Roman k w (32 resultados)
Editorial: Academic Press, New York, 1957
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- Primera edición
Librería: Archer's Used and Rare Books, Kent, OH, Estados Unidos de AmericaArcher's Used and Rare Books
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EUR 3,66
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Añadir al carritoHardcover (Original Cloth). Condición: Good (ex-library). 1st Edition. Bookplate. Ex-library copy. Quantity Available: 1. Category: Science & Technology; Botany; Pictures of this item not already displayed here available upon request. Inventory No: 2236.
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Librería: California Books, Miami, FL, Estados Unidos de AmericaCalifornia Books
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EUR 17,17
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Condición: New.
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Librería: GreatBookPrices, Columbia, MD, Estados Unidos de AmericaGreatBookPrices
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EUR 15,23
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Condición: As New. Unread book in perfect condition.
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Librería: Better World Books, Mishawaka, IN, Estados Unidos de AmericaBetter World Books
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EUR 17,70
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Condición: 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.
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Librería: GreatBookPrices, Columbia, MD, Estados Unidos de AmericaGreatBookPrices
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EUR 15,68
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Condición: New.
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Librería: California Books, Miami, FL, Estados Unidos de AmericaCalifornia Books
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EUR 18,08
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Condición: New.
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Librería: GreatBookPrices, Columbia, MD, Estados Unidos de AmericaGreatBookPrices
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EUR 19,30
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Condición: New.
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Librería: California Books, Miami, FL, Estados Unidos de AmericaCalifornia Books
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EUR 21,69
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Condición: New.
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Librería: PBShop.store US, Wood Dale, IL, Estados Unidos de AmericaPBShop.store US
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EUR 21,92
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PAP. Condición: New. New Book. Shipped from UK. Established seller since 2000.
Editorial: Ziff-Davis Publishing Company, 1951
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Librería: Books From California, Simi Valley, CA, Estados Unidos de AmericaBooks From California
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EUR 9,04
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Añadir al carritopaperback. Condición: Good. Minor chipping and creasing to the wraps, pages tanned.
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Librería: GreatBookPrices, Columbia, MD, Estados Unidos de AmericaGreatBookPrices
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EUR 21,62
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Condición: As New. Unread book in perfect condition.
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Librería: PBShop.store UK, Fairford, GLOS, Reino UnidoPBShop.store UK
Contactar con el vendedorVendedor de 5 estrellasCondición: Nuevo
EUR 19,64
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PAP. Condición: New. New Book. Shipped from UK. Established seller since 2000.
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Librería: GreatBookPricesUK, Woodford Green, Reino UnidoGreatBookPricesUK
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EUR 22,72
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Condición: As New. Unread book in perfect condition.
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Librería: GreatBookPricesUK, Woodford Green, Reino UnidoGreatBookPricesUK
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EUR 29,09
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Condición: As New. Unread book in perfect condition.
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Librería: GreatBookPricesUK, Woodford Green, Reino UnidoGreatBookPricesUK
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EUR 30,75
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Condición: New.
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Librería: GreatBookPricesUK, Woodford Green, Reino UnidoGreatBookPricesUK
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EUR 34,07
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Condición: New.
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- Primera edición
Librería: Xerxes Fine and Rare Books and Documents, Glen Head, NY, Estados Unidos de AmericaXerxes Fine and Rare Books and Documents
Contactar con el vendedorVendedor de 5 estrellasCondición: Usado - Muy bueno
EUR 22,60
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Añadir al carritoCondición: Near Fine. The Hague 1957 first edition. Published by Dr. W. Junk. Hardcover large 8vo., 246p. Institution stamp on verso of title page, Near Fine in Fairly Good DJ.
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Editorial: USGS, 2005
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Librería: Crossroads Books, Reno, NV, Estados Unidos de AmericaCrossroads Books
Contactar con el vendedorVendedor de 5 estrellasMiembro de asociación: IOBA
Condición: Nuevo
EUR 37,06
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Condición: 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 No…rth 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.
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Editorial: USGS, 2005
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Librería: Crossroads Books, Reno, NV, Estados Unidos de AmericaCrossroads Books
Contactar con el vendedorVendedor de 5 estrellasMiembro de asociación: IOBA
Condición: Nuevo
EUR 37,06
Envío por EUR 4,43Se envía dentro de Estados Unidos de AmericaCantidad disponible: 2 disponibles
Condición: 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 No…rth 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.
