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Geomorphology of the Courel Mountains Unesco Global Geopark (Galicia, NW Iberian Peninsula)
The Courel Mountains Geopark is in Galicia, Northwest Spain. Its total area is 578.29 km 2 . Parallel valleys and ridges characterize its relief from North to South. Their maximum altitude reaches 1,641 m. Their lithology is dominated by slates, quartzites, and limestones, together with small diabas...
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description | The Courel Mountains Geopark is in Galicia, Northwest Spain. Its total area is 578.29 km
2
. Parallel valleys and ridges characterize its relief from North to South. Their maximum altitude reaches 1,641 m. Their lithology is dominated by slates, quartzites, and limestones, together with small diabase outcrops. Materials are intensely fractured due to the tectonic dynamics that started during the Cenozoic, and sedimentary formations accumulated in response to environmental changes during the Pleistocene are abundant. As a result, a wide variety of structural landforms are present, along with a wide range of landforms and deposits of alluvial, fluvial, glacial, and periglacial origin. All of them have been mapped to enable sustainable use and management aimed at improving the livelihood of the inhabitants of the geopark area, which has suffered depopulation in recent decades.
Courel Mountains Unesco Global Geopark stands out for its geological and geomorphological diversity.
This sector shows evidence of different structural geoforms (alluvial, fluvial, glacier, and periglacial origin).
Geomorphological cartography graphically draws the most outstanding deposits and geoforms. |
doi_str_mv | 10.1080/17445647.2023.2257714 |
format | article |
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2
. Parallel valleys and ridges characterize its relief from North to South. Their maximum altitude reaches 1,641 m. Their lithology is dominated by slates, quartzites, and limestones, together with small diabase outcrops. Materials are intensely fractured due to the tectonic dynamics that started during the Cenozoic, and sedimentary formations accumulated in response to environmental changes during the Pleistocene are abundant. As a result, a wide variety of structural landforms are present, along with a wide range of landforms and deposits of alluvial, fluvial, glacial, and periglacial origin. All of them have been mapped to enable sustainable use and management aimed at improving the livelihood of the inhabitants of the geopark area, which has suffered depopulation in recent decades.
Courel Mountains Unesco Global Geopark stands out for its geological and geomorphological diversity.
This sector shows evidence of different structural geoforms (alluvial, fluvial, glacier, and periglacial origin).
Geomorphological cartography graphically draws the most outstanding deposits and geoforms.</description><identifier>ISSN: 1744-5647</identifier><identifier>EISSN: 1744-5647</identifier><identifier>DOI: 10.1080/17445647.2023.2257714</identifier><language>eng</language><publisher>Abingdon: Taylor & Francis</publisher><subject>Alluvial deposits ; Cenozoic ; Courel Mountains ; Environmental changes ; Galicia ; Geology ; Geomorphology ; Geopark ; Iberian Peninsula ; Landforms ; Lithology ; Mountains ; Outcrops ; Pleistocene ; Quartzite ; River networks ; Rural development ; Sediment deposits ; Slates ; Sustainable use ; Tectonics</subject><ispartof>Journal of maps, 2023-12, Vol.19 (1)</ispartof><rights>2023 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps 2023</rights><rights>2023 The Author(s). Published by Informa UK Limited, trading as Taylor & Francis Group on behalf of Journal of Maps. This work is licensed under the Creative Commons Attribution – Non-Commercial License http://creativecommons.org/licenses/by-nc/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c399t-3ce4ce8fad3032901d0dc9b7270ac7f10989fbb7d121fa8d88c8f3caa47bafbf3</cites><orcidid>0000-0002-7974-3207 ; 0000-0001-7428-4622</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.tandfonline.com/doi/pdf/10.1080/17445647.2023.2257714$$EPDF$$P50$$Ginformaworld$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.tandfonline.com/doi/full/10.1080/17445647.2023.2257714$$EHTML$$P50$$Ginformaworld$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,27479,27901,27902,59116,59117</link.rule.ids></links><search><creatorcontrib>Pérez-Alberti, Augusto</creatorcontrib><creatorcontrib>Gómez-Pazo, Alejandro</creatorcontrib><title>Geomorphology of the Courel Mountains Unesco Global Geopark (Galicia, NW Iberian Peninsula)</title><title>Journal of maps</title><description>The Courel Mountains Geopark is in Galicia, Northwest Spain. Its total area is 578.29 km
2
. Parallel valleys and ridges characterize its relief from North to South. Their maximum altitude reaches 1,641 m. Their lithology is dominated by slates, quartzites, and limestones, together with small diabase outcrops. Materials are intensely fractured due to the tectonic dynamics that started during the Cenozoic, and sedimentary formations accumulated in response to environmental changes during the Pleistocene are abundant. As a result, a wide variety of structural landforms are present, along with a wide range of landforms and deposits of alluvial, fluvial, glacial, and periglacial origin. All of them have been mapped to enable sustainable use and management aimed at improving the livelihood of the inhabitants of the geopark area, which has suffered depopulation in recent decades.
Courel Mountains Unesco Global Geopark stands out for its geological and geomorphological diversity.
This sector shows evidence of different structural geoforms (alluvial, fluvial, glacier, and periglacial origin).
