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Mass Market Paperback. Condizione: Very Good-. 6th printing #26906. Cover art is uncredited. "The complete script, with many photographs, cartoons and newspaper articles of the astounding aftermath! An introductory interview with Arthur C. Clarke." Cover partially sunned 9see scan); tanning; a little creasing. Book.

115 S., brosch., guter zustand,

Hardcover. Condizione: very good. Very Good Copy. Customer Service Guaranteed.

Taschenbuch, Condizione: Gut. 239 Seiten, Papierqualität und Alter führten zu einer Nachdunklung der Seiten und der Buchschnitt ist angebräunt. Im übrigen ist das Taschenbuch in einem guten Zustand. Sprache: Deutsch Gewicht in Gramm: 300.

guter Zustand. Lesebuch Asyl Gewicht in Gramm: 550.

guter Zustand. Lesebuch Vorurteile Gewicht in Gramm: 550.

Illustriert. Pappeinband 22x15 cm, Einband stark berieben und fleckig, Rücken repariert, Namenseinträge auf Vorsatzblatt und Titelseite, sehr vereinzelt Bleistiftmarkierungen. 126 S. Gewicht in Gramm: 270.

Mit Abb. a. Taf. 592 S. OLwd. - Gutes Ex. 1.

Softcover. Seiten 669 - 756 der fortlaufenden Jahrgangspaginierung mit mehreren Textabbildungen und den Tafeln 58 - 61. Gelbes Originalheft. 25 x 17,5 cm. Durchgehend wellig und minimal feuchtrandig. Insgesamt jedoch sauberes Exemplar in noch gutem Zustand. -- Bitte Portokosten außerhalb EU erfragen! / Please ask for postage costs outside EU! / S ' il vous plait demander des frais de port en dehors de l ' UE! // Bitte beachten Sie auch unsere Fotos! / Please also note our photos! / Veuillez noter nos photos -- Nehmen Sie sich ein gutes Buch mit auf die Sommerwiese. Bei uns werden Sie fündig! -- Wir kaufen Ihre werthaltigen Bücher! K21696-209872.

Heft; Condizione: Gut. 10 Seiten mit zahlr. Ill. Separatum/Sonderdruck aus wissenschaftlicher Bibliothek mit den entsprechenden Kennzeichnungen (Vermerke, Stempel.); Seiten alters-/papierbedingt angebräunt; ansonsten ordentlicher Erhaltungszustand. Aufgrund der Rarität und des geringen Umfangs des Werkes bitten wir um Verständnis, dass dieser Sonderdruck vom Rückgaberecht ausgeschlossen ist. Sprache: Deutsch Gewicht in Gramm: 80.

Condizione: 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.

Condizione: 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.

Condizione: 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.

Condizione: 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.

Condizione: 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.

Hardcover. Gr.-8° ( 23 : 16 cm). Neuerer Halbleinenband mit goldgeprägtem Rückentitel. (4), 570 Seiten mit sehr zahlreichen Abbildungen, Skizzen, Diagrammen etc. Auf dem vorderen Vorsatz mit Stempel: Mit den besten Empfehlungen überreicht von P. A. Thiessen. Mit eingebunden zwei Gedenkphotos für Uffz. Konrad Bläsius, gef. als Fallschirmjäger auf Kreta 20.5.1941 und Uffz. Heinz Böge, gef. 22.7.1941 in Rußland. Innen wie außen sauber, gutes Exemplar. Es handelt sich um gesammelte Sonderabdrucke aus diversen Fachzeitschriften wie z.B.: VDI-Beihefte, Ztschr. für anorg. und allgem. Chemie, Ztschr. für physik. Chemie, Justus Liebig's Annalen der Chemie, aber auch um Vorträge bei versch. Institutionen. Beiträge unter anderem von . -- Bitte Portokosten außerhalb EU erfragen! / Please ask for postage costs outside EU! / S ' il vous plait demander des frais de port en dehors de l ' UE! // Bitte beachten Sie auch unsere Fotos! / Please also note our photos! / Veuillez noter nos photos -- Nehmen Sie sich ein gutes Buch mit auf die Sommerwiese. Bei uns werden Sie fündig! -- Wir kaufen Ihre werthaltigen Bücher! Chem.

Gebundene Ausgabe, Halbleinen. Condizione: Gut. 1. Auflage. 291Seiten, mit s.w. Abbildungen. Buch gut erhalten, Einband und Buchrücken angeschmutzt, Buchblock vom Einband etwas gelöst, Seiten altersbedingt nachgedunklt, Schnitt angeshcmutzt. Sprache: Deutsch Gewicht in Gramm: 520.

Softcover. Condizione: Wie neu. 1. Auflage. 380 S., 6 Hefte , neuwertig.

Niederlanden. Akademie für Raumforschung und Landesplanung. V+69 S.Quart.m.Abb.Kt.-2). Akademie für Raumforschung. Hannover. 1988. Mit Gebrauchsspuren/Used condition. Kartoniert/Paperback. Sprache: deutsch/german.

