Results 21 to 30 of about 202 (159)

Complex genesis of N-channel eskers illustrated with the example of an esker near Tosie (east-central Poland)

open access: yesActa Universitatis Lodziensis. Folia Geographica Physica, 2021
The study presents the problem of complex genesis of eskers formed in N-channels on the example of an esker located near Tosie in east-central Poland.
Małgorzata Frydrych
doaj   +1 more source

Diamicton facies in the vicinity of Duhlata cave, Bosnek karst region, Southwestern Bulgaria

open access: yesReview of the Bulgarian Geological Society, 2021
Karst caverns in the Upper Triassic dolostones of the Rusinovdel Formation are filled with allochthonous clastics (brecciaconglomerates with maximum boulder size) and locally with speleothems (flowstones). Deposition of the former (diamicton facies) by debris flows resulted from extreme flood events along the upper reaches of Struma river. The polymict
Athanas Chatalov, Dilyana Hristova
openaire   +1 more source

The origin of water‐borne diamictons and their relation to turbidites [PDF]

open access: yesNew Zealand Journal of Marine and Freshwater Research, 1967
Summary The term “diamicton” has recently been proposed as a non‐genetic name for any non‐calcareous terrigenous sediment containing a wide variety of grain sizes; the lithified equivalent is a “diamictite.” The present paper deals with the origin and classification of water‐borne diamictons. The latter have been divided by the writer
openaire   +1 more source

Sedimentological characteristics of debris flow Deposits within ice−cored moraine of Ebbabreen, central Spitsbergen

open access: yesPolish Polar Research, 2015
The Ebbabreen ice−cored moraine area is covered with a sediment layer of up to 2.5 m thick, which mostly consists of massive diamicton. Due to undercutting by lateral streams, debris flow processes have been induced in marginal parts of this moraine.
Pleskot Krzysztof
doaj   +1 more source

A glaciotectonic landform in the Shyok valley, Trans-Himalayan Karakoram Range, India

open access: yesJournal of Glaciology
This study reports and discusses the first case of glaciotectonic landforms in the Shyok valley of the Trans-Himalayan Karakoram Range, Ladakh, where a large decomposed granite megablock (8.2 km2) along with underlying diamicton is thrust over the ...
Abdul Qayoom Paul   +2 more
doaj   +1 more source

Distinguishing characteristics of Diamictons at the Margin of the Matanuska Glacier, Alaska [PDF]

open access: yesAnnals of Glaciology, 1981
The origins of diamictons deposited at the Matanuska Glacier are identified in stratigraphic sequences mainly by the presence or absence of a pebble fabric, internal structure, and variation in gravel-size clast distribution. These properties correlate with major differences in depositional mechanisms and source material.
openaire   +1 more source

Depositional dynamics in the El'gygytgyn Crater margin: implications for the 3.6 Ma old sediment archive [PDF]

open access: yesClimate of the Past, 2012
The combination of permafrost history and dynamics, lake level changes and the tectonical framework is considered to play a crucial role for sediment delivery to El'gygytgyn Crater Lake, NE Russian Arctic.
G. Schwamborn   +5 more
doaj   +1 more source

A lee-side cavity fill diamicton under the Durance valley glacier: Insights from hoodoos of the Remollon Arch, Southern French Alps

open access: yesSedimentologika
Deep and narrow gullies dissecting reliefs of the Southern French Alps are filled with 10's to 100's meters thick accumulation of unsorted, boulder-rich muddy material (i.e., diamicton) left behind by glaciers that repeatedly covered the region during ...
Pierre Dietrich, Alexis Nutz
doaj   +1 more source

Timing of speleogenesis of Las Karmidas Cave (Mexico): first description of pseudokarst developed in ignimbrite

open access: yesInternational Journal of Speleology, 2017
Las Karmidas Cave (Puebla State, Mexico) is an unusual type of pseudokarstic cavity generated by piping and erosive processes within the contact of a diamicton and an overlying Quaternary ignimbrite.
María del Pilar Aliaga-Campuzano   +5 more
doaj   +1 more source

Ice-crevasse sedimentation in the eastern part of the Głubczyce Plateau (S Poland) during the final stage of the Drenthian Glaciation

open access: yesOpen Geosciences, 2020
Glacial sediments in the eastern part of the Głubczyce Plateau, at the Krowiarki site, were studied. Two units were distinguished within the sedimentary succession.
Salamon Tomasz
doaj   +1 more source

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