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Editorial: USGS, 2005
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Librería: Crossroads Books, Reno, NV, Estados Unidos de AmericaCrossroads Books
Contactar con el vendedorVendedor de 5 estrellasMiembro de asociación: IOBA
Condición: Nuevo
EUR 37,06
Envío por EUR 4,43Se envía dentro de Estados Unidos de AmericaCantidad disponible: 3 disponibles
Condición: 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 No…rth 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.
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Editorial: USGS, 2005
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Librería: Crossroads Books, Reno, NV, Estados Unidos de AmericaCrossroads Books
Contactar con el vendedorVendedor de 5 estrellasMiembro de asociación: IOBA
Condición: Nuevo
EUR 37,06
Envío por EUR 4,43Se envía dentro de Estados Unidos de AmericaCantidad disponible: 7 disponibles
Condición: 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 Nor…th 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.
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Editorial: USGS, 2005
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Librería: Crossroads Books, Reno, NV, Estados Unidos de AmericaCrossroads Books
Contactar con el vendedorVendedor de 5 estrellasMiembro de asociación: IOBA
Condición: Nuevo
EUR 37,06
Envío por EUR 4,43Se envía dentro de Estados Unidos de AmericaCantidad disponible: 2 disponibles
Condición: 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 Nor…th 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.
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Librería: Grand Eagle Retail, Bensenville, IL, Estados Unidos de AmericaGrand Eagle Retail
Contactar con el vendedorVendedor de 5 estrellasCondición: Nuevo
EUR 16,90
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Paperback. Condición: new. Paperback. She needs to ditch her past. He needs to believe in his future. Caroline Santos is chasing a clean slate. After a scandal shatters her reputation, she escapes across the country to take a lifeguarding job in her old hometown. As she settles in, she earns the respect of her coworkers and puts… a toe in the water of forming new friendships. But she keeps her defenses up, unwilling to trust too deeply-especially with the handsome but annoying fellow lieutenant she can't quite read.and who doesn't seem to like her much either. Is the key to rebuilding her sense of community, safety, and happiness getting him on her side-or is he a threat she can't risk?Jason Lowe has always loved the job. With the Cape May Beach Patrol, he thrives on the ocean, the responsibility, and the physical demands of guarding. Still, he struggles to see himself as a true leader, weighed down by his family's belief that lifeguarding isn't a "real" career. So, when Caroline arrives-confident, unapologetically proud, and razor-sharp-he's intrigued, but every attempt to connect with her seems to backfire.As the team works, trains, and competes together, Jason catches glimpses of the woman beneath the tough exterior, and her opinions start to reshape how he views himself. For Caroline, the past constantly threatens the progress she's trying to make. To truly move forward, she'll have to learn to trust-and risk opening her heart again-or watch all she's worked for slip away. Caroline needs to ditch her past. Jason needs to believe in his future. In this enemies-to-lovers romance, these two lifeguards compete as they work and learn to trust themselves and what they can be together. This item is printed on demand. Shipping may be from multiple locations in the US or from the UK, depending on stock availability.
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Idioma: Inglés
Editorial: Anessa Books Mai 2025, 2025
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Librería: AHA-BUCH GmbH, Einbeck, AlemaniaAHA-BUCH GmbH
Contactar con el vendedorVendedor de 5 estrellasCondición: Nuevo
EUR 23,68
Envío por EUR 62,04Se envía de Alemania a Estados Unidos de AmericaCantidad disponible: 2 disponibles
Taschenbuch. Condición: Neu. Neuware - Kaya's heart is shattered-she's reeling with the grief of losing her parents, she's been dumped, and is stuck in a job that has lost its meaning. Having somewhat recklessly fled to her family's old beach cottage, she questions her choices and even her sanity as she struggles with how to hea…l and move forward.Lucas is fine, thank you very much. He's a rising star well on his way to snagging his dream job, and has a good life in the shore town where he grew up, including friends who he's proud to have depend on him. He doesn't need anything else.that is, until a woman with a link to his past blows into town and he can't look away. The little shore town starts to work its magic-the locals including mysterious, handsome Lucas start to make Kaya feel things again. Can Kaya push past the deep scars of her trauma to put her heart back together Can Lucas trust himself enough to earn and hold onto the affection of this broken woman who has fascinated him for so long Or are some wounds too deep to overcome.
