J M Dawson D D (47 results)

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

Paperback. Condition: Good. Book in Good condition.

Soft cover. Condition: Good. (1976) iii, 28 pp., 18 bw photos & figs. (U.S.Geol. Surv. Prof. Paper 932-A) Paper covers. Library stamp on cover, no other markings. Top page corners curled.

Hardcover. Condition: Near Fine. HC - Orange cloth boards with brown lettering. Slight 1/2" crackto head of spine, is this book's only flaw on exterior. EX-LIBRIS FEP bookplate and name in pencil FFEP, otherwise MINT with no markings or writing. B/W Photo Illustrated. 8vo. 180pp. --P.M. "D" Dawson.

Condition: New.

Condition: As New. Unread book in perfect condition.

Hardcover. Condition: Fine. Facsimile Edition>. Green soft cover in green folding slipcase. 1/300 copies. Illustrated with map. Facsimile reprint of 1879 publication. 192 pp. FINE in FINE folding slipcase.

Hardcover. Condition: Fine. Dust Jacket Condition: Fine. 1st Edition. 1st ed., 2nd printing ; ix, 310 pages ; 24 cm ISBN 9780760739549, 0760739544 OCLC 54409153 ; brown abd maroon cloth in color illustrated dustjacket ; Visions of Ghost Armies introduces you to a side of war you might never have imagined possible. In more than one hundred true stories--reported by eyewitnesses and sometimes verified by the media--you will read eerie and haunting accounts of spirit soldiers and armies of the night who still fight battles decades to centuries after their wars have ended. ; "From the files of FATE magazine." ; FINE/FINE. Book.…

Soft cover. Condition: Very Good. 64 pages. Cover art by Bernard Greenbaum. Dan S Ingman "O.D.J.B." / Jimmy Noone drawn by B ten Hove / Harold Taylor "Morgan Music" / Spike Hughes "West End Fall" / "Golden Rain" composed by Harry Gold (sheet music) / Norman Impey "New Vogue" / Gerald Moore "What Is Style?" / Harry Gold "Technique Trouble" / Leonard Feather "(Fats) Waller Hasn't Wilted" / Mickey Reinhardt "Hot Licks" / B M Lytton-Edwards "Pennies To Pounds" / Jerry dawson "Kick-Off" / T W Thurban "Imaginary Pupils" / Accordion Section (M16/2).…

Condition: New.

Soft cover. Condition: Near Fine. First Paperback Ed. & 1st Printing.. Inventory # D503-1 FATE (Pulp Digest Magazine); Vol. 6, No. 7, Issue 40, July 1953 True Stories on The Strange, The Unusual, The Unknown - Has Atlantis Been Found? - Socrates Published by Highland Park, IL: Clark Publishing Company, CONTENTS; ** STORIES (1) Murder by a Ghost by James Crenshaw (2) Fire in No. 1 Hold by Robert V. Hulse (3) The Phantom Horse by Capt. Hugh Thomason (4) Three Dreams in the Presidents Family by William Oliver Stevens (5) The Face Beneath the Rubble by Warrington Dawson (6) How Lost Was My Father? by Stuart Palmer; ** ARTICLES = (1) Telepathy in Pets by Dr. W. E. Farbstein (2) The Case of Katie King by Dr. W. D. Chesney (3) The "Demon" of Socrates by Alson J. Smith (4) Case of the Approved Spoon by Harriet S. Hollister and Gertrude O. Tubby (5) Italys Great Healer by J. M. Sheppard (6) Voices of the Silences by Sidney O. Burke (7) Has Atlantis Been Found? by L. Sprague de Camp; CONDITION; Near Fine; minor spine wear/ fray bottom/ top PRICE = $59 Size: 12mo - over 6¾" - 7¾" tall. Book.…

Condition: As New. Unread book in perfect condition.

Condition: 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.…

Condition: 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.…

Condition: 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, 4.…

Condition: 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.…

Condition: 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. softcover, wrapped in shrink wrap, tight, crisp, 429 page.…

Condition: As New. Unread book in perfect condition.

Condition: New.

Condition: New. Print on Demand.

