Results 121 to 130 of about 18,588 (223)

Geomorphology of marine and glacio-lacustrine terraces and raised shorelines in the northern sector of Península Brunswick, Patagonia, Straits of Magellan, Chile

Journal of Maps, 2018
This paper illustrates a detailed geomorphological map (scale 1:50,000) of the marine and transitional terraces (glacio-lacustrine to marine) and raised shorelines linked to Holocene glacio-eustasy and neo-tectonics in the northern area of the Brunswick ...
Sandro De Muro, Sira Tecchiato, Marco Porta, Carla Buosi, Angelo Ibba   +4 more
doaj   +1 more source

Climate evolution during the Pleniglacial and Late Glacial as recorded in quartz grain morphoscopy of fluvial to aeolian successions of the European Sand Belt

Geologos, 2015
We present results of research into fluvial to aeolian successions at four sites in the foreland of the Last Glacial Maximum, i.e., the central part of the “European Sand Belt”.
Woronko Barbara, Zieliński Paweł, Sokołowski Robert Jan   +2 more
doaj   +1 more source

Inner forearc sequence architecture in response to climatic and tectonic forcing since 150 ka : Hawhe's Bay, New Zealand

, 2009
International audienceThe influence of eustasy, tectonic deformation, and sediment flux as controlling parameters on basin stratigraphy and depositional sequence development are largely accepted. Eustasy is usually considered as the dominant mechanism of
Barnes, P.M., Paquet, Fabien, Pettinga, J.R., Proust, Jean-Noël   +3 more
core   +4 more sources

Geomorphology of the mouth of the Arosa estuary (Coruña-Pontevedra, Spain)

Journal of Maps, 2017
This paper presents a geomorphological analysis of the littoral zone of the Arosa-Pontevedra estuary mouth and identifies geomorphological units and categorizes them into morphogenetic systems.
A. M. Martinez-Graña, L. Arias, J. L. Goy, C. Zazo, P. Silva   +4 more
doaj   +1 more source

Suelos y morfología en el parque natural de los montes de Málaga [PDF]

, 1996
[Resumen] Los suelos observados y analizados en el Parque Natural de los "Montes de Málaga", a escala 1:10.000, presentan estrecha dependencia con la morfología, tanto directamente (laderas, cumbres, rellanos, terrazas, ...) como indirectamente a través ...
Ferré Bueno, E., Senciales González, J. M.   +1 more
core   +1 more source

Frequency Distributions of Median Nutrient and Chlorophyll Concentrations across the Red River Basin, 1996-2006 [PDF]

, 2009
Acquisition and compilation of water quality data for a ten year time period (1996 – 2006) from 589 stream and river stations was conducted to support nutrient criteria development for the multi–state Red River Basin shared by Arkansas, Louisiana, New ...
Haggard, B.E., Longing, S.D.
core   +2 more sources

Differential uplift and incision of the Yakima River terraces, central Washington State [PDF]

, 2015
Amos, CB, Bender, AM, Bierman, P, Kelsey, H, Rood, DH, Sherrod, B, Staisch, L   +6 more
core   +1 more source

Evolution Of Vegetation, Relief And Geology In Central Poland Under Anthropopressure [PDF]

, 2014
Published in: Origin of Relief of Central Poland and Its Anthropogenic Transformation in Łódź University Geographical Research, edited by. E.Kobojek, T.MarszałThe review of the localities with biogenic, slope, fluvial and aeolian deposits in which the ...
Forysiak, Jacek, Kittel, Piotr, Twardy, Juliusz   +2 more
core  

Chronological Study of Fluvial Terraces along the Jusu River, Eastern Korea

Kikan Chirigaku, 1993
A series of fluvial terraces is well developed along the Jusu River flowing into the eastern side of the Taebaek Mts., Korea. Among these terraces, the development of the most well-preserved lower terraces were examined in connection with the climatic and sea-level changes since Last Interglacial by an investigation into the deposits and longitudinal ...
openaire   +2 more sources

Palaeochannels of the upper central Murray and lower Goulburn rivers, southeastern Australia

Journal of Maps
Palaeochannel systems are characteristic of alluvial plains across large parts of the Australian continent, but their evolution and modes of formation are still only partly understood.
Daniela Mueller, Tim J. Cohen, Ivars V. Reinfelds   +2 more
doaj   +1 more source