Sentence examples for range bedrock from inspiring English sources

The range bedrock mass movement types within Varnes-based landslide classification scheme are also reviewed.

Three case studies, Seymareh (Iran, La Clapière Francece), and Threatening Rock (United States), are presented in detail to illustrate the range of bedrock mass movement types and characteristics presented in this chapter.

The steady position of the grounding line, obtained from our SPH simulations, is in good agreement with laboratory observations for a wide range of bedrock slopes, ice-to-fluid density ratios, and flux.

Fifteen non-cultivated, shallow and leached mountain pedons were sampled in Israel along three transects that represent various rainfall ranges and bedrock lithologies.

It has been reported that the bedrock range has developed from shallow rankers to well-developed cambisols and fluvisols in the stream valleys [35].

Maximum U Th/4He ages obtained for the groundwater in the fractured bedrock range from 1473 ± 300 a to 137 ± 28 ka, suggesting the occurrence of several generations of fossil meltwater trapped under the clay plain after the last two glaciations.

A 120 m hilltop transect on Bodmin Moor, southwest UK, displays a parabolic hilltop form, which implies it is in geomorphic steady state, yet the measured depths to bedrock range almost 6-fold from 14 to 80 cm, and the soil production rates derived from 10Be concentrations in rock at the soil interface range by 2-fold from 10 to 20 m/My.

Sample sites were selected to include a range of distinct bedrock geologies (e.g. Proterozoic complex: northwest Ontario, Mesozoic sediments: Manitoba, and Cenozoic volcanics: Oregon) and cover a range of known δD values in precipitation from Alaska to southeastern US [12], [14], while ensuring samples could be collected in a single season to eliminate year effects.

The strontium isotope surrounding the Cambrian and Ordovician carbonate bedrock ranged from 0.7096 to 0.7140 (Liu et al. 2007).

The density of oxidized, fractured bedrock ranges from 2.7 to about 2.2 g cm− 3, saprolite and grus have densities between ∼2.0 and 1.8 g cm− 3, and 30 soil samples averaged 1.6 ± 0.2 g cm− 3.

The bedrock bedforms range from plastically moulded (p-forms) and wholly abraded forms, to stoss lee forms and plucked surfaces all on an outcrop scale (1 100 m).