Frye john a (125 résultats)

Etat : Good. 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.

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

Hardcover. Etat : Good. No Jacket. Former library book; Pages can have notes/highlighting. Spine may show signs of wear. ~ ThriftBooks: Read More, Spend Less.

hardcover. Etat : As New. Feels unopened. Perfect condition.

paperback. Etat : Very Good. This book is in very good condition, with only minor signs of wear and use. The pages may contain limited notes or highlighting, but overall, the text remains clean and legible. The cover and spine are also in great shape, with only minimal shelf wear or creasing. This book has been well-maintained and still presents a clean and attractive appearance. Textbooks may not include supplemental items i.e. CDs, access codes etc.…

Etat : Very Good. Item in very good condition! Textbooks may not include supplemental items i.e. CDs, access codes etc.

Paperback. Etat : Very Good. Vol 37, No 11, pp. 2581-2586, Illus, Author's Offprint, name on cover else VG.

hardcover. Etat : 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. Etat : Good. The cover and the pages at the front and back have shelf-wear at the corners from storage. No writing or underlining on any page. Size: 8vo - over 7¾" - 9¾" tall.

Hard Cover. First Edition, First printing. FINE IN FINE DJ.

Paperback. Etat : Fine. Bull 109, Pt 3, 33-48, Photos, Orig Grey Author's Offprint, name on cover else Fine.

paperback. Etat : Very good condition. very clean,fast ship.

Pamphlet. Etat : Very Good. 1st Edition. pp. 429-444, Extracted from orig vol, thus begins with title page, trimmed & stapled pamphlet, else VG.

PB. Etat : very good, wraps (softcover). 44pp.

Etat : As New. Unread book in perfect condition.

Soft cover. Etat : As New. The book appears unread and in excellent condition, with clean, crisp pages and a tight binding. No annotations or markings.

PB. Etat : very good, wraps (softcover). 23pp.

10 x 7, wrappers, 25 pp, 1 plate, 3 figures, bib, index, lower fore corner bumped. FIRST ED.

Etat : New.

Etat : New.

Pamphlet. Etat : Fine. 8vo; 7 pages.

Paperback. Etat : Good. covers have minor wear and soil, corners creased, stapled binding tight, interior clean, 23 pages, study and description of molluscan faunas of the Illinoian and Kansan Stages, bw maps, tables and graphs Size: 6.75 x 10.

Paperback. Etat : Good. covers have minor wear and soil, corners creased, stapled binding tight, interior clean, 12 pages, study of an exposure at Morris Illinois revealing an extensive lake was present in the upper Illinois Valley during Famdalian time, bw map and diagram Size: 6.75 x 10.

Trade Paperback. Etat : Very Good. 162 pp. Solidly bound copy with moderate external wear, crisp pages and clean text. Creased front cover. Damage to spine. John Clift (Cover Design) (illustrateur).

Etat : New.

Etat : New. In English.

Etat : As New. Unread book in perfect condition.

Soft cover. Etat : Good. No Jacket. STUDIES OF CENOZOIC GEOLOGY ALONG EASTERN MARGIN OF TEXAS HIGH PLAINS, ARMSTRONG TO HOWARD COUNTIES (Bureau of Economic Geology Report of Investigations No. 32), John Chapman Frye and A. Byron Leonard, softcover, illustrations (maps, drawings, photos, charts), two-staple binding covered by wraps, 1957. BOOK CONDITION: Good. The text block and illustrations are in fine condition, with no tears, marks, or dog-ears. There is no bookplate but the signature of prior owner is written inside each cover. Not a library book nor remainder. The green wraps are in good condition (faded and discolored along edges). 10 x 7, 62 pages, 8 ounces. [From the Handbook of Texas] The High Plains region, the northern and western side of Texas from the Panhandle to the Pecos River, is physiographically a quadrangular, mesa-like area that rises perceptibly by sharp escarpments above the adjacent lowlands to the east and to the west. It is characterized by a constructional topography formed on thick deposits of wind-blown materials that blanket the region. The textures of these materials vary from east to west, the finest textures occurring in an eastward zone, the coarser or sandy textures in a westward zone, with a transitional zone in between. The natural vegetation of the High Plains region consists primarily of short grasses, the northern portion of the Texas High Plains being one of the most distinctive short grass regions of the United States. To the south is a considerable growth of mesquite shrubs. The deep sand strips, particularly at the southwest, are characterized by shinnery growth admixed with tall bunch grasses, yucca, and associated herbs. Most of the High Plains country lies in the black earth or Cheronzem soils zone-a belt of country extending from the lower Rio Grande and the southern portion of the Texas Gulf coast northward across the middle and northern Great Plains well into the plains of western Canada. The Texas portion of the black earth makes up most of the southern third of this soils zone as it occurs in the United States. Agriculturally, the middle sector of the black earth, which is also the middle sector of the Great Plains, is predominantly the hard winter wheat region of the United States. This region extends southward well into the High Plains, occupying most of the Texas Panhandle. South of the Plainview area, cotton and grain sorghums are the dominant crops. Although topographically the High Plains region is an upland, it overlies a great basin-the Permian basin-which is a part of the Great Plains geosyndine; the latter is a vast structural feature lying eastward of the Rocky Mountains. Although the surface of the High Plains consists of a veneer of deposits geologically recent, the region is underlain by a thick agglomeration of Permian deposits, below which are still older beds of the Early Paleozoic, which in turn rest on the pre-Cambrian basement. In the Permian basin region occurs a complex of geologic features, the complicated character of which still poses unsolved problems even to the specialist in the geology of the area. In brief, however, the Permian basin consists of two sub-basins, the western Delaware basin and the eastern Midland basin, together with the West Texas, or Central Basin Platform in between. These sub-surface features are important for the oilfields of West Texas and southeastern New Mexico, which are aligned with reference to them. Great reserves make the High Plains one of the outstanding oil and gas regions of the state. …

Etat : As New. Unread book in perfect condition.

Soft Cover. Etat : Good. Softcovers; ex--library; shelfwear w/ corners of wraps and leaves creased; a couple of tears on upper paper covering of spine w/ small portion uppermost paper covering of spine perished; o/w in good condition.