Hardcover. Condition: Very Good. Dust Jacket Condition: Very Good. 1997 British Museum Press out of print hardcover edition. Light reading wear else very good condition. Contents: Introduction: Augustus Wollaston Franks - Towards a Portrait by David M. Wilson; Chapter 1: Collectors, Connoisseurs and Curators in the Victorian Age by Arthur MacGregor; Chapter 2: Antiquities and the Public: the Expanding Museum, 1851-96 by John Mack; Chapter 3: Franks and the British Museum - the Cuckoo in the Nest by Marjorie Caygill; Chapter 4: A Curator's Curator: Franks and the Stone Age Collections by Jill Cook; Chapter 5: Later Prehistory and Roman Britain: the Formation of the National Collections by T.W. Potter; Chapter 6: Franks and Ethnography by J.C.H. King; Chapter 7: 'Some recollection of me when I am gone': Franks and the Early Medieval Archaeology of Britain and Ireland by Marjorie Caygill; Chapter 8: Franks and the Medieval Collections by John Cherry; Chapter 9: Franks and European Ceramics, Glass and Enamels by Aileen Dawson; Chapter 10: Oriental Pottery and Porcelain by Jessica Harrison-Hall; Chapter 11: Franks and the Oxus Treasure by John Curtis; Chapter 12: Sculpture from India by Michael D. Willis; Chapter 13: The Art and Antiquities of Japan by Lawrence Smith; Chapter 14: 'Islamism, not an easy matter' by Rachel Ward; Chapter 15: Early Scientific Instruments and Horology by R.G.W. Anderson; Chapter 16: The Legacy of Edward Hawkins: Franks as Numismatist by Luke Syson; Chapter 17: Franks as a Bookplate Collector by Brian North Lee.…

Condition: New.

Condition: New.

Hardcover. Condition: Very Good. Dust Jacket Condition: Very Good. 2012 Cambridge University Press hadrcover edition. Light reading wear else very good condition. Bringing together a team of international scholars, this volume provides the first substantial text dedicated to the various contexts that frame Wharton's remarkable career. Each essay offers a clearly argued and lucid assessment of Wharton's work as it relates to seven key areas: life and works, critical receptions, book and publishing history, arts and aesthetics, social designs, time and place, and literary milieux. These sections provide a broad and accessible resource for students coming to Wharton for the first time while offering scholars new critical insights. CONTENTS: Part I. Life and Works 1. Edith Wharton: contextual revisions by Laura Rattray 2. Chronology: Wharton in cultural and historical context by Pamela Knights and Laura Rattray 3. Biography by Melanie Dawson 4. Composition and publication by Sharon Kehl Califano 5. Portraits of Wharton by Susan Goodman Part II. Critical Receptions 6. Contemporary reviews, 1877-1938 by Heidi M. Kunz 7. Obituaries by Linda De Roche 8. 'Justice' to Edith Wharton? The early critical responses by Melissa M. Pennell 9. Modern critical receptions by Jessica Schubert McCarthy Part III. Book and Publishing History 10. Wharton and her editors by Sharon Shaloo 11. Selling Wharton by Gary Totten 12. Serialization by Elsa Nettels 13. Short story markets by Bonnie Shannon McMullen Part IV. Arts and Aesthetics 14. Stage adaptations of Wharton's fiction by John Dennis Anderson 15. Wharton's writings on screen by Anne-Marie Evans 16. Visual arts by Emily J. Orlando 17. Architecture by Cecilia Macheski 18. Interior and garden design by Helena Chance 19. Images of Wharton by Katherine Joslin Part V. Social Designs 20. The marriage market by Pamela Knights 21. Leisured lives by Maureen E. Montgomery 22. Wharton and gender by Linda Wagner-Martin 23. Race and imperialism by Margaret Toth 24. Social transitions by Adam Jabbur Part VI. Time and Place 25. Wharton and France by William Blazek 26. Wharton and Italy by Robin Peel 27. Wharton and World War I by Julie Olin-Ammentorp 28. The 1920s by Gail D. Sinclair 29. Wharton and the Great Depression by Carol J. Singley Part VII. Literary Milieux 30. Literary influences by Judith P. Saunders 31. Wharton and the American romantics by Linda Costanzo Cahir 32. The novel of manners by Cecilia Macheski 33. Naturalism by Donna Campbell 34. Modernism by Jennifer Haytock.…

Condition: New.

Condition: New.

Condition: As New. Unread book in perfect condition.

Condition: Sehr gut. Zustand: Sehr gut | Seiten: 364 | Sprache: Englisch | Produktart: Bücher | Keine Beschreibung verfügbar.

Condition: New.

Condition: New.