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Showing 1 - 20 results of 69 for search '"bedrock"', query time: 2.69s Refine Results
  1. 1
    ...Bedrock mega-grooves are assemblages of straight and parallel troughs eroded in bedrock, typically...
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  2. 2
    ... to reconstruct the ice margin during warm intervals of the Oligocene–Miocene. Flat‐lying bedrock plateaus...
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  3. 3
    ...This paper investigates the controls on the formation of subglacially eroded bedrock bedforms...
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  4. 4
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    ... deformation rates, and a suite of modeled viscous rates, from GPS-derived three-dimensional bedrock velocities...
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  7. 7
    by Roberts, D. H., Long, A. J.
    Published in Boreas (2005)
    ...This study investigates the marginal subglacial bedrock bedforms of Jakobshavns Isbrae, West...
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  8. 8
  9. 9
    ... of the Bannow Till. Three sedimentary units at Bannow comprise a vertical continuum of sheared bedrock...
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  10. 10
    ... glacitectonic compression of bedrock, cupola hill construction and mega raft displacement but also displays...
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  11. 11
    by Long., A. J., Roberts, D. H.
    Published in Boreas (2003)
    ... deglaciation after 10.3rka cal. yr BP. Once deglaciation began, a bedrock high in the west of the bay exerted...
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  12. 12
    ...), mainly bedrock, (ii), part bedrock/part till; (iii), mainly till; (iv), part till/part sorted sediments...
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  13. 13
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    ...This paper presents the results of a detailed multidisciplinary study of the deformed bedrock...
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  15. 15
    ... networks of huge channels carved into bedrock (now submarine) on the Pacific margin of West Antarctica...
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  16. 16
    ... that the range of Re in river sediments (∼0.30‰) is controlled by a combination of source bedrock isotopic...
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  17. 17
    ... identified in addition to bedrock, glacier ice and made ground associated with pumice mining. The spatial...
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  18. 18
    ... of the spatial variability in landform-sediment imprints of catastrophic glacier advance across upland bedrock...
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  19. 19
    ... primary causes of ‘stickiness’: (i), bedrock bumps; (ii), till-free areas; (iii), areas of ‘strong’ (well...
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  20. 20
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