A periglaciális környezet felszínalakulása 2. rész

Many phenomena can undoubtedly be connected to freezing and thawing but cannot be clearly linked to a subsurface form of ice and were created due to complex processes. Their explanation is uncertain, often hypothetical and contradictory. To these phenomena belong the layer disturbances (cryoturbation), slope mass movements and nivation processes. Finally, a brief overview of the consequences of global warming can be read.

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Publication Details

Journal
GeoMetodika
Published
2025-01-01
DOI
https://doi.org/10.26888/geomet.2025.9.2.2
Primary Topic
Hungarian Social, Economic and Educational Studies
Type
article
Field-Weighted Citation Impact
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article

A periglaciális környezet felszínalakulása 2. rész

Gyula Gábris
GeoMetodika
Hungarian Social, Economic and Educational Studies
article

A periglaciális környezet felszínalakulása 2. rész

Gyula Gábris
article en

Abstract

Many phenomena can undoubtedly be connected to freezing and thawing but cannot be clearly linked to a subsurface form of ice and were created due to complex processes. Their explanation is uncertain, often hypothetical and contradictory. To these phenomena belong the layer disturbances (cryoturbation), slope mass movements and nivation processes. Finally, a brief overview of the consequences of global warming can be read.

GeoMetodikaVol. 9(2)
Openalex Percentile: Top 88%
Hungarian Social, Economic and Educational Studies
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A periglaciális környezet felszínalakulása 2. rész — Gyula Gábris · GeoMetodika (2025) | TGRS Research Map | TGRS