The Changing Global Environment:
We know a great deal about historical climate and its variations from various geo logical studies. There are two points worth remarking on. One is that the climate changes frequently and radically, but that the degree of variation and even sense of variation depends on the time scale which we are co...
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| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Dordrecht
Springer Netherlands
1975
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| Schlagworte: | |
| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | We know a great deal about historical climate and its variations from various geo logical studies. There are two points worth remarking on. One is that the climate changes frequently and radically, but that the degree of variation and even sense of variation depends on the time scale which we are considering. Secondly, that this is a most unusual geological period for the Planet Earth; we are living in a period of mountain building and glaciations, whereas during most of the last 250 million years (m.y.) there was little ice and little topography. A good view of climate change of the last hundred m.y. can be gained by looking at the paper of Kellogg. We are now in a period of extensive glaciations. The previous interval occurred 300 to 250 m.y. ago, when even the Sahara was glaciated. (Of course, it was at that time near the position of the South Pole; we know that 300 m.y. ago the continents had not broken apart and formed one land mass.) Apparently between 250 and 20 m.y. ago there was little ice on the Earth, even at Antarctica. Continental basins were flooded by shallow seas. This was the period when plant life and marine life proliferated and when most of our fossil fuels were laid down |
| Beschreibung: | 1 Online-Ressource (432 p. 13 illus) |
| ISBN: | 9789401017299 |
| DOI: | 10.1007/978-94-010-1729-9 |
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| 520 | |a We know a great deal about historical climate and its variations from various geo logical studies. There are two points worth remarking on. One is that the climate changes frequently and radically, but that the degree of variation and even sense of variation depends on the time scale which we are considering. Secondly, that this is a most unusual geological period for the Planet Earth; we are living in a period of mountain building and glaciations, whereas during most of the last 250 million years (m.y.) there was little ice and little topography. A good view of climate change of the last hundred m.y. can be gained by looking at the paper of Kellogg. We are now in a period of extensive glaciations. The previous interval occurred 300 to 250 m.y. ago, when even the Sahara was glaciated. (Of course, it was at that time near the position of the South Pole; we know that 300 m.y. ago the continents had not broken apart and formed one land mass.) Apparently between 250 and 20 m.y. ago there was little ice on the Earth, even at Antarctica. Continental basins were flooded by shallow seas. This was the period when plant life and marine life proliferated and when most of our fossil fuels were laid down | ||
| 650 | 4 | |a Earth Sciences | |
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Datensatz im Suchindex
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| dewey-full | 628 |
| dewey-hundreds | 600 - Technology (Applied sciences) |
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| dewey-tens | 620 - Engineering and allied operations |
| discipline | Physik Bauingenieurwesen Wirtschaftswissenschaften Geographie |
| doi_str_mv | 10.1007/978-94-010-1729-9 |
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| id | DE-604.BV045177148 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:46Z |
| institution | BVB |
| isbn | 9789401017299 |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030566378 |
| oclc_num | 1053800010 |
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| owner | DE-634 |
| owner_facet | DE-634 |
| physical | 1 Online-Ressource (432 p. 13 illus) |
| psigel | ZDB-2-EES ZDB-2-EES_Archiv ZDB-2-EES ZDB-2-EES_Archiv |
| publishDate | 1975 |
| publishDateSearch | 1975 |
| publishDateSort | 1975 |
| publisher | Springer Netherlands |
| record_format | marc |
| spelling | The Changing Global Environment edited by S. Fred Singer Dordrecht Springer Netherlands 1975 1 Online-Ressource (432 p. 13 illus) txt rdacontent c rdamedia cr rdacarrier We know a great deal about historical climate and its variations from various geo logical studies. There are two points worth remarking on. One is that the climate changes frequently and radically, but that the degree of variation and even sense of variation depends on the time scale which we are considering. Secondly, that this is a most unusual geological period for the Planet Earth; we are living in a period of mountain building and glaciations, whereas during most of the last 250 million years (m.y.) there was little ice and little topography. A good view of climate change of the last hundred m.y. can be gained by looking at the paper of Kellogg. We are now in a period of extensive glaciations. The previous interval occurred 300 to 250 m.y. ago, when even the Sahara was glaciated. (Of course, it was at that time near the position of the South Pole; we know that 300 m.y. ago the continents had not broken apart and formed one land mass.) Apparently between 250 and 20 m.y. ago there was little ice on the Earth, even at Antarctica. Continental basins were flooded by shallow seas. This was the period when plant life and marine life proliferated and when most of our fossil fuels were laid down Earth Sciences Environmental Science and Engineering Environment, general Atmospheric Sciences Earth sciences Atmospheric sciences Environmental sciences Environment Klima (DE-588)4031170-3 gnd rswk-swf Luftverschmutzung (DE-588)4074381-0 gnd rswk-swf Umwelt (DE-588)4061616-2 gnd rswk-swf Klima (DE-588)4031170-3 s Luftverschmutzung (DE-588)4074381-0 s 1\p DE-604 Umwelt (DE-588)4061616-2 s 2\p DE-604 Singer, Siegfried Fred 1924-2020 (DE-588)128175443 edt Erscheint auch als Druck-Ausgabe 9789027704023 https://doi.org/10.1007/978-94-010-1729-9 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 2\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | The Changing Global Environment Earth Sciences Environmental Science and Engineering Environment, general Atmospheric Sciences Earth sciences Atmospheric sciences Environmental sciences Environment Klima (DE-588)4031170-3 gnd Luftverschmutzung (DE-588)4074381-0 gnd Umwelt (DE-588)4061616-2 gnd |
| subject_GND | (DE-588)4031170-3 (DE-588)4074381-0 (DE-588)4061616-2 |
| title | The Changing Global Environment |
| title_auth | The Changing Global Environment |
| title_exact_search | The Changing Global Environment |
| title_full | The Changing Global Environment edited by S. Fred Singer |
| title_fullStr | The Changing Global Environment edited by S. Fred Singer |
| title_full_unstemmed | The Changing Global Environment edited by S. Fred Singer |
| title_short | The Changing Global Environment |
| title_sort | the changing global environment |
| topic | Earth Sciences Environmental Science and Engineering Environment, general Atmospheric Sciences Earth sciences Atmospheric sciences Environmental sciences Environment Klima (DE-588)4031170-3 gnd Luftverschmutzung (DE-588)4074381-0 gnd Umwelt (DE-588)4061616-2 gnd |
| topic_facet | Earth Sciences Environmental Science and Engineering Environment, general Atmospheric Sciences Earth sciences Atmospheric sciences Environmental sciences Environment Klima Luftverschmutzung Umwelt |
| url | https://doi.org/10.1007/978-94-010-1729-9 |
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