Earth-Moon Relationships: Proceedings of the Conference held in Padova, Italy at the Accademia Galileiana di Scienze Lettere ed Arti, November 8?10, 2000
Sediments and sedimentary processes on the Moon and Earth are very different. In the absence of water, an atmosphere, the magnetosphere, and much less oxygen in its rocks, the Moon has neither clay minerals nor carbonates, and no Fe3+. Mechanical weathering by impacts is the principal process of sed...
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| Format: | Elektronisch E-Book |
| Sprache: | English |
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Dordrecht
Springer Netherlands
2001
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| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | Sediments and sedimentary processes on the Moon and Earth are very different. In the absence of water, an atmosphere, the magnetosphere, and much less oxygen in its rocks, the Moon has neither clay minerals nor carbonates, and no Fe3+. Mechanical weathering by impacts is the principal process of sediment generation on the Moon; on Earth, chemical weathering predominates. Whereas processes of sediment transport are principally ballistic on the Moon, movement by air, water and ice prevail on the Earth. The radical differences between Earth and Moon sediments make them useful end-members between which all sediments of all terrestrial planetary bodies are expected to lie. The purpose of this paper is (l) to compare and contrast major characteristics of the origin, transportation, deposition, and preservation of sediments, especially dust, in the Earth and the Moon, and (2) to suggest how sediments of other rocky planetary bodies, especially Mars, may fit in-between the sediments of the Earth and the Moon |
| Beschreibung: | 1 Online-Ressource (X, 575 p. 244 illus., 2 illus. in color) |
| ISBN: | 9789401008006 |
| DOI: | 10.1007/978-94-010-0800-6 |
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| 520 | |a Sediments and sedimentary processes on the Moon and Earth are very different. In the absence of water, an atmosphere, the magnetosphere, and much less oxygen in its rocks, the Moon has neither clay minerals nor carbonates, and no Fe3+. Mechanical weathering by impacts is the principal process of sediment generation on the Moon; on Earth, chemical weathering predominates. Whereas processes of sediment transport are principally ballistic on the Moon, movement by air, water and ice prevail on the Earth. The radical differences between Earth and Moon sediments make them useful end-members between which all sediments of all terrestrial planetary bodies are expected to lie. The purpose of this paper is (l) to compare and contrast major characteristics of the origin, transportation, deposition, and preservation of sediments, especially dust, in the Earth and the Moon, and (2) to suggest how sediments of other rocky planetary bodies, especially Mars, may fit in-between the sediments of the Earth and the Moon | ||
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| spelling | Earth-Moon Relationships Proceedings of the Conference held in Padova, Italy at the Accademia Galileiana di Scienze Lettere ed Arti, November 8?10, 2000 edited by Cesare Barbieri, Francesca Rampazzi Proceedings of the Conference held in Padova, Italy at the Accademia Galileiana di Scienze Lettere ed Arti, November 8-10, 2000 Dordrecht Springer Netherlands 2001 1 Online-Ressource (X, 575 p. 244 illus., 2 illus. in color) txt rdacontent c rdamedia cr rdacarrier Sediments and sedimentary processes on the Moon and Earth are very different. In the absence of water, an atmosphere, the magnetosphere, and much less oxygen in its rocks, the Moon has neither clay minerals nor carbonates, and no Fe3+. Mechanical weathering by impacts is the principal process of sediment generation on the Moon; on Earth, chemical weathering predominates. Whereas processes of sediment transport are principally ballistic on the Moon, movement by air, water and ice prevail on the Earth. The radical differences between Earth and Moon sediments make them useful end-members between which all sediments of all terrestrial planetary bodies are expected to lie. The purpose of this paper is (l) to compare and contrast major characteristics of the origin, transportation, deposition, and preservation of sediments, especially dust, in the Earth and the Moon, and (2) to suggest how sediments of other rocky planetary bodies, especially Mars, may fit in-between the sediments of the Earth and the Moon Earth Sciences Planetology Astronomy, Observations and Techniques Earth Sciences, general Chemistry/Food Science, general Environment, general Earth sciences Chemistry Observations, Astronomical Astronomy / Observations Environment 1\p (DE-588)1071861417 Konferenzschrift gnd-content Barbieri, Cesare edt Rampazzi, Francesca edt Erscheint auch als Druck-Ausgabe 9789401038553 https://doi.org/10.1007/978-94-010-0800-6 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | Earth-Moon Relationships Proceedings of the Conference held in Padova, Italy at the Accademia Galileiana di Scienze Lettere ed Arti, November 8?10, 2000 Earth Sciences Planetology Astronomy, Observations and Techniques Earth Sciences, general Chemistry/Food Science, general Environment, general Earth sciences Chemistry Observations, Astronomical Astronomy / Observations Environment |
| subject_GND | (DE-588)1071861417 |
| title | Earth-Moon Relationships Proceedings of the Conference held in Padova, Italy at the Accademia Galileiana di Scienze Lettere ed Arti, November 8?10, 2000 |
| title_alt | Proceedings of the Conference held in Padova, Italy at the Accademia Galileiana di Scienze Lettere ed Arti, November 8-10, 2000 |
| title_auth | Earth-Moon Relationships Proceedings of the Conference held in Padova, Italy at the Accademia Galileiana di Scienze Lettere ed Arti, November 8?10, 2000 |
| title_exact_search | Earth-Moon Relationships Proceedings of the Conference held in Padova, Italy at the Accademia Galileiana di Scienze Lettere ed Arti, November 8?10, 2000 |
| title_full | Earth-Moon Relationships Proceedings of the Conference held in Padova, Italy at the Accademia Galileiana di Scienze Lettere ed Arti, November 8?10, 2000 edited by Cesare Barbieri, Francesca Rampazzi |
| title_fullStr | Earth-Moon Relationships Proceedings of the Conference held in Padova, Italy at the Accademia Galileiana di Scienze Lettere ed Arti, November 8?10, 2000 edited by Cesare Barbieri, Francesca Rampazzi |
| title_full_unstemmed | Earth-Moon Relationships Proceedings of the Conference held in Padova, Italy at the Accademia Galileiana di Scienze Lettere ed Arti, November 8?10, 2000 edited by Cesare Barbieri, Francesca Rampazzi |
| title_short | Earth-Moon Relationships |
| title_sort | earth moon relationships proceedings of the conference held in padova italy at the accademia galileiana di scienze lettere ed arti november 8 10 2000 |
| title_sub | Proceedings of the Conference held in Padova, Italy at the Accademia Galileiana di Scienze Lettere ed Arti, November 8?10, 2000 |
| topic | Earth Sciences Planetology Astronomy, Observations and Techniques Earth Sciences, general Chemistry/Food Science, general Environment, general Earth sciences Chemistry Observations, Astronomical Astronomy / Observations Environment |
| topic_facet | Earth Sciences Planetology Astronomy, Observations and Techniques Earth Sciences, general Chemistry/Food Science, general Environment, general Earth sciences Chemistry Observations, Astronomical Astronomy / Observations Environment Konferenzschrift |
| url | https://doi.org/10.1007/978-94-010-0800-6 |
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