Varved clay Stock Photos and Images
Varved Clay of Baumkirchen Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-varved-clay-of-baumkirchen-78138752.htmlRMEF3ENM–Varved Clay of Baumkirchen
. The Canadian field-naturalist. View 5.. View 6. View 5 looking upstream at the Wawbewawa slide shows the varved clay debris on the bed of the old stream. To the right are banks of clay, 60 to 80 feet high, that are in immediate danger of sliding as the stream is undercutting on the banks at a sharp bend in the stream. View 6 shows a landslide on the Blanche river about 3 miles east of Englehart where a bridge and several hundred feet of road were destroyed.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-canadian-field-naturalist-view-5-view-6-view-5-looking-upstream-at-the-wawbewawa-slide-shows-the-varved-clay-debris-on-the-bed-of-the-old-stream-to-the-right-are-banks-of-clay-60-to-80-feet-high-that-are-in-immediate-danger-of-sliding-as-the-stream-is-undercutting-on-the-banks-at-a-sharp-bend-in-the-stream-view-6-shows-a-landslide-on-the-blanche-river-about-3-miles-east-of-englehart-where-a-bridge-and-several-hundred-feet-of-road-were-destroyed-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-image233581524.htmlRMRG0FH8–. The Canadian field-naturalist. View 5.. View 6. View 5 looking upstream at the Wawbewawa slide shows the varved clay debris on the bed of the old stream. To the right are banks of clay, 60 to 80 feet high, that are in immediate danger of sliding as the stream is undercutting on the banks at a sharp bend in the stream. View 6 shows a landslide on the Blanche river about 3 miles east of Englehart where a bridge and several hundred feet of road were destroyed.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration
Pleistocene varved clay of Baumkirchen Makro Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-pleistocene-varved-clay-of-baumkirchen-makro-78136701.htmlRMEF3C4D–Pleistocene varved clay of Baumkirchen Makro
![. The Canadian field-naturalist. . View 4. View 3, looking downstream shows the debris of varved clay piled on the side of the pre-glacial channel. The horizontal line shows the pre-slide river level. Near the arrow was a cribwork for diverting logs into the main channel of the river. "^lew 4 shows the laminated clays that formed the bed of the river. They are much distorted in place due to movement during the slide or to gentle long continued movement preceding the actual slide To the right is an old channel in the clays now filled wtih silt and logs.. Please note that these images are e Stock Photo](https://c8.alamy.com/comp/RG0FJ7/the-canadian-field-naturalist-view-4-view-3-looking-downstream-shows-the-debris-of-varved-clay-piled-on-the-side-of-the-pre-glacial-channel-the-horizontal-line-shows-the-pre-slide-river-level-near-the-arrow-was-a-cribwork-for-diverting-logs-into-the-main-channel-of-the-river-quotlew-4-shows-the-laminated-clays-that-formed-the-bed-of-the-river-they-are-much-distorted-in-place-due-to-movement-during-the-slide-or-to-gentle-long-continued-movement-preceding-the-actual-slide-to-the-right-is-an-old-channel-in-the-clays-now-filled-wtih-silt-and-logs-please-note-that-these-images-are-e-RG0FJ7.jpg ". The Canadian field-naturalist. . View 4. View 3, looking downstream shows the debris of varved clay piled on the side of the pre-glacial channel. The horizontal line shows the pre-slide river level. Near the arrow was a cribwork for diverting logs into the main channel of the river. "^lew 4 shows the laminated clays that formed the bed of the river. They are much distorted in place due to movement during the slide or to gentle long continued movement preceding the actual slide To the right is an old channel in the clays now filled wtih silt and logs.. Please note that these images are e Stock Photo"){kind=icon}
