris avalanche deposits. Particularly common along steep north flank of mountain escarpment south of Beaver Creek. Slump deposits consist chiefly of masses of volcanic rock as much as hundreds of meters wide; debris deposits are chiefly diamicton and rubble Solifluction deposits (Holocene and Pleistocene)—Deposits on low-angle, low-relief slopes at relatively high elevations. Mostly bedrock rubble but may include some Wisconsin and older glacial drift Rock glacier deposits (Holocene)—Deposits of active rock glaciers exhibiting well-defined lobate forms. Chiefly angular blocks and diamicton Alaskan glaciation deposits (Holocene)—Terminal and lateral moraine at base of small ice field in sec. 34, T. 2 N., R. 22 E. Chiefly diamicton Younger Wisconsin glaciation deposits (Pleistocene)—Terminal and lateral moraines of late(?) phase of Wisconsin glaciation. Chiefly diamicton and rubble Older Wisconsin glaciation deposits (Pleistocene)—Chiefly ground moraine of main(?) phase of Wisconsin glaciation. Diamicton, local gravel and sand Fluvio-glacial deposits (Pleistocene)—Chiefly outwash related to main(?) phase of Wisconsin glaciation. Silt, sand, gravel, and boulders |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
author |
Sonya Creek Shield Volcano |
spellingShingle |
Sonya Creek Shield Volcano VOLCANIC AND ASSOCIATED ROCKS (WRANGELL LAVA) |
author_facet |
Sonya Creek Shield Volcano |
author_sort |
Sonya Creek |
title |
VOLCANIC AND ASSOCIATED ROCKS (WRANGELL LAVA) |
title_short |
VOLCANIC AND ASSOCIATED ROCKS (WRANGELL LAVA) |
title_full |
VOLCANIC AND ASSOCIATED ROCKS (WRANGELL LAVA) |
title_fullStr |
VOLCANIC AND ASSOCIATED ROCKS (WRANGELL LAVA) |
title_full_unstemmed |
VOLCANIC AND ASSOCIATED ROCKS (WRANGELL LAVA) |
title_sort |
volcanic and associated rocks (wrangell lava) |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.688.5560 http://pubs.usgs.gov/imap/i-2695/i-2695so.pdf |
genre |
Beaver Creek |
genre_facet |
Beaver Creek |
op_source |
http://pubs.usgs.gov/imap/i-2695/i-2695so.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.688.5560 http://pubs.usgs.gov/imap/i-2695/i-2695so.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766373993628041216 |