W k hartmann (108 Ergebnisse)

Trade Paperback. Zustand: Very Good. First Paperback Edition. Filled w/ color & black & white illustrations, introduction by Ray Bradbury. Has Small Pub Remainder Mark. Size: 4to - over 9¾" - 12" tall. Color & b/w Illustrations (illustrator). Remainder.

hardcover. Zustand: Very Good. Connecting readers with great books since 1972! Used books may not include companion materials, and may have some shelf wear or limited writing. We ship orders daily and Customer Service is our top priority.

Hardcover. Zustand: Near Fine. 1st Edition. Ix, 179 Pp. Green Cloth. First Printing, 1974. Fine. Large Format; Near Fine. Color And B/W Photographs, Charts (illustrator).

Cloth Bound. Zustand: Very Good. No Jacket. no writing written in German see picture.

Zustand: Poor. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. In poor condition, suitable as a reading copy. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,900grams, ISBN.

Paperback. Zustand: New. komplett überarbeitete.

Hardcover. Gr.-8°. 24 x 16 cm. Gelbe Originalbroschur in einfachem Pappumschlag mit schwarzem Leinenrücken. Ausgeschiedenes Exemplar der Landwirtschaftlichen Hochschule Berlin, Institut für Obstbau und mit deren Stempeln und Signaturen. Gut erhaltenes, vollständiges Heft mit den Seiten 337-503 und 7 Textabb. u. 9 Taf. -- Bitte Portokosten außerhalb EU erfragen! / Please ask for postage costs outside EU! / S ' il vous plait demander des frais de port en dehors de l ' UE! // Bitte beachten Sie auch unsere Fotos! / Please also note our photos! / Veuillez noter nos photos -- Wenn es draußen stürmt, können Sie es sich mit einem guten Buch gemütlich machen und ein warmes Getränk dazu genießen. Bei uns finden Sie die passende Lektüre! -- Wir kaufen Ihre werthaltigen Bücher! K06700-307729.…

Soft cover. Zustand: VG-Fine. 1st ed. (1)+288, num.ills & b/w plates; an excellent, clean, unmarked copy in clean virtually unworn printed card cover.

HRD. Zustand: New. New Book. Shipped from UK. Established seller since 2000.

Zustand: Good. This is an ex-library book and may have the usual library/used-book markings inside.This book has hardback covers. Clean from markings. In good all round condition. No dust jacket. Please note the Image in this listing is a stock photo and may not match the covers of the actual item,1300grams, ISBN:9780534546304.…

Hardcover. Zustand: Brand New. 93 pages. German language. 6.02x0.39x8.27 inches. In Stock.

Orig.-Leinen. 110 S. mit zahlr. Abb. Einb. etw. lichtverf. - sehr gutes Exemplar. Sprache: Deutsch.

Hardback. Zustand: New.

Buch. Zustand: Neu. Neuware -Die vorliegende Anleitung dient der Beschreibung von Bodenhorizonten und -profilen sowie der bodenkundlichen und sensorischen Ansprache von Bodenproben in einem Umgang, wie er für den vorsorgenden und nachsorgenden Bodenschutz gemäß BBodSchV in der Fassung vom 9. Juli 2021 erforderlich ist. Diese 2. Auflage der Arbeitshilfe soll die Anforderungen der 6. Auflage der Bodenkundlichen Kartieranleitung (KA6) mit jenen des vor- und nachsorgenden Bodenschutzes zusammenführen und als eine Grundlage für den Vollzug des Bodenschutzrechts dienen. Die Modernisierung der bodenkundlichen Feldaufnahme und Datenverarbeitung, wie sie insbesondere auch durch das Geologiedatengesetz (GeolDG) vorangetrieben wurde, und die Verrechtlichung der Bodenkundlichen Baugegleitung in der BBodSchV machen deutlich, dass die Feldaufnahme auch für den Vollzug des Bodenschutzes standardisiert werden sollte. 93 pp. Deutsch.…

Hardcover. Zustand: Gut bis sehr gut. 1. Auflage. vignette auf vorblatt, gut, eher sehr gut, nur geringe lagerspuren, 498 seiten LAGER A-893.

