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Book Surficial Geology  Tanquary Fiord  Nunavut  NTS 340 D

Download or read book Surficial Geology Tanquary Fiord Nunavut NTS 340 D written by and published by . This book was released on 2015 with total page 7 pages. Available in PDF, EPUB and Kindle. Book excerpt: The Quttinirpaaq National Park region is mountainous including the highest peak in eastern North America. Glaciers cover about half of the map area, including unique floating ice shelves along the north coast, which have largely broken up in the last few decades but many fiord and valley glaciers still contact the sea. Sedimentary rock outcrops form the dominant surficial unit, including large areas of frost shattered rubble mantling broad summits and slopes. Glacial debris is also widespread normally forming a thin discontinuous veneer of till or as isolated erratic boulders. In the past, as now, the main source of run-off and sediment is supplied by glacial meltwater. Consequently most of the unconsolidated sediment lies within formerly glaciated valleys and coastlines where there are complex associations of moraines, glaciofluvial and glaciomarine deposits related to the advance and retreat of valley glaciers and ice caps, coupled with falling sea levels caused by postglacial crustal uplift.

Book Surficial Geology  Tanquary Fiord  Nunavut  NTS 340 D

Download or read book Surficial Geology Tanquary Fiord Nunavut NTS 340 D written by and published by . This book was released on 2015 with total page 7 pages. Available in PDF, EPUB and Kindle. Book excerpt: The Quttinirpaaq National Park region is mountainous including the highest peak in eastern North America. Glaciers cover about half of the map area, including unique floating ice shelves along the north coast, which have largely broken up in the last few decades but many fiord and valley glaciers still contact the sea. Sedimentary rock outcrops form the dominant surficial unit, including large areas of frost shattered rubble mantling broad summits and slopes. Glacial debris is also widespread normally forming a thin discontinuous veneer of till or as isolated erratic boulders. In the past, as now, the main source of run-off and sediment is supplied by glacial meltwater. Consequently most of the unconsolidated sediment lies within formerly glaciated valleys and coastlines where there are complex associations of moraines, glaciofluvial and glaciomarine deposits related to the advance and retreat of valley glaciers and ice caps, coupled with falling sea levels caused by postglacial crustal uplift.

Book Surficial Geology  M Clintock Inlet Area  Nunavut  NTS 340 E and Part of NTS 340 H

Download or read book Surficial Geology M Clintock Inlet Area Nunavut NTS 340 E and Part of NTS 340 H written by and published by . This book was released on 2015 with total page 7 pages. Available in PDF, EPUB and Kindle. Book excerpt: The Quttinirpaaq National Park region is mountainous including the highest peak in eastern North America. Glaciers cover about half of the map area, including unique floating ice shelves along the north coast, which have largely broken up in the last few decades but many fiord and valley glaciers still contact the sea. Sedimentary rock outcrops form the dominant surficial unit, including large areas of frost shattered rubble mantling broad summits and slopes. Glacial debris is also widespread normally forming a thin discontinuous veneer of till or as isolated erratic boulders. In the past, as now, the main source of run-off and sediment is supplied by glacial meltwater. Consequently most of the unconsolidated sediment lies within formerly glaciated valleys andcoastlines where there are complex associations of moraines, glaciofluvial and glaciomarine deposits related to the advance and retreat of valley glaciers and ice caps, coupled with falling sea levels caused by postglacial crustal uplift.

Book Surficial Geology  M Clintock Inlet Area  Nunavut  NTS 340 E and Part of 340 H

Download or read book Surficial Geology M Clintock Inlet Area Nunavut NTS 340 E and Part of 340 H written by Jan M. Bednarski and published by . This book was released on 2016 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt: "The Quttinirpaaq National Park region is mountainous including the highest peak in eastern North America. Glaciers cover about half of the map area, including unique floating ice shelves along the north coast, which have largely broken up in the last few decades but many fiord and valley glaciers still contact the sea. Sedimentary rock outcrops form the dominant surficial unit, including large areas of frost shattered rubble mantling broad summits and slopes. Glacial debris is also widespread normally forming a thin discontinuous veneer of till or as isolated erratic boulders. In the past, as now, the main source of run-off and sediment is supplied by glacial meltwater. Consequently most of the unconsolidated sediment lies within formerly glaciated valleys and coastlines where there are complex associations of moraines, glaciofluvial and glaciomarine deposits related to the advance and retreat of valley glaciers and ice caps, coupled with falling sea levels caused by postglacial crustal uplift"--Page [2].

