Mountains: the origins of the Earth's mountain systems
Most mountains on Earth occur within relatively well-defined, narrow belts separated by wide expanses of much lower-lying ground. Their distribution is not random but is caused by the now well-understood geological processes of plate tectonics. Some mountains mark the site of a former plate collisio...
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| Main Author: | |
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| Format: | Book |
| Language: | English |
| Published: |
Edinburgh ; London
Dunedin
[2018]
|
| Subjects: | |
| Summary: | Most mountains on Earth occur within relatively well-defined, narrow belts separated by wide expanses of much lower-lying ground. Their distribution is not random but is caused by the now well-understood geological processes of plate tectonics. Some mountains mark the site of a former plate collision – where one continental plate has ridden up over another, resulting in a zone of highly deformed and elevated rocks. Others are essentially volcanic in origin. The most obvious mountain belts today – the Himalayas, the Alps and the Andes, for example – are situated at currently active plate boundaries. Others, such as the Caledonian mountains of the British Isles and Scandinavia, are the product of a plate collision that happened far in the geological past and have no present relationship to a plate boundary. These are much lower, with a generally gentler relief, worn down through millennia of erosion. |
| Item Description: | Literaturverzeichnis: Seite 195-197 |
| Physical Description: | xi, 212 Seiten Illustrationen, Diagramme, Karten |
| ISBN: | 9781780460666 9781780465807 |
Staff View
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| 520 | 3 | |a Most mountains on Earth occur within relatively well-defined, narrow belts separated by wide expanses of much lower-lying ground. Their distribution is not random but is caused by the now well-understood geological processes of plate tectonics. Some mountains mark the site of a former plate collision – where one continental plate has ridden up over another, resulting in a zone of highly deformed and elevated rocks. Others are essentially volcanic in origin. The most obvious mountain belts today – the Himalayas, the Alps and the Andes, for example – are situated at currently active plate boundaries. Others, such as the Caledonian mountains of the British Isles and Scandinavia, are the product of a plate collision that happened far in the geological past and have no present relationship to a plate boundary. These are much lower, with a generally gentler relief, worn down through millennia of erosion. | |
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Record in the Search Index
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| any_adam_object | |
| author | Park, Graham |
| author_GND | (DE-588)141929413 |
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| contents | The Earth's active mountain systems are explained, describing how plate tectonic processes have shaped them. It then looks more briefly at some of the older mountain systems whose tectonic origins are more obscure. It will inform both amateur and professional geologists |
| ctrlnum | (OCoLC)1083278209 (DE-599)OBVAC13766151 |
| discipline | Geographie |
| format | Book |
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| id | DE-604.BV045415408 |
| illustrated | Illustrated |
| indexdate | 2024-07-10T08:17:31Z |
| institution | BVB |
| isbn | 9781780460666 9781780465807 |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030801390 |
| oclc_num | 1083278209 |
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| owner | DE-384 DE-29 |
| owner_facet | DE-384 DE-29 |
| physical | xi, 212 Seiten Illustrationen, Diagramme, Karten |
| publishDate | 2018 |
| publishDateSearch | 2018 |
| publishDateSort | 2018 |
| publisher | Dunedin |
| record_format | marc |
