Image for Earth-Moon Relationships

Earth-Moon Relationships : Proceedings of the Conference held in Padova, Italy at the Accademia Galileiana di Scienze Lettere ed Arti, November 8–10, 2000 (Softcover reprint of the original 1st ed. 2001)

Barbieri, Cesare(Edited by)Rampazzi, Francesca(Edited by)
See all formats and editions

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.

Read More
Special order line: only available to educational & business accounts. Sign In
£179.99
Product Details
Springer
9401038554 / 9789401038553
Paperback / softback
523.3
20/11/2013
Netherlands
575 pages, 2 Illustrations, color; 242 Illustrations, black and white; X, 575 p. 244 illus., 2 illus
160 x 240 mm