Book Reconnaissance surficial geology  Yellow Bluff  west   Nunavut  NTS 46 D west

Download or read book Reconnaissance surficial geology Yellow Bluff west Nunavut NTS 46 D west written by and published by . This book was released on 2013 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Surficial Geology  Somerset Island  Nunavut  NTS 58 B  NTS 58 C  and Parts of NTS 58 A  NTS 58 D  NTS 58 E  NTS 58 F

Download or read book Surficial Geology Somerset Island Nunavut NTS 58 B NTS 58 C and Parts of NTS 58 A NTS 58 D NTS 58 E NTS 58 F written by Geological Survey of Canada and published by . This book was released on 2015 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt: This new surficial geology map product represents the conversion of Map 1555A and its legend, using the Geological Survey of Canada's Surficial Data Model (SDM version 2.1) which can be found in Open File 7741. All geoscience knowledge and information from Map 1555A that conformed to the current SDM were maintained during the conversion process. The purpose of converting legacy map data to a common science language and common legend is to enable and facilitate the efficient digital compilation, interpretation, management and dissemination of geologic map information in a structured and consistent manner. This provides an effective knowledge management tool designed around a geo-database which can expand following the type of information to appear on new surficial geology maps.

Book Surficial geology  Montresor River  Nunavut  NTS 66 I

Download or read book Surficial geology Montresor River Nunavut NTS 66 I written by Geological Survey of Canada and published by . This book was released on 2017 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Surficial Geology  Eastern Devon Island  Nunavut  NTS 48 E   38 F and 48 H   38 G

Download or read book Surficial Geology Eastern Devon Island Nunavut NTS 48 E 38 F and 48 H 38 G written by Geological Survey of Canada and published by . This book was released on 2018 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Surficial Geology  Wollaston Peninsula  Victoria Island  Nunavut Northwest Territories  NTS 87 D  Parts of 87 A  B  C  E  and F

Download or read book Surficial Geology Wollaston Peninsula Victoria Island Nunavut Northwest Territories NTS 87 D Parts of 87 A B C E and F written by Geological Survey of Canada and published by . This book was released on 2017 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Surficial Geology  Somerset Island  Nunavut  NTS 58 B  C  Parts of 58 A  D  E  F

Download or read book Surficial Geology Somerset Island Nunavut NTS 58 B C Parts of 58 A D E F written by and published by . This book was released on 2016 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt: "This new surficial geology map product represents the conversion of Map 1555A and its legend, using the Geological Survey of Canada's Surficial Data Model (SDM version 2.1) which can be found in Open File 7741. All geoscience knowledgeand information from Map 1555A that conformed to the current SDM were maintained during the conversion process. The purpose of converting legacy map data to a common science language and common legend is to enable and facilitate the efficient digital compilation, interpretation, management and dissemination of geologic map information in a structured and consistent manner. This provides an effective knowledge management tool designed around a geo-database which can expand following the type of information to appear on new surficial geology maps"--Page [2].

Book Surficial Geology  Agu Bay and Easter Cape  Nunavut  NTS 47 F and Parts of 57 E

Download or read book Surficial Geology Agu Bay and Easter Cape Nunavut NTS 47 F and Parts of 57 E written by Geological Survey of Canada and published by . This book was released on 2018 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Surficial Geology  Central Devon Island  Nunavut  NTS 48 F and G

Download or read book Surficial Geology Central Devon Island Nunavut NTS 48 F and G written by Geological Survey of Canada and published by . This book was released on 2018 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Surficial Geology  Lady Franklin Bay Area  Nunavut  NTS 120 C and Part of NTS 120 D

Download or read book Surficial Geology Lady Franklin Bay Area Nunavut NTS 120 C and Part of NTS 120 D written by and published by . This book was released on 2015 with total page 6 pages. Available in PDF, EPUB and Kindle. Book excerpt: ABSTRACT BSTRACTThe Quttinirpaaq National Park region is mountainous including the highest peak in eastern North America. Glaciers cover about half of the map area, including unique floating ice shelves along the north coast, which have largely broken up in the last few decades but many fiord and valley glaciers still contact the sea. Sedimentary rock outcrops form the dominant surficial unit, including large areas of frost shattered rubble mantling broad summits and slopes. Glacial debris is also widespread normally forming a thin discontinuous veneer of till or as isolated erratic boulders. In the past, as now, the main source of run-off and sediment is supplied by glacial meltwater. Consequently most of the unconsolidated sediment lies within formerly glaciated valleys and coastlines where there are complex associations of moraines, glaciofluvial andglaciomarine deposits related to the advance and retreat of valley glaciers and ice caps, coupled with falling sea levels caused by postglacial crustal uplift.

Book Surficial geology  Hepburn Island  Nunavut  NTS 76 M

Download or read book Surficial geology Hepburn Island Nunavut NTS 76 M written by Geological Survey of Canada and published by . This book was released on 2017 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt:

Book Surficial Geology  Storkerson Peninsula  Victoria Island  and Stefansson Island  Nunavut  NTS 78 A  D  and Parts of 78 B  C

Download or read book Surficial Geology Storkerson Peninsula Victoria Island and Stefansson Island Nunavut NTS 78 A D and Parts of 78 B C written by Geological Survey of Canada and published by . This book was released on 2016 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt: