Wyniki wyszukiwania

1

Permafrost terminology

100%

Brown R. J. E., Kupsch W. O.

Biuletyn Peryglacjalny

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1992

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tom 32

2

Symptoms of the permafrost presence in Middle Poland during the last 150 000 years

86%

Klatkowa H.

Biuletyn Peryglacjalny

|

1996

|

tom 35

3

Application of DC resistivity soundings and geomorphological surveys in studies of modern Arctic glacier marginal zones, Petuniabukta, Spitsbergen

72%

Gibas J., Rachlewicz G., Szczucinski W.

Polish Polar Research

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2005

|

tom 26

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nr 4

239-258

C resistivity soundings and geomorphological surveys have been carried out in the marginal zones and adjacent outwash plains of two glaciers in central Spitsbergen, Norwegian Arctic: Ebbabreen and Horbyebreen. The study has revealed complex relationships between landforms, buried glacier ice and permafrost. From this work it is possible to distinguish between moraine ridges which are ice-cored and those which are not. The latter occur in areas which have possibly been affected by glacier surge. The active layer thickness was found to be 0.4 to 2.5 m for diamicton deposits (moraines) and 0.3 to 1.6 m in outwash glacifluvial sediments. The sediment infill thickness in valleys was determined to be as much as 20 m, thereby demonstrating that sandurs have important role in sediment storage in a glacial system. Typical resistivity values for sediment types in both the active layer and in permafrost were also determined.

4

Permafrost advances at Yellowknife, Canada: report of the seventh international conference on permafrost

72%

French H. M., Dobinski W.

Biuletyn Peryglacjalny

|

1998

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tom 37

5

Le probleme de l'extension et de la profondeur du pergelisol pleistocene en Normandie [France du nord-ouest]

72%

Lautridou J. P., Coutard J. P.

Quaestiones Geographicae. Zeszyt Specjalny

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1995

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tom 04

6

Comments and observations on the application of resistivity sounding in the research of permafrost

72%

Moscicki J. W., Kedzia S.

Biuletyn Peryglacjalny

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2000

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tom 39

7

Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik

Relic cryogenic indicators of diagnostic horizons in rusty and parabrown soils in European Lowland

72%

Kowalkowski A.

Acta Agrophysica

|

2001

|

tom 50

In the last Vistulian glacial period, the profiles of periglacial perstructions and the profiles of old cryosols were formed in the extra glacial and gradually released from retreating continental glacier regions, originally in conditions of over 6-8 ka existing arctic desert before approximately 14.5 ka, and then from 14.5 to 10.5 ka BP, in the changing short rhythms of glacier deserts, shrub and park tundras as well as in short lasting pine-birch and birch forests. The whole profile thickness of the remaning periglacial horizons of the pleistocene paleosoils at the earth surface consists of a sequence or series of periglacial frost perstruction zones. In the cryogenic perstruction process of surface and subsurface sediment layers in the periglacial environment there were diagnostic horizons - cryosideric - crBv, cryoargillic - crBt, and cryospodic - crBk formed. Their localisation in the perstruction profile, in the soil horizons profile and the grain size profile, with readily recognisable associations of cold climate characteristics, may be used for quantification and diagnosis of rusty and parabrown paleosoils in the framework of superordinatektaxonomic unit of paleocryosols.

8

Memories from the 1096's S.Jan Dylik and periglacial researchin Spitsbergen and Lappland

72%

Rapp A.

Biuletyn Peryglacjalny

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1998

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tom 37

9

Histoire et dynamique du pergelisol europeen au Weichselien

72%

Van Vliet-Lanoe B.

Biuletyn Peryglacjalny

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1994

|

tom 33

10

Permafrost, real estate, and climate change: The case of Thompson, Northern Manitoba, Canada

72%

French H. M.

Biuletyn Peryglacjalny

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1998

|

tom 37

11

The periglacial impact on the deglaciated area of Northern Poland after 20 KYR BP

72%

Kozarski S.

Biuletyn Peryglacjalny

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1995

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tom 34

12

The thermal condition of the active layer in the permafrost at Hornsund, Spitsbergen

58%

Leszkiewicz J., Caputa Z.

Polish Polar Research

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2004

|

tom 25

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nr 3-4

223-239

13

Permafrost evolution and its impact on deposition conditions between 20 and 10 ka BP in Poland

58%

Gozdzik J. S.

Biuletyn Peryglacjalny

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1995

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tom 34

14

Relict Late Quaternary permafrost on a former nunatak at Plateau Mountain, S.W.Alberta, Canada

58%

Harris S. A.

Biuletyn Peryglacjalny

|

1997

|

tom 36

Ograniczanie wyników

Permafrost terminology

Symptoms of the permafrost presence in Middle Poland during the last 150 000 years

Application of DC resistivity soundings and geomorphological surveys in studies of modern Arctic glacier marginal zones, Petuniabukta, Spitsbergen

Permafrost advances at Yellowknife, Canada: report of the seventh international conference on permafrost

Le probleme de l'extension et de la profondeur du pergelisol pleistocene en Normandie [France du nord-ouest]

Comments and observations on the application of resistivity sounding in the research of permafrost

Relic cryogenic indicators of diagnostic horizons in rusty and parabrown soils in European Lowland

Memories from the 1096's S.Jan Dylik and periglacial researchin Spitsbergen and Lappland

Histoire et dynamique du pergelisol europeen au Weichselien

Permafrost, real estate, and climate change: The case of Thompson, Northern Manitoba, Canada

The periglacial impact on the deglaciated area of Northern Poland after 20 KYR BP

The thermal condition of the active layer in the permafrost at Hornsund, Spitsbergen

Permafrost evolution and its impact on deposition conditions between 20 and 10 ka BP in Poland

Relict Late Quaternary permafrost on a former nunatak at Plateau Mountain, S.W.Alberta, Canada