Results 121 to 130 of about 13,538 (295)
Boreas, EarlyView.The characteristics of settlement of Neanderthals in northern Central Europe during the earlier phases of the Middle Palaeolithic (Marine Isotope Stage 8–6) have been a matter of debate for decades, specifically regarding the population dynamics at such latitudes during the coldest phases. In this paper, we review the known archaeological record of the
Gianpiero Di Maida +5 more
wiley +1 more source
DEVELOPMENT OF LANDFORM CLASSIFICATION USING DIGITAL ELEVATION MODEL
, 1994 Inclination of the trend surface, the frequency of ridges and valleys, and the frequency of the break of inclination were abstracted from the digital topographical map (DEM) to make an automated landform classification. It was found that current landform
岩橋, 純子
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Boreas, EarlyView.We present a 25‐stage reconstruction of the ice‐flow pattern evolution of the Scandinavian Ice Sheet based on mapping and analysis of ~240 000 subglacial lineations and lineation fields across Norway, Sweden, Finland, and parts of NW Russia. Our reconstruction uses a glacial geomorphological inversion approach, in which we generated 611 individual ...
Frances E. G. Butcher +9 more
wiley +1 more source
Touristic aspects of landform geodiversity in Carpathians
, 2010 Artykuł przedstawia metody uzyskiwania mapy georóżnorodności rzeźby w środowisku GIS-owskim oraz jej wykorzystanie do wskazania atrakcji turystycznych w Karpatach. Zaproponowano metodyczny schemat postępowania.
Zwoliński, Z.
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Landform evolution in Australasia [PDF]
, 2017 A reappraisal of landform evolution in Australasia is both timely and necessary. Over a decade has elapsed since the publication of Landform Studies from Australia and New Guinea edited by J.N. Jennings and J.A.
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Palaeowinds and depositional conditions from Holocene loess in Sweden and Finland
Boreas, EarlyView.The nature of deglacial and Holocene wind regimes in Fennoscandia is debated, as is the degree to which wind‐blown loess deposits exist in the region. Loess deposits in Fennoscandia are often relatively thin, discontinuous and less well‐sorted than typical loess, and questions remain over the degree of their post‐depositional reworking and the impact ...
Calum J. Edward +6 more
wiley +1 more source
Boreas, EarlyView.Map of Lower sediment (LS) thickness is a surrogate for the distribution of Thorncliffe Formation (TF) and ~75% of TF thickness from the slope of Niagara Escarpment east to Brighton. Inset images show the LS sequence at the Don Valleys brickyards (DVBY) and undeformed TF sand and gravel (~15 m) below Newmarket Till (NT) at sites L and Co.
David R. Sharpe +3 more
wiley +1 more source
WILSIM (Web-based Interactive Landform Simulation Model)
, 2002 WILSIM is a web-based interactive landform simulation model that is designed to improve students' learning experience of landform evolution. It is a Java Applet and can be accessed anytime and anywhere via a standard java enabled web browser.
Wei Luo
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Landform classes in the conterminous USA at different resolutions.
, 2016 Landform classes in the conterminous USA at different resolutions.
Dylan Harrison-Atlas (834220) +3 more
core +1 more source
Boreas, EarlyView.Effective and sustainable land use, conservation, and the use of geological resources (incl. raw materials, aggregates and groundwater) require a clear classification system of sedimentary units, with well‐defined vocabulary and unified mapping practices.
Jussi Hovikoski +6 more
wiley +1 more source