Christopher kenneth w (51 résultats)

Hardcover. Etat : Fair.

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.

Etat : Very Good. Former library copy. Pages intact with possible writing/highlighting. Binding strong with minor wear. Dust jackets/supplements may not be included. Includes library markings. Stock photo provided. Product includes identifying sticker. Better World Books: Buy Books. Do Good.

Paperback. Etat : Very Good.

Hardcover. Etat : Good - Cash. Etat de la jaquette : Fair. General use wear, surface and edges rubbed. Corners bumped and show wear. Pages show reader wear. Secure pages, solid binding. Dust jacket has heavy wear, chipping, tears, and missing pieces. Stock photos may not look exactly like the book.

Wraps. Etat : Very Good+. Vol. 39, No. 5. Cover by Jack Gaughan for "Alpha Bets" (novelet) by Sonya Dorman. Includes "The Throne and the Usurper" (novelet) by Christopher Anvil; "The Mayday" by Keith Roberts; "Starting from Scratch" by Robert Sheckley; "The Misfortune Cookie" by Charles E. Fritch; "Time Dog" by Richard A. Lupoff. Special Reprint Feature: "The Venus of Ille" by Prosper Merimee. Features: "Films" by Baird Searles; "Science: -But How" by Isaac Asimov; Cartoon by Gahan Wilson". Heavy marks on contents pages, erased, but impressions remain; couple of minor edge chips; short tears at upper front cover edge. Magazine. …

Wraps. Etat : Very Good+ to Near Fine. Vol. 39, No. 5. Cover by Jack Gaughan for "Alpha Bets" (novelet) by Sonya Dorman. Includes "The Throne and the Usurper" (novelet) by Christopher Anvil; "The Mayday" by Keith Roberts; "Starting from Scratch" by Robert Sheckley; "The Misfortune Cookie" by Charles E. Fritch; "Time Dog" by Richard A. Lupoff. Special Reprint Feature: "The Venus of Ille" by Prosper Merimee. Features: "Films" by Baird Searles; "Science: -But How" by Isaac Asimov; Cartoon by Gahan Wilson". Tanning, else Near Fine. Magazine.…

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.

SingleIssueMagazine. Etat : Good to Very Good-. Vol. 54, No. 4 (Whole No. 323). Edited by Edward L. Ferman. Cover art by David Hardy for this "All British Issue". Includes "The Watched" (novella) by Christopher Priest; "Ariade Potts" (novelet) by Keith Roberts; "Three Ways" (novelet) by Brian W. Aldiss; "Marriage" (novelet) by Robert Aickman; "The Man Who Understood Carboniferous Flora" by John Brunner; "My Soul Swims in a Goldfish Bowl" by Ian Watson; "Drink Me, Francesca" by Richard Cowper; "Psycho Sis" by Kenneth Bulmer. Article: "The Gulf and the Forest: Contemporary SF in Britain" by Brian W. Aldiss. Departments: "Films and Television" by Baird Searles; "Cartoon" by Gahan Wilson; "Science: The Floating Crystal Palace" by Isaac Asimov. Bits of label remain on front cover; creasing, corner wear; mild tanning; minor soiling. Book. …

Etat : Trade paperback, New. New York: Hippocampus Press:, 2017. Trade paperback, New, 338 pp. "Lovecraftian Voyages is the eclectic amalgam expected of a man who is equally at home discussing Lovecraft's annual income as he is pondering proper pronunciation of Cthulhu. This is a book for everyone interested in the external influences of Lovecraft's life and how they shaped his career. Faig's research remains the gold standard; as fascinating, relevant, and valuable as when it was pulled from a typewriter in the early 1970s. This updated 2017 edition has been prepared for Hippocampus Press by editors Christopher M. O'Brien and J.-M. Rajala, who have augmented the text with chapter divisions to assist readers in locating particular topics. Additional annotations are provided, distinguished from Faig's notes. Finally, a thorough listing of works to date by and about Faig has been assembled, celebrating his unstinting and continuing devotion to the study of the Providence writer. S. T. Joshi has provided a new foreword.".…

Etat : New.

Paperback or Softback. Etat : New. Lovecraftian Voyages. Book.

Etat : As New. Unread book in perfect condition.

Soft Cover. Etat : Very Good. First Edition. 23 pp., references, 1 table, appendix, 11 figures, mathematical formulae. A NASA Technical Note in beige wrap. Minor foxing.; 4to - over 9¾" - 12" tall.

Octavo, pictorial wrappers. First published edition, revised and updated. The "holy grail" of Lovecraft scholars of the 1970s by "the man now credited with transforming research on Lovecraft and his circle from a haphazard collection of amateurs into a literary discipline unto itself." The bibliographic research is very out dated. Trade paperback format. A fine copy. (#174961).…

Etat : New.

Hardcover. Etat : Near Fine. Etat de la jaquette : Fair. 1st Edition. Copy from private WW2 book collection. Stated 5th impression. Dust Jacket is fair, tears and chips - but complete. Now in Brodart cover. Red Cloth cover has only slight rubbing at spine. Binding is tight. Inside pages are clean, crisp with no writing or marks except owners name (unrecognizable from anyone who doesn't know the signature) Revised Edition. Includes chapters on the history of the Soviet armed forces, the Soviet air force, the Soviet navy, the Soviet ground forces, strategic rocket forces, and an appendix on uniforms of the Soviet army. Not ex-library. Photos gladly provided. Additional postage for international delivery. …

Paperback. Etat : Very Good. 1st Thus. A creased spine with edge rubbings and a piece torn from the FFEP.No store stamp. Stories by : John Keith, Christopher Priest, Brian W. Aldiss, Cherry Wilder, David S. garnett, Laurence James, Ramsey Campbell, Ian Watson, Ritchie Smith & Thomas Penman.

