Geology√

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Geology√

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Geology√

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Geology√

1974 Archival description results for Geology√

1974 results directly related Exclude narrower terms

Cliff in dislocated glacial deposits.

Cliff in dislocated glacial deposits. Dislocation stage, last glacial period. Dislocation of the series and planing of the stratum ends by glacial movement. D. Ground moraine in glacier. G. Overthrust planes. Source: Atlas of Denmark.

Cliff in dislocated glacial deposits.

Cliff in dislocated glacial deposits. Surface-forming stages in late- and post-glacial period. III. Ground moraine, deposited discordantly over dislocated meltwater deposits. IV. Deflation-plain, the result of removal of fine-grained moraine components by the alnd surface and inducing the formation of a humification horizon over stones. VI. Blown sand covering other deposits. D2. Stones. E. Humus horizon. F. Blown sand. In this substratum the present cliff was formed by the action of the sea and atmospheric forces. Source: Atlas of Denmark.

Cliff in dislocated glacial deposits.

Cliff in dislocated glacial deposits. Present stage. 1. Precipice in continuous clay secions. 2. Screes. 3. Gullies between clay walls formed by the slipping sand beds, erosion of running water and wind action. 4. Beach, low tide. 5. Slide plane in screes caused by wave action. 6. Rain gulley. 7. Cone deposited sand. 8. Accumulation of blawn sand above gully. 9. Dune landscape. 10. Ridge formation through intersection of clay with surface. B-G, see slides 60-62. Source: Atlas of Denmark.

Climate

Climate. Generalized graph of temperature variation since the Precambrian. Kummell, 1961, p. 469.

Climate

Climate. Past positions of the February marine isotherms along the Pacific Coast of North America. Kummell, 1961, p. 475.

Close up contact between middle stratified drift and Leinan Till

Close up contact between middle stratified drift and Leinan Till. Lower part of Middle stratified drift is covered by slope wash. Swiift Current Creek section along north sside of tributary to Swift Current Creek in Sec. 10, T. 19, R. 13, W. 3 meridian. Tuesday September 13, 1960.

Close up of Flaxville Pliocene (?) gravels at base overlain by basal till

Close up of outcrop showing Flaxville Pliocene (?) gravels at base overlain by about 1 foot basal till and about 6 feet of stony ablation till with stony concentration at base unit. Jack Brandt in picture. South edge of Loring Plateau where road descends into the Milk River Valley, outcrop along Loring-Malta road. April 1964.

Results 286 to 300 of 1974