Several glacially carved troughs with depths exceeding 1 km below sea level have been mapped using sonar in the continental shelf offshore from western Mar... DS Wilson,BP Luyendyk,CC Sorlien,... - AGU Fall Meeting Abstracts 被引量: 3发表: 2001年 Monitoring of east antarctic marginal zone ...
Application of Earth Observation Techniques at Pasterze Glacier: Data Basis, Spatial and Temporal Variability, Quality Assessment Results: Monitoring of Processes and Landforms Discussion Synopsis: Processes/Landforms and Data Acquisition Conclusions Author Contributions Funding Acknowledgments Conflicts of Interest...
along the coast of North and South America, crosses the equator until it reaches the circumpolar region south of the tip of Africa where it flows over the even denser Antarctic Bottom Water (AABW). Meanwhile, the Circumpolar Deep Water (CDW) "penetrates onto the relatively deep continental ...
The continental significance of this geomorphosite is complemented by the remarkable petrographic diversity of the granitoids of the Rila-West Rhodopes Batholith and metamorphic rocks contained therein, intersected by numerous pegmatite, aplite and quartz veins, vein-like granite bodies, diorite, and...
Stress estimates indicate this ongoing faulting is driven by NW–SE oriented maximum horizontal stress (SHmax), resulting from continued continental convergence and anti-clockwise rota- tion of the Adriatic plate (Hubbard and Mancktelow 1992; Maurer et al. 1997; Pleuger et al. 2012). Although ...
erosion. Furthermore, variations in melt water discharge also play an important role in the development of glacial landforms (Eyles2006; Salcher et al.2009). Estimates of the volume/rate of melt water release, assessment of the character of the drainage pathways beneath continental ice sheets, ...
According to the Köppen climate classification, they belong to the continental temperate climate zone. The Tatra Mountains constitute a natural orographic barrier to the advection of air masses from the Atlantic Ocean to Central Europe. The climatic conditions depend mainly on altitude and to a ...
Lake District to the east, and the Olsztyn Lake District to the west. In terms of geomorphology the region is situated within the reach of the last glaciation formations and forms. The diversified hilly mosaic relief with a large number of lakes is the effect of glacier activity (Kondracki...
This paper aims to identify how the deglaciation of the fjord and plateau terrain of north Norway has influenced the glacial geomorphology and relative sea-level history of both local and adjacent areas and so serve as a model for interpreting similar areas along the continental margins of ...
Evidence of valley glaciers have been proposed for other locations in the Catskill Mountains at present there is not enough data to substantiate if the Willow Moraine developed as an independent valley glacier or as a sublobe of the Hudson Lobe continental ice.KOZLOWSKI, Andrew L...