Dawson k r (48 Ergebnisse)

Paperback. Zustand: Very Good. First Edition. Minimal wear to cover. Pages clean and binding tight. shelf wear. bumped edges Paperback. Charles C. Dawson;Charles M. Quinlan;R.C. Adams;K. Rudin;Unknown Artist;Charlie Wylie;Catherine Yronwode;Greywolf Townsend (illustrator).

Paperback. Zustand: Very Good. Children's nurses are faced with unique challenges when undertaking clinical skills, adapting their knowledge and practice for the physical and developmental age of their patients. The Oxford Handbook of Clinical Skills for Children's and Young People's Nursing is a practical guide to both the most basic and the increasingly complex elements of caring for the health needs of children and young people. Focusing on the key principles underpinning all elements of care, it provides a solid, evidence-based framework which practitioners can use to develop their clinical knowledge, skills, and attitudes. It systematically covers the body systems and the clinical skills relating to them, and includes additional tips and suggested courses of action when encountering difficulties with a procedure, with practical advice from current practitioners. Written by experienced children's nurses working either within clinical paediatric settings or as educators in the field, this handbook is an essential, quick, and reliable practice reference tool for any clinical setting. The book has been read, but is in excellent condition. Pages are intact and not marred by notes or highlighting. The spine remains undamaged.…

No Binding. Zustand: Very Good. ORIGINAL ARTICLE, disbound from Geological Survey of Canada publication; no covers; in very good condition. Journal.

Soft cover. Zustand: Very Good. Written in ink on top of plain front cover, With the writers' compliments. pp 549-556 plus three plates. 2nd inscribed at top "Prof. Bloom with compliments" with W. Bloom name stamp underneath, pp 645-652 plus plates. Plain brown wraps.

Paperback. Zustand: Brand New. In Stock.

Hardcover. Zustand: Very Good with no dust jacket. Unmarked, except for short dedication and signature of author. ; 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. Book Published without Dust Jacket.; Tables; 8vo 8" - 9" tall; 476 pages; B0025ZNQMW; Signed by Author DH1.…

Zustand: New.

Zustand: As New. Unread book in perfect condition.

Paperback. Zustand: Brand New. 96 pages. 8.50x5.60x0.70 inches. In Stock. Charles C. Dawson;Charles M. Quinlan;R.C. Adams;K. Rudin;Unknown Artist;Charlie Wylie;Catherine Yronwode;Greywolf Townsend (illustrator).

Hardcover. Zustand: Brand New. In Stock.

Kaupia 3: 179-192, 7 figs 4to, offprint.

Zustand: New.

Hardcover. Zustand: Good. Ex-library. The cover has dark blue cloth with goldtone letters and a vignette. 190 pages; color frontispiece; 71 b/w illustrations on plates. The front endpaper has a handwritten date in pencil of 1937. The spine strip has darkened. A few pages and the text block ends have light foxing. Three plates each have a closed tear on the bottom margin, 1 to 4 1/2 in. A diagonal bend line is on the front FEP, frontispiece, and first 24 pages. The pages have mild, musty odor. International shipping will require extra cost. Scans e-mailed upon request. A. Horace Gerrard and K. Leigh-Pemberton (illustrator).…

Zustand: As New. Unread book in perfect condition.

Zustand: 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.…

Zustand: 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.…

Zustand: 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.…

Zustand: 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.…

Zustand: 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 pages.…

Zustand: Very Good. x, 86, col photos, col text figs. A4. PB. Vg. Owner's name to title page. River Habitat Survey Report No. 2 May 1998. [9781873160428].

Taschenbuch. Zustand: Neu. Neuware.

1974, 1st edition. (Card covers) Very good. ix, 157pp. Minor yellow underlining on several pages in Appendix B. Includes map in seperate envelope. Map is seemingly unopened. Economic Geology Report 29.

Zustand: new. Pages: 400 Language: Russian. Glubokaja i nasyschennaja kniga-putevoditel dlja roditelej podrostkov, kotorym slozhno sosredotochitsja, byt organizovannymi i dovodit dela do kontsa.Esli vash rebenok postojanno otvlekaetsja, otkladyvaet domashnie zadanija na poslednij moment, iz-za chego ne uspevaet v shkole. I pri etom otvergaet pomosch, vosprinimaja ee kak vmeshatelstvo, govorit "otstan" i "eto moja zhizn" - vy ne odinoki. Eta kniga - o tom, kak ne sdatsja, ne poterjat kontakt i po-nastojaschemu pomoch.V osnove - unikalnaja model podderzhki, razrabotannaja esche v 80-e gody, proverennaja vremenem i aktualizirovannaja s uchetom sovremennykh realij. Avtory, opirajas na 40-letnij opyt raboty s podrostkami s SDVG i drugimi nejrootlichijami, deljatsja prakticheskimi instrumentami i podkhodami i objasnjajut, kak opredelit konkretnuju problemu i podobrat optimalnye sposoby reshenija. Oni ubezhdeny: u kazhdogo rebenka est silnye i slabye storony, vazhno lish nauchitsja videt i rabotat s nimi - bez davlenija, s ponimaniem i uvazheniem.Dlja kogo eta kniga- Dlja roditelej detej 8-13 let.- Dlja pedagogov srednej shkoly.- Dlja psikhologov, sotsialnykh rabotnikov, i vsekh, kto v professionalnoj dejatelnosti stalkivaetsja s problemami detej predpodrostkovogo i mladshego podrostkovogo vozrasta. 9785002144679.…