Broschur, 8°. Condizione: Neu. 1998. 216 S. Buch ist neu, aus priv. Vorbesitz, ungelesen. -----Inhalt:. This little book is conceived as a service to mathematicians attending the 1998 International Congress of Mathematicians in Berlin. It presents a comprehensive, condensed overview of mathematical activity in Berlin, from Leibniz almost to the present day (without, however, including biographies of living mathematicians). Since many towering figures in mathematical history worked in Berlin, most of the chapters of this book are concise biographies. These are held together by a few survey articles presenting the overall development of entire periods of scientific life at Berlin. Overlaps between various chapters and differences in style between the chap ters were inevitable, but sometimes this provided opportunities to show different aspects of a single historical event - for instance, the Kronecker-Weierstrass con troversy. The book aims at readability rather than scholarly completeness. There are no footnotes, only references to the individual bibliographies of each chapter. Still, we do hope that the texts brought together here, and written by the various authors for this volume, constitute a solid introduction to the history of Berlin mathematics. Mathematics at the Prussian Academy of Sciences 1700-1810.- Mathematics in Berlin, 1810-1933.- Augustus Leopold Crelle.- Gustav Peter Lejeune Dirichlet.- Carl Gustav Jacob Jacobi.- Jacob Steiner and Synthetic Geometry.- Gotthold Eisenstein.- Kummer and Kronecker.- Weierstrass and some members of his circle: Kovalevskaia, Fuchs, Schwarz, Schottky.- Frobenius, Schur, and the Berlin Algebraic Tradition.- Erhard Schmidt, John von Neumann.- Constantin Carathéodory.- Richard von Mises.- Einstein in Berlin.- The Nazi era: the Berlin way of politicizing mathematics.- The University of Berlin from Reopening until 1953.- Helmut Hasse, Hermann Ludwig Schmid and their students in Berlin.- Freie Universität Berlin, a summary of its history.- Mathematics at the Berlin Technische Hochschule/Technische Universität.- Mathematics in Berlin at the Humboldt University: from 1953 until now.- The Mathematical Institute of the Academy of Sciences of the GDR.- Fast Algorithms, Fast Computers: The Konrad-Zuse-Zentrum Berlin (ZIB).- Weierstrass Institute for Applied Analysis and Stochastics (WIAS).- Zentralblatt für Mathematik und ihre Grenzgebiete.- Sources of photographs.- Addresses of authors and editors. ISBN: 9783764359430 Wir senden umgehend mit beiliegender MwSt.Rechnung. Sprache: Englisch Gewicht in Gramm: 288.

Lesebuch Asyl. 223 S. gr.8. mit Textabbildungen. ISBN: 3797102593. Signal. Baden-Baden. 1987. Guter Zustand/Good condition. Leinen mit Schutzumschlag/Hardcover/Dustjacket. Sprache: deutsch/german.

Hardcover. Originalpappband im Schutzumschlag, 21 x 15 cm, 158 Seiten, gut erhalten. -- Bitte Portokosten außerhalb EU erfragen! / Please ask for postage costs outside EU! / S ' il vous plait demander des frais de port en dehors de l ' UE! // Bitte beachten Sie auch unsere Fotos! / Please also note our photos! / Veuillez noter nos photos -- Nehmen Sie sich ein gutes Buch mit auf die Sommerwiese. Bei uns werden Sie fündig! -- Wir kaufen Ihre werthaltigen Bücher! Paeda.

No Binding. Condizione: As New. First Edition. 12" LPs. Sealed in the original plastic; never played. Date not visible on outside, but appears to be from the 1970s or earlier.

Paperback. Condizione: New.

143 S. m. zahlr. Ill., 21,5 x 17 cm, ill. OPbd. (Gutes Exemplar) Versand per Deutsche Post /DHL. Vorkasse grundsätzlich vorbehalten. BECAUSE OF THE EPR REGULATION NO SHIPPIMG POSSIBLE TO AUSTRIA, BULGARIA, FRANCE, GREECE, LUXEMBOURG, POLAND, ROMANIA, SWEDE, SLOVAKIA, SPAIN. Sprache: Deutsch Gewicht in Gramm: 500.

paperbound, samll 8vo, 10 volumes ca. 1000 pp. nrs. 49, 42, 97, 83, 29, 73, 69, 109, 102, 50 of the series; very good condition (almost unused).

328 S. m. zahlr. Abb., 22 x 23 cm, OKart. (Gutes Exemplar) Versand per Deutsche Post /DHL. Vorkasse grundsätzlich vorbehalten. BECAUSE OF THE EPR REGULATION NO SHIPPIMG POSSIBLE TO AUSTRIA, BULGARIA, FRANCE, GREECE, LUXEMBOURG, POLAND, ROMANIA, SWEDE, SLOVAKIA, SPAIN. Sprache: Deutsch Gewicht in Gramm: 1500.

250 (2) s. + planschsid. Förlagsband med skyddsomslag.

Gr.-8°. Mit12 farb. Tafeln und zahlr. Textillustrationen. 32 Bll. Farb. illustr. OHln. (fleckig, beschabt und bestoßen. Kanten und Ecken mit Läsuren. Papier wasserrandig und etw. gebräunt).

Regierungsbezirks Hildesheim. 1. Teil: Unterstufe. Vlg. C. Meyer. Hann. 1929. VII + 126 S. gr8. m. zahlr. Zeichnungen. Hln. -3/4).