Geomorphological cartography graphically draws the most outstanding deposits and geoforms.</description><subject>Alluvial deposits</subject><subject>Cenozoic</subject><subject>Courel Mountains</subject><subject>Environmental changes</subject><subject>Galicia</subject><subject>Geology</subject><subject>Geomorphology</subject><subject>Geopark</subject><subject>Iberian Peninsula</subject><subject>Landforms</subject><subject>Lithology</subject><subject>Mountains</subject><subject>Outcrops</subject><subject>Pleistocene</subject><subject>Quartzite</subject><subject>River networks</subject><subject>Rural development</subject><subject>Sediment deposits</subject><subject>Slates</subject><subject>Sustainable use</subject><subject>Tectonics</subject><issn>1744-5647</issn><issn>1744-5647</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>0YH</sourceid><sourceid>DOA</sourceid><recordid>eNp9UUuPEzEMHiGQWBZ-AlIkLiDR4jxmkrmBKiiVlseBFQcOkZNJdlPScclMhfrvSemCOHGyZX8Py1_TPOWw5GDgFddKtZ3SSwFCLoVotebqXnNxmi9Oi_v_9A-bR9O0BWgNmPai-bYOtKOyv6VMN0dGkc23ga3oUEJmH-gwzpjGiV2PYfLE1pkcZlY5eyzf2fM15uQTvmQfv7KNCyXhyD6HsTIOGV88bh5EzFN4clcvm-t3b7-s3i-uPq03qzdXCy_7fl5IH5QPJuIgQYoe-ACD750WGtDryKE3fXROD1zwiGYwxpsoPaLSDqOL8rLZnHUHwq3dl7TDcrSEyf4eULmxWObkc7BeqLYNpnMQnFIAhse-i5IrV31k8FXr2VlrX-jHIUyz3dZfjPV8K8HoTnS9bCuqPaN8oWkqIf515WBPmdg_mdhTJvYuk8p7fealMVLZ4U8qebAzHjOVWHD0qdr8X-IXPZ6SmA</recordid><startdate>20231231</startdate><enddate>20231231</enddate><creator>Pérez-Alberti, Augusto</creator><creator>Gómez-Pazo, Alejandro</creator><general>Taylor & Francis</general><general>Taylor & Francis Ltd</general><general>Taylor & Francis Group</general><scope>0YH</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7XB</scope><scope>8FK</scope><scope>8G5</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>M2O</scope><scope>MBDVC</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>Q9U</scope><scope>SOI</scope><scope>DOA</scope><orcidid>https://orcid.org/0000-0002-7974-3207</orcidid><orcidid>https://orcid.org/0000-0001-7428-4622</orcidid></search><sort><creationdate>20231231</creationdate><title>Geomorphology of the Courel Mountains Unesco Global Geopark (Galicia, NW Iberian Peninsula)</title><author>Pérez-Alberti, Augusto ; Gómez-Pazo, Alejandro</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c399t-3ce4ce8fad3032901d0dc9b7270ac7f10989fbb7d121fa8d88c8f3caa47bafbf3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Alluvial deposits</topic><topic>Cenozoic</topic><topic>Courel Mountains</topic><topic>Environmental changes</topic><topic>Galicia</topic><topic>Geology</topic><topic>Geomorphology</topic><topic>Geopark</topic><topic>Iberian Peninsula</topic><topic>Landforms</topic><topic>Lithology</topic><topic>Mountains</topic><topic>Outcrops</topic><topic>Pleistocene</topic><topic>Quartzite</topic><topic>River networks</topic><topic>Rural development</topic><topic>Sediment deposits</topic><topic>Slates</topic><topic>Sustainable use</topic><topic>Tectonics</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Pérez-Alberti, Augusto</creatorcontrib><creatorcontrib>Gómez-Pazo, Alejandro</creatorcontrib><collection>Taylor & Francis Open Access</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central</collection><collection>ProQuest Central Essentials</collection><collection>AUTh Library subscriptions: ProQuest Central</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Proquest Research Library</collection><collection>Research Library (Corporate)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>Journal of maps</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Pérez-Alberti, Augusto</au><au>Gómez-Pazo, Alejandro</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geomorphology of the Courel Mountains Unesco Global Geopark (Galicia, NW Iberian Peninsula)</atitle><jtitle>Journal of maps</jtitle><date>2023-12-31</date><risdate>2023</risdate><volume>19</volume><issue>1</issue><issn>1744-5647</issn><eissn>1744-5647</eissn><abstract>The Courel Mountains Geopark is in Galicia, Northwest Spain. Its total area is 578.29 km
2
. Parallel valleys and ridges characterize its relief from North to South. Their maximum altitude reaches 1,641 m. Their lithology is dominated by slates, quartzites, and limestones, together with small diabase outcrops. Materials are intensely fractured due to the tectonic dynamics that started during the Cenozoic, and sedimentary formations accumulated in response to environmental changes during the Pleistocene are abundant. As a result, a wide variety of structural landforms are present, along with a wide range of landforms and deposits of alluvial, fluvial, glacial, and periglacial origin. All of them have been mapped to enable sustainable use and management aimed at improving the livelihood of the inhabitants of the geopark area, which has suffered depopulation in recent decades.
Courel Mountains Unesco Global Geopark stands out for its geological and geomorphological diversity.
This sector shows evidence of different structural geoforms (alluvial, fluvial, glacier, and periglacial origin).
Geomorphological cartography graphically draws the most outstanding deposits and geoforms.</abstract><cop>Abingdon</cop><pub>Taylor & Francis</pub><doi>10.1080/17445647.2023.2257714</doi><orcidid>https://orcid.org/0000-0002-7974-3207</orcidid><orcidid>https://orcid.org/0000-0001-7428-4622</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Alluvial deposits Cenozoic Courel Mountains Environmental changes Galicia Geology Geomorphology Geopark Iberian Peninsula Landforms Lithology Mountains Outcrops Pleistocene Quartzite River networks Rural development Sediment deposits Slates Sustainable use Tectonics |
title | Geomorphology of the Courel Mountains Unesco Global Geopark (Galicia, NW Iberian Peninsula) |
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