Results 231 to 240 of about 1,994 (297)

Explanation of the influence of geomorphometric variables on the landform classification based on selected areas in Poland. [PDF]

Sci Rep
Dyba K.
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Convergent morphological and genetic patterns delimit Evolutionary Significant Units in endangered Aipysurus sea snakes. [PDF]

BMC Ecol Evol
Nankivell JH, Sanders KL.
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Past intrusion of Circumpolar Deep Water in the Ross Sea: Impacts on the ancient Ross Ice Shelf. [PDF]

Sci Adv
Pambianco C, Nogarotto A, Sabino M, Capotondi L, Battaglia F, Giglio F, Mollenhauer G, Hefter J, Di Roberto A, Belt ST, Pochini E, Muschitiello F, Geniram A, Colizza E, Giorgetti G, Torricella F, Tesi T.   +16 more
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Physiographic Environment Classification: a Controlling Factor Classification of Landscape Susceptibility to Waterborne Contaminant Loss. [PDF]

Environ Manage
Rissmann CWF, Pearson LK, Snelder TH.
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Provenance of late Pleistocene loess in central and eastern Europe: isotopic evidence for dominant local sediment sources. [PDF]

Sci Rep
Fenn K, Millar IL, Bird A, Veres D, Wagner D.   +4 more
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Glacial geomorphology: Towards a convergence of glaciology and geomorphology

Progress in Physical Geography: Earth and Environment, 2010
This review presents a perspective on recent trends in glacial geomorphological research, which has seen an increasing engagement with investigating glaciation over larger and longer timescales facilitated by advances in remote sensing and numerical modelling.
Bingham, Robert G., King, Edward C., Smith, Andrew M., Pritchard, Hamish D.   +3 more
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Glacial Geomorphology at Glasgow

Scottish Geographical Journal, 2009
Abstract This paper reviews a century of geographical contributions at the University of Glasgow to the development of glacial geomorphology. Significant advances were made from the 1960s, when geographers and topographic scientists began to combine geomorphic and survey expertise in accurately charting spatial and temporal changes in Icelandic glacier
openaire   +2 more sources

Buried Glacial Geomorphology

1982
Most glacial deposits are made of different materials deposited at different times. The surface of the latest deposit is the present land surface — the present geomorphology. The surface of each buried deposit is a surface of paleogeomorphology, either entirely depositional, entirely erosional, or partly of each.
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Glacial geomorphology and geographic information systems

Earth-Science Reviews, 2007
Recent developments in the field of glacial geomorphology have dramatically increased the need to acquire, maintain, manipulate, and analyze large amounts of landform, landscape and sediment data. The use of Geographic Information Systems (GIS) has provided new platforms and tools for analysis and visualization of geomorphic data.
Jacob Napieralski, Jon Harbor, Yingkui Li   +2 more
openaire   +1 more source