Results 21 to 30 of about 162 (154)

Submarginal drumlin formation and late Holocene history of Fláajökull, southeast Iceland

open access: yesAnnals of Glaciology, 2016
Fláajökull is a non-surging outlet glacier draining the south-eastern part of the Vatnajökull, southeast Iceland. Fláajökull was stationary or advanced slightly between 1966 and 1995 and formed a prominent end moraine.
Sverrir Aðalsteinn Jónsson   +6 more
doaj   +1 more source

Drumlins [PDF]

open access: yesScience, 1884
Mode of access: Internet.
openaire   +2 more sources

Erosive features caused by a Magellanic penguin (Spheniscus magellanicus) colony on Martillo Island, Beagle Channel, Argentina

open access: yesCuadernos de Investigación Geográfica, 2020
An active Magellanic penguin (Spheniscus magellanicus) colony has been established on Martillo Island, Beagle Channel (54°54´26” S; 67°22´58” W) since 1976.
D.R.A. Quiroga   +7 more
doaj   +1 more source

Subglacial landforms beneath Rutford Ice Stream, Antarctica: detailed bed topography from ice-penetrating radar [PDF]

open access: yesEarth System Science Data, 2016
We present a digital elevation model of the bed of Rutford Ice Stream, Antarctica, derived from radio-echo sounding data. The data cover an 18  ×  40 km area immediately upstream of the grounding line of the ice stream.
E. C. King, H. D. Pritchard, A. M. Smith
doaj   +1 more source

Superimposed Drumlins [PDF]

open access: yesJournal of Glaciology, 1977
AbstractDrumlins in parts of central Scotland and east Cumbria form two populations according to their size. In certain cases the small features are superimposed on the large. Drumlins, superimposed drumlins, and megadrumlins are considered to be part of a continuum of glacier bed forms, which is the product of changes in the stress applied by glaciers
J. Rose, J. M. Letzer
openaire   +1 more source

Enigmatic glacigenic ridges from the Odra Glaciation in the vicinity of Krzepice (Woźniki-Wieluń Upland, Poland)

open access: yesEnvironmental & Socio-economic Studies, 2016
The central part of the Woźniki-Wieluń Upland is characterised by mature old glacial landforms associated with the Middle- Polish Glaciations. In some areas, however, more pronounced post-glacial landforms can be observed that were remodelled by later ...
Waga Jan Maciej, Fajer Maria
doaj   +1 more source

AN GEOLOGICAL OVERVIEW OF GLACIAL ACCUMULATION AND EROSIONAL OCCURRENCES AT THE VELEBIT AND THE BIOKOVO MTS., CROATIA

open access: yesRudarsko-geološko-naftni Zbornik, 2017
Numerous accumulation and erosional forms originating from the activity of small valley glaciers or cirque glaciers occur in the highest mountains in Croatia: Velebit (1757 m) and Biokovo (1762 m).
Josipa Velić   +5 more
doaj   +1 more source

Bewegungen des Inlandeises im Lohja—Seebecken, Südfinnland [PDF]

open access: yesBulletin of the Geological Society of Finland, 1971
About 760 glacial striae measurements made on polished bedrock outcrops indicate variations in the direction of the movement of Fennoscandian ice-stream in the lake basin of Lohjanjärvi, South Finland.
G. Glückert
doaj   +1 more source

Drumlin relief

open access: yesGeomorphology, 2012
AbstractDrumlin relief is a key parameter for testing predictions of models of drumlin formation. Although this metric is commonly described in textbooks as being of the order of a few tens of metres, our critical review of the literature suggests an average value of about 13m, but with much uncertainty.
Spagnolo, Matteo   +2 more
openaire   +3 more sources

Zur Struktur von Eskern in Schleswig-Holstein, unter besonderer Berücksichtigung des „Esker-Kames-Systems Forst Steinburg“ in morphologischer Hochlage [PDF]

open access: yesEiszeitalter und Gegenwart, 2011
Die unterschiedlichen Esker-Formen Schleswig-Holsteins wurden für das Geotop-Kataster des Landes mittels Literatur- und Feldarbeiten neu bearbeitet: Esker i.e.S., Aufpressungs-Esker mit Kern aus Geschiebemergel oder Beckensedimenten, Perlenschnur-Esker ...
A. Grube
doaj   +1 more source

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