Hardcover. Zustand: Gut. ix, 491 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. w04759 9780792370512 Sprache: Englisch Gewicht in Gramm: 1100.

During 1977 RV ?Valdivia? recovered 46 cores, occupied two hydrographic stations, and ran eleven bathymetric profiles in the roughly rectangular Sulu Sea, which trends northeast and covers about 250,000 km2. The Sulu Sea Deep in the southeast is separated from the shallower Palawan Depression in the northwest by the northeast-trending Cagayan Ridge. The maximum sill depth between the sea and the open ocean is about 400 m, and the water column is layered, cutting off the deep water, which is homogeneous, warm (10? C), and oxygen deficient (< 1.6 ml/ml O2), from normal oceanic water. The shelves are generally broad and covered with calcareous sand and gravel, except in the east and southeast, where they are narrow and covered with muddy sand and gravel. The shelf carbonates give way to bathyal oozes, and the muddy sands grade into varied silts dominated by volcanic and sedimentary debris. The smooth abyssal plain of the Sulu Sea Deep is at a depth of 4800?5000 m, and northwest of it is an plain at 4000?4200 m. Turbidites characterize both plains. The aragonite and calcite compensation depths are at about 1400 m and 4500 m, respectively. The turbidite beds average 5?10 cm thick, with all Bouma s divisions recognizable, apart from ?a? The southern turbidites (station 14224) are of two types: calcareous and terrigenous. The calcareous turbidites, characterized by shell debris including shallow-water foraminifera, were derived from the upper slopes flanking the broad shelves. The terrigenous turbidites, characterized by sedimentary and volcanic rock fragments, apparently originated from the slopes off Mindanao. The eastern turbidites (station 14233) are finer grained, characterized by sedimentary rock fragments, and came from the narrow muddy shelves further east, off Panay, Negros and Mindanao. Radiocarbon dating suggests that depositional rates for the turbidite sequences (ca. 100 cm/1000 yr.) are an order of magnitude greater than the rates for bathyal oozes. Organic carbon contents in the surface sediments are highest between 500 m and 1200 m water depth, exceeding 2% off Mindanao (station 14226), and reaching 1.82% on the Palawan slope (station 14206). The lowest contents are at the Palawan Shelf edge (0.11% at station 14204) where the proportion of carbonate sand is very high, and in the bathyal oozes of the central Sulu Sea (< 1%) where sedimentation rates are low and mineralisation of organic matter is effective. Contents average 1% below 4500 m in the Sulu Sea Deep. The colour of the surface sediment appears to be related to the organic carbon content: olive colours above 1200 m and below 4500 m, and brown colours between. The surficial sediments are characterized by living shelly faunas and intense bioturbation above 150 m, and by intense bioturbation and absence of a shelly fauna down to 3000 m. Bioturbation decreases below 3000 m, and in the Sulu Sea Deep is confined to a few Zoophycos, Granulites and Cosmorhaphe burrows. The faunal changes are apparently related to bottom water oxygen concentrations. 31 pp., 12 figs, 2 tabs, gr. 8.…

Zustand: Brand New. German language. 5.91x1.18x8.66 inches. In Stock.

Zustand: very_good. Gently read. May have name of previous ownership, or ex-library edition. Binding tight; spine straight and smooth, with no creasing; covers clean and crisp. Minimal signs of handling or shelving. 100% GUARANTEE! Shipped with delivery confirmation, if you're not satisfied with purchase please return item! Ships USPS Media Mail.…

Ärzteverein, Hannover, 1979. 195 S. mit zahlr. Abb., Pbd.--- 750 Gramm.

