Carel Otte (15 results)

Hardcover. Condition: Very Good. No Jacket. Missing dust jacket; May have limited writing in cover pages. Pages are unmarked. ~ ThriftBooks: Read More, Spend Less.

Hardcover. Condition: Good. Hardback with dust jacket; surplus library copy with some stamping; clean text, tight binding. Dust jacket, faded, edge wear, soiling, a few small tears.

Condition: Good. First. Pages intact with minimal writing/highlighting. The binding may be loose and creased. Dust jackets/supplements are not included. Stock photo provided. Product includes identifying sticker. Better World Books: Buy Books. Do Good.

Hardcover. Condition: Very Good. Dust Jacket Condition: Good. First Edition, Later Printing. Light brown covers with black printing. Pictorial dust jacket with several tears and chips; some soiling. Front endpapers have previous department stamp and glue residue.

Hardcover. Condition: VG. Dust Jacket Condition: No Dust Jacket. Covers exceptionally bright, clean; owner's name. Contents tight, unmarked. ;

Hardcover. Condition: Near Fine. Dust Jacket Condition: Very Good. Maps, Graphs, Tables (illustrator). 360 clean, unmarked pages/index; dj w/unclipped price; owner's name.

hardcover. Condition: 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!

Paperback. Condition: Very Good. First Edition. Unmrked, except for a numbr of marginal marks on a few pages. Previus owner's name on inside cover page. Bumping of most edges and corners. ; Book Description; Spine has no signs of creasing. Pages are clean and not marred by notes or folds. Covers are square with minor wear. Ships Safe and Fast. Late Pennsylvanian and early Permian strata in the northernmost Sacramento Mountains, NM, were studied to interpret their complex deposition in the south-central NM area, and to clarify the sedimentary and tectonic history. A critical area of about 80 mi2 was mapped on a scale of 4 inches equal to 1 mi, including 30 mi2 covered in detail. The map area covers the northern part of the Sacramento Mountains escarpment, which is a block that was uplifted in late Cenozoic time along a fault on the west and tilted to the east. Prior to this basin-and-range faulting, the rocks were gently folded in early Tertiary time and were intruded by Tertiary sills and dikes of acid and intermediate composition. Minor high-angle faults, largely associated with the boundary fault zone, occur in the area and locally complicate the structure. Late Pennsylvanian and early Permian folding and high-angle faulting occurred in the southeasternmost part of the map area. Quaternary stream deposits cover about one-fifth of the area, which otherwise is unusually well exposed. Folded plates in rear pocket. ; New Mexico. Bureau of Mines and Mineral Resources. Bulletin; Vol. 59; B&W Photographs; 8vo 8" - 9" tall; 111 pages DH3.

Soft cover. Condition: Good. ORIGINAL 1959 PUBLICATION; softcovers; includes fourteen folded plates in rear pocket (complete for this publication); ex-corporate library; spine reinforced with tape; gutter of first couple of pages reinforced w/ tape; o/w in good condition. Book.

Paperback. Condition: Good+. Unmarked, except for previous owner's name on front cover. Mild bumping of some corners and edges. ; Book Description; Spine has no signs of creasing. Pages are clean and not marred by notes or folds. Covers are square with minor wear. Ships Safe and Fast. Late Pennsylvanian and early Permian strata in the northernmost Sacramento Mountains, NM, were studied to interpret their complex deposition in the south-central NM area, and to clarify the sedimentary and tectonic history. A critical area of about 80 mi2 was mapped on a scale of 4 inches equal to 1 mi, including 30 mi2 covered in detail. The map area covers the northern part of the Sacramento Mountains escarpment, which is a block that was uplifted in late Cenozoic time along a fault on the west and tilted to the east. Prior to this basin-and-range faulting, the rocks were gently folded in early Tertiary time and were intruded by Tertiary sills and dikes of acid and intermediate composition. Minor high-angle faults, largely associated with the boundary fault zone, occur in the area and locally complicate the structure. Late Pennsylvanian and early Permian folding and high-angle faulting occurred in the southeasternmost part of the map area. Quaternary stream deposits cover about one-fifth of the area, which otherwise is unusually well exposed. Folded plates in rear pocket. ; New Mexico. Bureau of Mines and Mineral Resources. Bulletin 50; 8vo 8" - 9" tall; 111 pages DB2.

First Edition. Softcover. Bulletin 50. 111pp. Photo illustrated. Sleeve at rear of book has the 13 folded maps, (from small to very large) V.Goodl.

Hardcover. Condition: Very Good. Publisher: Stanford University Press, 1973, V.Good, HB, ISBN: 0-8047-0822-3. Book.

Condition: Good. Your purchase helps support Sri Lankan Children's Charity 'The Rainbow Centre'. Ex-library, so some stamps and wear, but in good overall condition. Our donations to The Rainbow Centre have helped provide an education and a safe haven to hundreds of children who live in appalling conditions.

Hardcover. X, 360 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. w10668 0804708223 Sprache: Englisch Gewicht in Gramm: 550.

Hardcover. Ehem. Bibliotheksexemplar mit Signatur und Stempel. GUTER Zustand, ein paar Gebrauchsspuren. Ex-library with stamp and library-signature. GOOD condition, some traces of use. Sprache: Englisch Gewicht in Gramm: 550.