| spelling | Park, Graham Verfasser (DE-588)141929413 aut Mountains the origins of the Earth's mountain systems Graham Park Edinburgh ; London Dunedin [2018] xi, 212 Seiten Illustrationen, Diagramme, Karten txt rdacontent n rdamedia nc rdacarrier Literaturverzeichnis: Seite 195-197 The Earth's active mountain systems are explained, describing how plate tectonic processes have shaped them. It then looks more briefly at some of the older mountain systems whose tectonic origins are more obscure. It will inform both amateur and professional geologists Most mountains on Earth occur within relatively well-defined, narrow belts separated by wide expanses of much lower-lying ground. Their distribution is not random but is caused by the now well-understood geological processes of plate tectonics. Some mountains mark the site of a former plate collision – where one continental plate has ridden up over another, resulting in a zone of highly deformed and elevated rocks. Others are essentially volcanic in origin. The most obvious mountain belts today – the Himalayas, the Alps and the Andes, for example – are situated at currently active plate boundaries. Others, such as the Caledonian mountains of the British Isles and Scandinavia, are the product of a plate collision that happened far in the geological past and have no present relationship to a plate boundary. These are much lower, with a generally gentler relief, worn down through millennia of erosion. Inselbogen (DE-588)4338258-7 gnd rswk-swf Känozoikum (DE-588)4075273-2 gnd rswk-swf Orogen (DE-588)4172848-8 gnd rswk-swf Historische Geologie (DE-588)4025104-4 gnd rswk-swf Gebirge (DE-588)4019535-1 gnd rswk-swf Paläotektonik (DE-588)4173119-0 gnd rswk-swf Tektonik (DE-588)4059351-4 gnd rswk-swf Geologie (DE-588)4020227-6 gnd rswk-swf Faltengebirge (DE-588)4153639-3 gnd rswk-swf Mesozoikum (DE-588)4038793-8 gnd rswk-swf Neotektonik (DE-588)4138986-4 gnd rswk-swf Orogenese (DE-588)4172850-6 gnd rswk-swf Paläozoikum (DE-588)4130860-8 gnd rswk-swf Falten- und Überschiebungsgürtel (DE-588)4695349-8 gnd rswk-swf Orogen (DE-588)4172848-8 s Falten- und Überschiebungsgürtel (DE-588)4695349-8 s Faltengebirge (DE-588)4153639-3 s Geologie (DE-588)4020227-6 s DE-604 Gebirge (DE-588)4019535-1 s Historische Geologie (DE-588)4025104-4 s Känozoikum (DE-588)4075273-2 s Mesozoikum (DE-588)4038793-8 s Paläozoikum (DE-588)4130860-8 s Tektonik (DE-588)4059351-4 s Neotektonik (DE-588)4138986-4 s Orogenese (DE-588)4172850-6 s Paläotektonik (DE-588)4173119-0 s Inselbogen (DE-588)4338258-7 s Erscheint auch als Online-Ausgabe, EPUB 978-1-78046-579-1 |
| spellingShingle | Park, Graham Mountains the origins of the Earth's mountain systems The Earth's active mountain systems are explained, describing how plate tectonic processes have shaped them. It then looks more briefly at some of the older mountain systems whose tectonic origins are more obscure. It will inform both amateur and professional geologists Inselbogen (DE-588)4338258-7 gnd Känozoikum (DE-588)4075273-2 gnd Orogen (DE-588)4172848-8 gnd Historische Geologie (DE-588)4025104-4 gnd Gebirge (DE-588)4019535-1 gnd Paläotektonik (DE-588)4173119-0 gnd Tektonik (DE-588)4059351-4 gnd Geologie (DE-588)4020227-6 gnd Faltengebirge (DE-588)4153639-3 gnd Mesozoikum (DE-588)4038793-8 gnd Neotektonik (DE-588)4138986-4 gnd Orogenese (DE-588)4172850-6 gnd Paläozoikum (DE-588)4130860-8 gnd Falten- und Überschiebungsgürtel (DE-588)4695349-8 gnd |
| subject_GND | (DE-588)4338258-7 (DE-588)4075273-2 (DE-588)4172848-8 (DE-588)4025104-4 (DE-588)4019535-1 (DE-588)4173119-0 (DE-588)4059351-4 (DE-588)4020227-6 (DE-588)4153639-3 (DE-588)4038793-8 (DE-588)4138986-4 (DE-588)4172850-6 (DE-588)4130860-8 (DE-588)4695349-8 |
| title | Mountains the origins of the Earth's mountain systems |
| title_auth | Mountains the origins of the Earth's mountain systems |
| title_exact_search | Mountains the origins of the Earth's mountain systems |
| title_full | Mountains the origins of the Earth's mountain systems Graham Park |
| title_fullStr | Mountains the origins of the Earth's mountain systems Graham Park |
| title_full_unstemmed | Mountains the origins of the Earth's mountain systems Graham Park |
| title_short | Mountains |
| title_sort | mountains the origins of the earth s mountain systems |
| title_sub | the origins of the Earth's mountain systems |
| topic | Inselbogen (DE-588)4338258-7 gnd Känozoikum (DE-588)4075273-2 gnd Orogen (DE-588)4172848-8 gnd Historische Geologie (DE-588)4025104-4 gnd Gebirge (DE-588)4019535-1 gnd Paläotektonik (DE-588)4173119-0 gnd Tektonik (DE-588)4059351-4 gnd Geologie (DE-588)4020227-6 gnd Faltengebirge (DE-588)4153639-3 gnd Mesozoikum (DE-588)4038793-8 gnd Neotektonik (DE-588)4138986-4 gnd Orogenese (DE-588)4172850-6 gnd Paläozoikum (DE-588)4130860-8 gnd Falten- und Überschiebungsgürtel (DE-588)4695349-8 gnd |
| topic_facet | Inselbogen Känozoikum Orogen Historische Geologie Gebirge Paläotektonik Tektonik Geologie Faltengebirge Mesozoikum Neotektonik Orogenese Paläozoikum Falten- und Überschiebungsgürtel |
| work_keys_str_mv | AT parkgraham mountainstheoriginsoftheearthsmountainsystems |