Paperback. Etat : New.

Hardcover. Etat : New.

Etat : New. In English.

Etat : New.

Etat : As New. Unread book in perfect condition.

Softcover. xxix, 634 pp. Softcover. LCC: 868380 Very good condition; very light color fading along spine.

Hardcover. Etat : Very Good. 1st Edition. Book length examination of the influence of the Christian Right on the 2016 election from many established political scientists. Hardcover in cloth, no DJ if issued. Binding is solid, tight, sound. Interior is clean, bright, free of marks. Boards have some very minor rubbing and dust-soiled areas but are clean and firm. Attractive and relatively affordable copy of this hardcover which retails new at $120.…

paperback. Etat : Good. Number Three 1957 issue of Southerly, FROM THE LIBRARY OF AUSTRALIAN AUTHOR CHRISTOPHER KOCH, this issue including Koch's poem 'The Name' - flat-signed 'C Koch Dec. '57' to half-title page; being the Brennan Anniversary Number, marking the 25th anniversary of his death, and devoted to studies of his poetry, and also including poems by Olive Pell, RH Morrison, Robert Clark, and others; edited by Kenneth Slessor; hand-tipped b&w frontispiece showing a photo of Brennan in 1931 from the collection of Vince Kelly; mild watermark top corner of some pages, o.w. G-VG throughout; wraps lightly rubbed/tanned to spine . 60pp. large 8vo. Good. b&w frontispiece illustration (illustrateur).…

Etat : new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western North American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. " DV2. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.…

Etat : new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western North American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. " DV1. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.…

Etat : new. "The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western North American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea." DV4. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.…

Etat : new. The Proterozoic and Phanerozoic metallogenic and tectonic evolution of the Russian Far East, Alaska, and the Canadian Cordillera is recorded in the cratons, craton margins, and orogenic collages of the Circum-North Pacific mountain belts that separate the North Pacific from the eastern North Asian and western North American Cratons. The collages consist of tectonostratigraphic terranes and contained metallogenic belts, which are composed of fragments of igneous arcs, accretionary-wedge and subduction-zone complexes, passive continental margins, and cratons. The terranes are overlapped by continental-margin-arc and sedimentary-basin assemblages and contained metallogenic belts. The metallogenic and geologic history of terranes, overlap assemblages, cratons, and craton margins has been complicated by postaccretion dismemberment and translation during strike-slip faulting that occurred subparallel to continental margins. Seven processes overlapping in time were responsible for most of metallogenic and geologic complexities of the region (1) In the Early and Middle Proterozoic, marine sedimentary basins developed on major cratons and were the loci for ironstone (Superior Fe) deposits and sediment-hosted Cu deposits that occur along both the North Asia Craton and North American Craton Margin. (2) In the Late Proterozoic, Late Devonian, and Early Carboniferous, major periods of rifting occurred along the ancestral margins of present-day Northeast Asia and northwestern North America. The rifting resulted in fragmentation of each continent, and formation of cratonal and passive continental-margin terranes that eventually migrated and accreted to other sites along the evolving margins of the original or adjacent continents. The rifting also resulted in formation of various massive-sulfide metallogenic belts. (3) From about the late Paleozoic through the mid-Cretaceous, a succession of island arcs and contained igneous-arc-related metallogenic belts and tectonically paired subduction zones formed near continental margins. (4) From about mainly the mid-Cretaceous through the present, a succession of continental-margin igneous arcs (some extending offshore into island arcs) and contained metallogenic belts, and tectonically paired subduction zones formed along the continental margins. (5) From about the Jurassic to the present, oblique convergence and rotations caused orogen-parallel sinistral, and then dextral displacements within the plate margins of the Northeast Asian and North American Cratons. The oblique convergences and rotations resulted in the fragmentation, displacement, and duplication of formerly more continuous arcs, subduction zones, passive continental margins, and contained metallogenic belts. These fragments were subsequently accreted along the margins of the expanding continental margins. (6) From the Early Jurassic through Tertiary, movement of the upper continental plates toward subduction zones resulted in strong plate coupling and accretion of the former island arcs, subduction zones, and contained metallogenic belts to continental margins. In this region, the multiple arc accretions were accompanied and followed by crustal thickening, anatexis, metamorphism, formation of collision-related metallogenic belts, and uplift; this resulted in the substantial growth of the North Asian and North American continents. (7) In the middle and late Cenozoic, oblique to orthogonal convergence of the Pacific Plate with present-day Alaska and Northeast Asia resulted in formation of the present ring of volcanoes and contained metallogenic belts around the Circum-North Pacific. Oblique convergence between the Pacific Plate and Alaska also resulted in major dextral-slip faulting in interior and southern Alaska and along the western part of the Aleutian- Wrangell arc. Associated with dextral-slip faulting was crustal extrusion of terranes from western Alaska into the Bering Sea. DX1. softcover, wrapped in shrink wrap, tight, crisp, 429 pages.…