Paraglaciar , la enciclopedia libre

Paraglaciar quiere decir condiciones de inestabilidad^[1] causadas por un tiempo de relajación considerable para procesos y patrones geomórficos tras tiempos de clima glacial.^[2] Más precisamente el término refiere a procesos no glaciales condicionados por glacianes en lugares recientemente liberados de glaciares.^[3] ^[4]

Véase también[editar]

Referencias[editar]

↑ Renwick, W.H. 1992: Equilibrium, disequilibrium, and nonequilibrium landforms in the landscape. Geomorphology 5, 265-76
↑ Church, Michael and June M Ryder, Paraglacial Sedimentation: A Consideration of Fluvial Processes Conditioned by Glaciation, GSA Bulletin; October 1972; v. 83; no. 10; p. 3059-3072
↑ Benn, Douglas I. y Evands, David J.A. 1998. Glaciers and glaciation. Arnold. Pág. 261-269
↑ Slaymaker O., 2011. Criteria to distinguish between periglacial, proglacial and paraglacial environments. Quaestiones Geographicae 30(1): 85–94. DOI 10.2478/v10117-011-0008-y.

Datos: Q3895117

[1] Renwick, W.H. 1992: Equilibrium, disequilibrium, and nonequilibrium landforms in the landscape. Geomorphology 5, 265-76

[2] Church, Michael and June M Ryder, Paraglacial Sedimentation: A Consideration of Fluvial Processes Conditioned by Glaciation, GSA Bulletin; October 1972; v. 83; no. 10; p. 3059-3072

[Benn1-3] Benn, Douglas I. y Evands, David J.A. 1998. Glaciers and glaciation. Arnold. Pág. 261-269

[4] Slaymaker O., 2011. Criteria to distinguish between periglacial, proglacial and paraglacial environments. Quaestiones Geographicae 30(1): 85–94. DOI 10.2478/v10117-011-0008-y.

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