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Terrace (geology)
The tread and the steeper descending slope (riser or scarp) together constitute the terrace. Terraces can also consist of a tread bounded on all sides by a ... More »
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bulletin.geoscienceworld.org/content/95/12/1413.full.pd... bulletin.geoscienceworld.org/content/95/12/1413.full.pdf
measurements of a sequence of terrace scarps along the ..... terrace formation ( the segment of the terrace scarp T6', upstream from the fault, is higher than ...
gsabulletin.gsapubs.org/content/95/12/1413
Analysis of fault and fluvial terrace scarps in the West Yellowstone Basin south of Hebgen Lake, Montana, indicates that, during degradation, the gradient of the ...
linkinghub.elsevier.com/retrieve/pii/S0169555X05003028
The widely used linear diffusion model for hillslope evolution does not accurately predict the degradation of terrace scarps produced by the Late Pinedale West ...
onlinelibrary.wiley.com/doi/10.1002/esp.3290080303/pdf
KEY WORDS Landform evolution Terraces Scarps Rappahannock River. INTRODUCTION. The impetus for this study resulted from two lines of current ...
onlinelibrary.wiley.com/doi/10.1111/j.1751-8369.1987.tb... onlinelibrary.wiley.com/doi/10.1111/j.1751-8369.1987.tb00354.x/abstract
May 5, 2007 ... SWETT, K. and MANN, K. (1987), Terrace scarp deflation as a renewable source for eolian sediments in an arctic periglacial setting.
www.polarresearch.net/index.php/polar/article/download/... www.polarresearch.net/index.php/polar/article/download/6867/7700
Swett K. & Mann K., 1986: Terrace scarp deflation as a renewable source for eolian sediments in an arctic periglacial setting. Polar Research 5 n.s.. 45-52.
whipple362.asu.edu/papers/pierce_colman_gsab86.pdf
Terrace scarps can serve as a nearly ideal natural laboratory tor the study of the ... Late Pleistocene terrace scarps now as steep as 33.25“. as well as moasllrtifl ...
serc.carleton.edu/vignettes/collection/37941.html
Feb 1, 2011 ... The red arrow marks the position of the cutbank shown in Figure 3, and the blue arrow marks the terrace scarp (between terraces 1 and 2), ...
www.sciencedirect.com/science/article/pii/0033589476900... www.sciencedirect.com/science/article/pii/0033589476900429
Terrace scarps may be from 1 to 75 m high. Terraces are cut into all ... Cryoplanation terraces form by scarp retreat as the result of nivation. Surficial debris is ...
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