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Sandy River bank erosion
No full textThick deposits of glacial outwash sand are eroded by the Sandy River. 1-4: The high, stratified sand bank is on the east shore of the river. Cobbles form the sand bank/bar on the west shore. 5: Tom Weddle (MGS) examines meander channel cut into galcial outwash. 6-7: sample location on east bank where woody debris yielded 2120 carbon date. Project Name: Marvinney Historical Photoshttps://digitalmaine.com/mgs_geologic_field_photos/37014/thumbnail.jp
Sandy River bank erosion
No full textThick deposits of glacial outwash sand are eroded by the Sandy River. 1-4: The high, stratified sand bank is on the east shore of the river. Cobbles form the sand bank/bar on the west shore. 5: Tom Weddle (MGS) examines meander channel cut into galcial outwash. 6-7: sample location on east bank where woody debris yielded 2120 carbon date. Project Name: Marvinney Historical Photoshttps://digitalmaine.com/mgs_geologic_field_photos/37015/thumbnail.jp
Sandy River bank erosion
No full textThick deposits of glacial outwash sand are eroded by the Sandy River. 1-4: The high, stratified sand bank is on the east shore of the river. Cobbles form the sand bank/bar on the west shore. 5: Tom Weddle (MGS) examines meander channel cut into galcial outwash. 6-7: sample location on east bank where woody debris yielded 2120 carbon date. Project Name: Marvinney Historical Photoshttps://digitalmaine.com/mgs_geologic_field_photos/37016/thumbnail.jp
Mesozoic basalt, Southwest Head
No full textCliffs underlain with massive basalt unit of the North Basin Basalt. Jurassic Project Name: Marvinney Historical Photoshttps://digitalmaine.com/mgs_geologic_field_photos/37043/thumbnail.jp
Cow Head Formation, Newfoundland
No full textExamples of the Cow Head Formation and Breccia, Cow Head, Newfoundland. Cambrian-Ordovician. Part of the Humber Arm allocthon thrust from east to west over younger rocks. Approx. location. 1: Doug Reusch (UMF) speaks to U Maine group, Stephen Norton (UM, yellow jacket), Walter Anderson (MGS, right). Project Name: Marvinney Historical Photoshttps://digitalmaine.com/mgs_geologic_field_photos/37048/thumbnail.jp
Cambrian-Ordovician sedimentary rocks, Western Brook Pond
No full textUpturned Cambrian-Ordovician shelf rocks, Western Brook Pond, Newfoundland Project Name: Marvinney Historical Photoshttps://digitalmaine.com/mgs_geologic_field_photos/37063/thumbnail.jp
Ultramafic rocks, Table Mountain, Newfoundland
No full textUltramafic rocks exposed on Table Mountain are part of an ophiolite sequence including oceanic crust and mantle rocks. Images show examples of cumulate layering in the ultramafic rocks and some thin chromitite layers. Project Name: Marvinney Historical Photoshttps://digitalmaine.com/mgs_geologic_field_photos/37072/thumbnail.jp
B24: Plate 7A & 7B
No full text7A. Relict climbing-ripple sets (lower) merging into parallel-bedded section (center). Alkali feldspar-cordierite-bearing gneissic granofels, locality as given in pl. 6B. 7B. Transverse section of i·elict linguoid ripples overlying section described in pl. 6B. Project Name: Bulletin 24 Plateshttps://digitalmaine.com/mgs_geologic_field_photos/37112/thumbnail.jp
B24: Plate 8
No full textSketch and source photograph of relict climbing-ripple sets in metaquartzwacke section. Relict graded bedding within the sets is well preserved. Long Falls (locality D , text fig. 5). Project Name: Bulletin 24 Plateshttps://digitalmaine.com/mgs_geologic_field_photos/37113/thumbnail.jp
B24: Plate 22
No full textB24: Plate 22Bulletin 24 Plateshttps://digitalmaine.com/mgs_geologic_field_photos/37116/thumbnail.jp