theoretical geomorphology von scheidegger adrian (12 Ergebnisse)

HC. 333 w12728 Ehem. Bibliotheksexemplar mit entsprechenden Merkmalen in geutem Zustand. Sprache: Englisch Gewicht in Gramm: 550.

Bibliothekseinband. Zustand: Gut. 2nd revised Edition;. 435 Seiten; Das hier angebotene Buch stammt aus einer teilaufgelösten wissenschaftlichen Bibliothek und trägt die entsprechenden Kennzeichnungen (Rückenschild, Instituts-Stempel.); leichte altersbedingte Anbräunung des Papiers; der Buchzustand ist ansonsten ordentlich und dem Alter entsprechend gut. In ENGLISCHER Sprache. Sprache: Englisch Gewicht in Gramm: 800.

Zustand: Good. 1961. No Edition Remarks. 333 pages. No dust jacket. This is an ex-Library book. Brown cloth covered boards with gilt. Black and white diagrams. Ex library copy with associated labels, inserts, stamps and annotations. Pages remain bright and clean with minimal tanning and foxing. Binding remains firm. Boards have moderate shelf wear with mild bumping and fraying to corners and crushing and fraying to spine ends. Some marks and staining to surfaces.

Zustand: Good. 1961. No Edition Remarks. 333 pages. No dust jacket. This is an ex-Library book. Brown cloth. Library copy, with expected inserts and inscriptions. Binding remains firm. Pages are lightly tanned throughout. Boards have light shelf-wear with corner bumping. Slight crushing to spine ends.

Zustand: Good. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. In good all round condition. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,950grams, ISBN:0387525106.

Hardcover. Third, completely revised ed. XIV, 434 S. Ehem. Bibliotheksexemplar mit Signatur und Stempel. GUTER Zustand, ein paar Gebrauchsspuren. Ex-library with stamp and library-signature. GOOD condition, some traces of use. w11025 3540525106 Sprache: Englisch Gewicht in Gramm: 550.

Gr.-8°, Originalkarton (Hardcover) , 434 S., ISBN 3540525106 LIEFERUNG als Briefsendung (Deutsche Post) oder Paket (DHL) , handschriftliche Nummer aut Titelblatt, papierbedingt leicht gebräunt, sonst gutes Exemplar.

Zustand: New. In.

Zustand: Good. Some shelfwear. Marks to the cover on both sides. Corners slightly worn in places. Inscriptions at the front of the book. Sticker to inside cover. Content seems ok.

Hardcover. Zustand: Very Good. Zustand des Schutzumschlags: Very Good. First Edition. Pages clean and bright, no markings, light wear to edges. Dust Jacket unclipped. ALL ITEMS ARE DISPATCHED FROM THE UK WITHIN 48 HOURS ( BOOKS ORDERED OVER THE WEEKEND DISPATCHED ON MONDAY) ALL OVERSEAS ORDERS SENT BY TRACKABLE AIR MAIL. IF YOU ARE LOCATED OUTSIDE THE UK PLEASE ASK US FOR A POSTAGE QUOTE FOR MULTI VOLUME SETS BEFORE ORDERING.

Paperback. Zustand: Brand New. 3rd edition. 448 pages. 9.40x6.80x1.10 inches. In Stock.

Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - The surface features of the Earth are commonly split into two categories, the first of which comprises those features that are due to processes occurring inside the solid Earth (endogenic features) and the second those that are due to processes occurring outside the solid Earth (exogenic features). Specifically, the endogenic features are treated in the science of geodynamics, the exogenic features in the science of geomorphology. I have treated the theoretical aspects of the endogenic features in my Principles of Geodynamics, and it is my aim to supplement my earlier book with a discussion of the theory of the exogenic features, the taxonomy of the latter having been discussed in my Systematic Geomorphology. It is my hope that the three books will together pre sent a reasonably coherent, if necessarily incomplete, account of theoretical geology. Contrary to endogenic phenomena, exogenic processes can often be directly observed as they occur: the action of a river, the develop ment of a slope, and the evolution of a shore platform are all suffi ciently rapid so that they can be seen as they take place. This has the result that in geomorphology one is generally on much less specula tive ground regarding the mechanics of the processes at work than one is in geodynamics.