Softcover. Zustand: Good. 1832. A reasonably presentable map engraving, with some fairly significant impression marks caused by the original folding of the map, some light hand-colouring to highlight borders and limits. Neatly trimmed to prevent edge wear, and with vertical fold line as originally presented, carefully flattened and reinforced with conservation tape3 on the rear to prevent any significant wear. Why on Amazon do most sellers not describe their actual book? Buy with confidence and support a genuine Independent Bricks & Mortar Real Bookshop. We are Maynard & Bradley CAMBO & PBFA(now lapsed) members here in Leicester City Centre. Size: 225 x 300 mm. 1. Item Type: Book. Quantity Available: 1. Shipped Weight: Under 500 grams. Category: Geography & Maps; Britain/UK; 19th century; Inventory No: 47328.…

Softcover. Zustand: Good. 1832. A fairly well-presented map engraving, with some impression marks along the left side caused by the original folding of the map, some light hand-colouring to highlight borders and limits. Neatly trimmed to prevent edge wear, and with vertical fold line as originally presented, carefully flattened and reinforced on the rear to prevent any significant wear. Why on Amazon do most sellers not describe their actual book? Buy with confidence and support a genuine Independent Bricks & Mortar Real Bookshop. We are Maynard & Bradley CAMBO & PBFA(now lapsed) members here in Leicester City Centre. Size: 265 x 335 mm. 1. Item Type: Book. Quantity Available: 1. Shipped Weight: Under 500 grams. Category: Geography & Maps; Britain/UK; 19th century; Inventory No: 45741.…

Softcover. Zustand: Good. 1832. A fairly well-presented map engraving, with some impression marks along the left side caused by the original folding of the map, some light hand-colouring to highlight borders and limits. Neatly trimmed to prevent edge wear, and with vertical fold line as originally presented, carefully flattened and reinforced on the rear to prevent any significant wear. Why on Amazon do most sellers not describe their actual book? Buy with confidence and support a genuine Independent Bricks & Mortar Real Bookshop. We are Maynard & Bradley CAMBO & PBFA(now lapsed) members here in Leicester City Centre. Size: 240 x 310 mm. 1. Item Type: Book. Multiple copies available this title. Quantity Available: 2. Shipped Weight: Under 500 grams. Category: Geography & Maps; Britain/UK; 19th century; Inventory No: 45742.…

Softcover. Zustand: Good. 1832. A fairly well-presented map engraving, with some impression marks along the left side caused by the original folding of the map, some light hand-colouring to highlight borders and limits. Neatly trimmed to prevent edge wear, and with vertical fold line as originally presented, carefully flattened and reinforced on the rear to prevent any significant wear. Why on Amazon do most sellers not describe their actual book? Buy with confidence and support a genuine Independent Bricks & Mortar Real Bookshop. We are Maynard & Bradley CAMBO & PBFA(now lapsed) members here in Leicester City Centre. Size: 225 x 300 mm. 1. Item Type: Book. Quantity Available: 1. Shipped Weight: Under 500 grams. Category: Geography & Maps; Britain/UK; 19th century; Inventory No: 45746.…

Softcover. Zustand: Good. 1832. A fairly well-presented map engraving, clean across the entire image surface with only a few very faint spots, some light hand-colouring to highlight borders and limits. Neatly trimmed to prevent edge wear, and with corners patched and repaired with conservation tape to help preserve overall integrity. Why on Amazon do most sellers not describe their actual book? Buy with confidence and support a genuine Independent Bricks & Mortar Real Bookshop. We are Maynard & Bradley CAMBO & PBFA(now lapsed) members here in Leicester City Centre. Size: 220 x 340 mm. 1. Item Type: Book. Quantity Available: 1. Shipped Weight: Under 500 grams. Category: Geography & Maps; Britain/UK; 19th century; Inventory No: 45732.…

Softcover. Zustand: Good. 1832. A fairly well-presented map engraving, clean across the entire image surface with only a few very faint spots, some light hand-colouring to highlight borders and limits. Neatly trimmed to prevent edge wear, and with a a few small nicks repaired with conservation tape to help preserve overall integrity. Why on Amazon do most sellers not describe their actual book? Buy with confidence and support a genuine Independent Bricks & Mortar Real Bookshop. We are Maynard & Bradley CAMBO & PBFA(now lapsed) members here in Leicester City Centre. Size: 190 x 310 mm. 1. Item Type: Book. Quantity Available: 1. Shipped Weight: Under 500 grams. Category: Geography & Maps; Britain/UK; 19th century; Inventory No: 45737.…

Softcover. Zustand: Good. 1832. A fairly well-presented map engraving, clean across the entire image surface with only a few very faint spots, some light hand-colouring to highlight borders and limits. Neatly trimmed to prevent edge wear, and with a corner patched and repaired with conservation tape to help preserve overall integrity. Why on Amazon do most sellers not describe their actual book? Buy with confidence and support a genuine Independent Bricks & Mortar Real Bookshop. We are Maynard & Bradley CAMBO & PBFA(now lapsed) members here in Leicester City Centre. Size: 220 x 310 mm. 1. Item Type: Book. Quantity Available: 1. Shipped Weight: Under 500 grams. Category: Geography & Maps; Britain/UK; 19th century; Inventory No: 45736.…