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Small Scale Glacial Erosion Forms and their Possible Relation to Post-Glacial Weathering
The paper describes several types of small scale forms on the stoss side of a roche moutonnée surface, recently exposed in a gravel pit in the Fjärås bräcka complex, SW Sweden. The forms were filled with weathered rock debris. When excavated, they showed a striking resemblance to forms generally acc...
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Published in: | Geografiska annaler. Series A, Physical geography Physical geography, 1991, Vol.73 (1), p.1-7 |
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description | The paper describes several types of small scale forms on the stoss side of a roche moutonnée surface, recently exposed in a gravel pit in the Fjärås bräcka complex, SW Sweden. The forms were filled with weathered rock debris. When excavated, they showed a striking resemblance to forms generally accepted to be shaped by glacial/glaciofluvial erosion. In addition to these forms there were irregular cavities for instance smoothly rounded throughs and irregular rough surfaces resembling those claimed to be preglacial weathering forms. In spite of the few observations made, many small scale glacial erosion forms are likely to be the result of a three-step process i.e. glacial pressure deformation of the bedrock, subsequent weathering of the deformed rock, and finally excavation of the deformed rock by exogenic processes. Further on it seems probable that many rough surfaces of the type described in the paper are the result of glacial pressure deformation and subsequent weathering. |
doi_str_mv | 10.1080/04353676.1991.11880328 |
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The forms were filled with weathered rock debris. When excavated, they showed a striking resemblance to forms generally accepted to be shaped by glacial/glaciofluvial erosion. In addition to these forms there were irregular cavities for instance smoothly rounded throughs and irregular rough surfaces resembling those claimed to be preglacial weathering forms. In spite of the few observations made, many small scale glacial erosion forms are likely to be the result of a three-step process i.e. glacial pressure deformation of the bedrock, subsequent weathering of the deformed rock, and finally excavation of the deformed rock by exogenic processes. 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Series A, Physical geography</title><description>The paper describes several types of small scale forms on the stoss side of a roche moutonnée surface, recently exposed in a gravel pit in the Fjärås bräcka complex, SW Sweden. The forms were filled with weathered rock debris. When excavated, they showed a striking resemblance to forms generally accepted to be shaped by glacial/glaciofluvial erosion. In addition to these forms there were irregular cavities for instance smoothly rounded throughs and irregular rough surfaces resembling those claimed to be preglacial weathering forms. In spite of the few observations made, many small scale glacial erosion forms are likely to be the result of a three-step process i.e. glacial pressure deformation of the bedrock, subsequent weathering of the deformed rock, and finally excavation of the deformed rock by exogenic processes. Further on it seems probable that many rough surfaces of the type described in the paper are the result of glacial pressure deformation and subsequent weathering.</description><subject>Bedrock</subject><subject>Bgi / Prodig</subject><subject>Deformation</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Erosion</subject><subject>Europe</subject><subject>Exact sciences and technology</subject><subject>Excavations</subject><subject>Fysisk geografi</subject><subject>Glacial landforms</subject><subject>Glaciers</subject><subject>Marine and continental quaternary</subject><subject>Moraines</subject><subject>Outcrops</subject><subject>Physical Geography</subject><subject>Rocks</subject><subject>Scandinavian States. 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Finland</topic><topic>Surficial geology</topic><topic>Weathering processes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Franzén, Lars G.</creatorcontrib><creatorcontrib>Olvmo, Mats</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Periodicals Index Online Segment 22</collection><collection>Periodicals Index Online</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - West</collection><collection>Primary Sources Access (Plan D) - International</collection><collection>Primary Sources Access & Build (Plan A) - MEA</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Midwest</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Northeast</collection><collection>Primary Sources Access (Plan D) - Southeast</collection><collection>Primary Sources Access (Plan D) - North Central</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Southeast</collection><collection>Primary Sources Access (Plan D) - South Central</collection><collection>Primary Sources Access & Build (Plan A) - UK / I</collection><collection>Primary Sources Access (Plan D) - Canada</collection><collection>Primary Sources Access (Plan D) - EMEALA</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - North Central</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - South Central</collection><collection>Primary Sources Access & Build (Plan A) - International</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - International</collection><collection>Primary Sources Access (Plan D) - West</collection><collection>Periodicals Index Online Segments 1-50</collection><collection>Primary Sources Access (Plan D) - APAC</collection><collection>Primary Sources Access (Plan D) - Midwest</collection><collection>Primary Sources Access (Plan D) - MEA</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - Canada</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - UK / I</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - EMEALA</collection><collection>Primary Sources Access & Build (Plan A) - APAC</collection><collection>Primary Sources Access & Build (Plan A) - Canada</collection><collection>Primary Sources Access & Build (Plan A) - West</collection><collection>Primary Sources Access & Build (Plan A) - EMEALA</collection><collection>Primary Sources Access (Plan D) - Northeast</collection><collection>Primary Sources Access & Build (Plan A) - Midwest</collection><collection>Primary Sources Access & Build (Plan A) - North Central</collection><collection>Primary Sources Access & Build (Plan A) - Northeast</collection><collection>Primary Sources Access & Build (Plan A) - South Central</collection><collection>Primary Sources Access & Build (Plan A) - Southeast</collection><collection>Primary Sources Access (Plan D) - UK / I</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - APAC</collection><collection>Primary Sources Access—Foundation Edition (Plan E) - MEA</collection><collection>SwePub</collection><collection>SwePub Articles</collection><collection>SWEPUB Göteborgs universitet</collection><jtitle>Geografiska annaler. Series A, Physical geography</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Franzén, Lars G.</au><au>Olvmo, Mats</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Small Scale Glacial Erosion Forms and their Possible Relation to Post-Glacial Weathering</atitle><jtitle>Geografiska annaler. Series A, Physical geography</jtitle><date>1991</date><risdate>1991</risdate><volume>73</volume><issue>1</issue><spage>1</spage><epage>7</epage><pages>1-7</pages><issn>0435-3676</issn><issn>1468-0459</issn><eissn>1468-0459</eissn><coden>GAPGAP</coden><abstract>The paper describes several types of small scale forms on the stoss side of a roche moutonnée surface, recently exposed in a gravel pit in the Fjärås bräcka complex, SW Sweden. The forms were filled with weathered rock debris. When excavated, they showed a striking resemblance to forms generally accepted to be shaped by glacial/glaciofluvial erosion. In addition to these forms there were irregular cavities for instance smoothly rounded throughs and irregular rough surfaces resembling those claimed to be preglacial weathering forms. In spite of the few observations made, many small scale glacial erosion forms are likely to be the result of a three-step process i.e. glacial pressure deformation of the bedrock, subsequent weathering of the deformed rock, and finally excavation of the deformed rock by exogenic processes. Further on it seems probable that many rough surfaces of the type described in the paper are the result of glacial pressure deformation and subsequent weathering.</abstract><cop>Oxford</cop><pub>Taylor & Francis</pub><doi>10.1080/04353676.1991.11880328</doi><tpages>7</tpages></addata></record> |
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subjects | Bedrock Bgi / Prodig Deformation Earth sciences Earth, ocean, space Erosion Europe Exact sciences and technology Excavations Fysisk geografi Glacial landforms Glaciers Marine and continental quaternary Moraines Outcrops Physical Geography Rocks Scandinavian States. Finland Surficial geology Weathering processes |
title | Small Scale Glacial Erosion Forms and their Possible Relation to Post-Glacial Weathering |
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