. The Canadian field-naturalist. . View 4. View 3, looking downstream shows the debris of varved clay piled on the side of the pre-glacial channel. The horizontal line shows the pre-slide river level. Near the arrow was a cribwork for diverting logs into the main channel of the river. "^lew 4 shows the laminated clays that formed the bed of the river. They are much distorted in place due to movement during the slide or to gentle long continued movement preceding the actual slide To the right is an old channel in the clays now filled wtih silt and logs.. Please note that these images are e Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-canadian-field-naturalist-view-4-view-3-looking-downstream-shows-the-debris-of-varved-clay-piled-on-the-side-of-the-pre-glacial-channel-the-horizontal-line-shows-the-pre-slide-river-level-near-the-arrow-was-a-cribwork-for-diverting-logs-into-the-main-channel-of-the-river-quotlew-4-shows-the-laminated-clays-that-formed-the-bed-of-the-river-they-are-much-distorted-in-place-due-to-movement-during-the-slide-or-to-gentle-long-continued-movement-preceding-the-actual-slide-to-the-right-is-an-old-channel-in-the-clays-now-filled-wtih-silt-and-logs-please-note-that-these-images-are-e-image233581551.htmlRMRG0FJ7–. The Canadian field-naturalist. . View 4. View 3, looking downstream shows the debris of varved clay piled on the side of the pre-glacial channel. The horizontal line shows the pre-slide river level. Near the arrow was a cribwork for diverting logs into the main channel of the river. "^lew 4 shows the laminated clays that formed the bed of the river. They are much distorted in place due to movement during the slide or to gentle long continued movement preceding the actual slide To the right is an old channel in the clays now filled wtih silt and logs.. Please note that these images are e
. Bulletin of the British Museum (Natural History), Geology. ENVIRONMENTAL CHANGES 381 Glacial sequences 1 Central Sahara North Africa P acuminatus G persculptus. Central Portugal 3 Celtiberia N.E.Spain Fluvio-glacial sand varved and slumped clay Fluvio-glacial sand Varved clay Terrestrial tillite Pro-glacial and sub-glacial melt-out sands RAWTHEYAN Deep shelf Fault Sub-glacial manne-tilloid Shallow massive sands Regressive shelt sequence Calcareous tuff Sub-glacial marine tilloid Bedded sandstones 9 karstified surface Mid-deep shelf Carbonate shelves 4 Manitoulin Ontario, Canada 5 Anticosti E Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bulletin-of-the-british-museum-natural-history-geology-environmental-changes-381-glacial-sequences-1-central-sahara-north-africa-p-acuminatus-g-persculptus-central-portugal-3-celtiberia-nespain-fluvio-glacial-sand-varved-and-slumped-clay-fluvio-glacial-sand-varved-clay-terrestrial-tillite-pro-glacial-and-sub-glacial-melt-out-sands-rawtheyan-deep-shelf-fault-sub-glacial-manne-tilloid-shallow-massive-sands-regressive-shelt-sequence-calcareous-tuff-sub-glacial-marine-tilloid-bedded-sandstones-9-karstified-surface-mid-deep-shelf-carbonate-shelves-4-manitoulin-ontario-canada-5-anticosti-e-image233952380.htmlRMRGHCJ4–. Bulletin of the British Museum (Natural History), Geology. ENVIRONMENTAL CHANGES 381 Glacial sequences 1 Central Sahara North Africa P acuminatus G persculptus. Central Portugal 3 Celtiberia N.E.Spain Fluvio-glacial sand varved and slumped clay Fluvio-glacial sand Varved clay Terrestrial tillite Pro-glacial and sub-glacial melt-out sands RAWTHEYAN Deep shelf Fault Sub-glacial manne-tilloid Shallow massive sands Regressive shelt sequence Calcareous tuff Sub-glacial marine tilloid Bedded sandstones 9 karstified surface Mid-deep shelf Carbonate shelves 4 Manitoulin Ontario, Canada 5 Anticosti E
. Guide leaflet. - ? I Post-glacial stratified sands, eight feet thick, overlying the varved glacial clay of LakeHackensack. Mehrhof Brothers clay pit, one mile south of Little Ferry, New Jersey.. Post-glacial sand and gravel (a tributary delta deposit) overlying varviLake Hudson, Hornbeckers sand-pit, West Ilaverstraw, New York. il glacial clay of 33 34 AMERICAN MUSEUM GUIDE LEAFLET Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/guide-leaflet-i-post-glacial-stratified-sands-eight-feet-thick-overlying-the-varved-glacial-clay-of-lakehackensack-mehrhof-brothers-clay-pit-one-mile-south-of-little-ferry-new-jersey-post-glacial-sand-and-gravel-a-tributary-delta-deposit-overlying-varvilake-hudson-hornbeckers-sand-pit-west-ilaverstraw-new-york-il-glacial-clay-of-33-34-american-museum-guide-leaflet-image370768731.htmlRM2CF5Y8B–. Guide leaflet. - ? I Post-glacial stratified sands, eight feet thick, overlying the varved glacial clay of LakeHackensack. Mehrhof Brothers clay pit, one mile south of Little Ferry, New Jersey.. Post-glacial sand and gravel (a tributary delta deposit) overlying varviLake Hudson, Hornbeckers sand-pit, West Ilaverstraw, New York. il glacial clay of 33 34 AMERICAN MUSEUM GUIDE LEAFLET