Eine Festschrift der hannoverschen Bezirksstelle der Ärztekammer Niedersachsen. Der Ärzteverein, Hannover, 1979. 196 S. mit zahlr. Abb. und Tafelbildern, Pbd.--- 500 Gramm.

Hardcover. Zustand: Very Good. No Jacket. Hardback copy, no dustjacket as issued. 498pp. Colour and b/w charts and graphs throughout. Not library copy, no inscriptions. (45/4).

Buch. Zustand: Neu. Neuware - Die vorliegende Anleitung dient der Beschreibung von Bodenhorizonten und -profilen sowie der bodenkundlichen und sensorischen Ansprache von Bodenproben in einem Umgang, wie er für den vorsorgenden und nachsorgenden Bodenschutz gemäß BBodSchV in der Fassung vom 9. Juli 2021 erforderlich ist. Diese 2. Auflage der Arbeitshilfe soll die Anforderungen der 6. Auflage der Bodenkundlichen Kartieranleitung (KA6) mit jenen des vor- und nachsorgenden Bodenschutzes zusammenführen und als eine Grundlage für den Vollzug des Bodenschutzrechts dienen. Die Modernisierung der bodenkundlichen Feldaufnahme und Datenverarbeitung, wie sie insbesondere auch durch das Geologiedatengesetz (GeolDG) vorangetrieben wurde, und die Verrechtlichung der Bodenkundlichen Baugegleitung in der BBodSchV machen deutlich, dass die Feldaufnahme auch für den Vollzug des Bodenschutzes standardisiert werden sollte.…

Gebunden. Zustand: New.

Zustand: New.

Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Mars is about one-eighth the mass of the Earth and it may provide an analogue of what the Earth was like when it was at such an early stage of accretion. The fur ther growth of the Earth was sustained by major collisions with planetesimals and planets such as that which resulted in the formation ofthe Earth's moon (Hartmann and Davis, 1975; Cameron and Ward, 1976; Wetherill, 1986; Cameron and Benz, 1991). This late accretionary history, which lasted more than 50 Myr in the case of the Earth (Halliday, 2000a, b), appears to have been shorter and less catastrophic in the case of Mars (Harper et ai. , 1995; Lee and Halliday, 1997). In this article we review the basic differences between the bulk composition of Mars and the Earth and the manner in which this plays into our understanding of the timing and mechanisms of accretion and core formation. We highlight some of the evidence for early cessation of major collisional growth on Mars. Finally, we reevaluate the isotopic evidence that Mars differentiated quickly. Fundamental differences between the composition of Mars and that of other terrestrial planets are apparent from the planet's slightly lower density and from the compositions of Martian meteorites. The low density is partially explicable if there is a greater proportion of more volatile elements.…

Buch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Mars is about one-eighth the mass of the Earth and it may provide an analogue of what the Earth was like when it was at such an early stage of accretion. The fur ther growth of the Earth was sustained by major collisions with planetesimals and planets such as that which resulted in the formation ofthe Earth's moon (Hartmann and Davis, 1975; Cameron and Ward, 1976; Wetherill, 1986; Cameron and Benz, 1991). This late accretionary history, which lasted more than 50 Myr in the case of the Earth (Halliday, 2000a, b), appears to have been shorter and less catastrophic in the case of Mars (Harper et ai. , 1995; Lee and Halliday, 1997). In this article we review the basic differences between the bulk composition of Mars and the Earth and the manner in which this plays into our understanding of the timing and mechanisms of accretion and core formation. We highlight some of the evidence for early cessation of major collisional growth on Mars. Finally, we reevaluate the isotopic evidence that Mars differentiated quickly. Fundamental differences between the composition of Mars and that of other terrestrial planets are apparent from the planet's slightly lower density and from the compositions of Martian meteorites. The low density is partially explicable if there is a greater proportion of more volatile elements.…

Zustand: New. pp. 512.

Zustand: New. pp. ix + 491, Map (Some Col.).

Paperback. Zustand: Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book.