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Idioma: Inglés
Editorial: Anessa Books Nov 2025, 2025
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Librería: AHA-BUCH GmbH, Einbeck, AlemaniaAHA-BUCH GmbH
Contactar con el vendedorVendedor de 5 estrellasCondición: Nuevo
EUR 28,44
Envío por EUR 62,02Se envía de Alemania a Estados Unidos de AmericaCantidad disponible: 2 disponibles
Taschenbuch. Condición: Neu. Neuware - She's writing the next chapter of her life story one decision at a time.and overthinking all of them. Lucy Torres is stuck. Don't misunderstand-she loves her friends, her town, her work; she even loves having her mom as her roomie. Life is comfortable. Predictable. Safe. But now her mom wan…ts to downsize to a condo of her own, and Lucy has to face that her 'temporary' living situation has lasted a little too long. It's time for change. The trouble is, Lucy's been waiting. For the spark her grandmother swore would come in her twenty-sixth year-this year-the magic that would point her toward what's supposed to come next in her life. Lucy wants to move forward, but only with purpose. She wants direction. A nudge from the universe. Some sort of a sign, but she hasn't yet seen one. So when a charming newcomer sweeps her off her feet, Lucy dares to believe the moment has arrived. Maybe this is the sign she's been holding out for. But the more she chases a different life, the harder it gets, and she risks overlooking the quiet truth that's been unfolding around her all along. In the end, Lucy will have to dig deep and decide what is worth trusting: magic that dazzles, or love that lasts.
Data Mining: A Knowledge Discovery Approach
Cios, Krzysztof J., Pedrycz, Witold, Swiniarski, Roman W., K
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Librería: Mispah books, Redhill, SURRE, Reino UnidoMispah books
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EUR 153,27
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Paperback. Condición: Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book.
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Librería: Chiron Media, Wallingford, Reino UnidoChiron Media
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EUR 349,23
Envío por EUR 18,15Se envía de Reino Unido a Estados Unidos de AmericaCantidad disponible: 5 disponibles
Hardcover. Condición: New.
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Librería: AussieBookSeller, Truganina, VIC, AustraliaAussieBookSeller
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EUR 30,94
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Paperback. Condición: new. Paperback. She needs to ditch her past. He needs to believe in his future. Caroline Santos is chasing a clean slate. After a scandal shatters her reputation, she escapes across the country to take a lifeguarding job in her old hometown. As she settles in, she earns the respect of her coworkers and puts… a toe in the water of forming new friendships. But she keeps her defenses up, unwilling to trust too deeply-especially with the handsome but annoying fellow lieutenant she can't quite read.and who doesn't seem to like her much either. Is the key to rebuilding her sense of community, safety, and happiness getting him on her side-or is he a threat she can't risk?Jason Lowe has always loved the job. With the Cape May Beach Patrol, he thrives on the ocean, the responsibility, and the physical demands of guarding. Still, he struggles to see himself as a true leader, weighed down by his family's belief that lifeguarding isn't a "real" career. So, when Caroline arrives-confident, unapologetically proud, and razor-sharp-he's intrigued, but every attempt to connect with her seems to backfire.As the team works, trains, and competes together, Jason catches glimpses of the woman beneath the tough exterior, and her opinions start to reshape how he views himself. For Caroline, the past constantly threatens the progress she's trying to make. To truly move forward, she'll have to learn to trust-and risk opening her heart again-or watch all she's worked for slip away. Caroline needs to ditch her past. Jason needs to believe in his future. In this enemies-to-lovers romance, these two lifeguards compete as they work and learn to trust themselves and what they can be together. This item is printed on demand. Shipping may be from our Sydney, NSW warehouse or from our UK or US warehouse, depending on stock availability.
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Librería: CitiRetail, Stevenage, Reino UnidoCitiRetail
Contactar con el vendedorVendedor de 5 estrellasCondición: Nuevo
EUR 23,52
Envío por EUR 43,35Se envía de Reino Unido a Estados Unidos de AmericaCantidad disponible: 1 disponibles
Paperback. Condición: new. Paperback. She needs to ditch her past. He needs to believe in his future. Caroline Santos is chasing a clean slate. After a scandal shatters her reputation, she escapes across the country to take a lifeguarding job in her old hometown. As she settles in, she earns the respect of her coworkers and puts… a toe in the water of forming new friendships. But she keeps her defenses up, unwilling to trust too deeply-especially with the handsome but annoying fellow lieutenant she can't quite read.and who doesn't seem to like her much either. Is the key to rebuilding her sense of community, safety, and happiness getting him on her side-or is he a threat she can't risk?Jason Lowe has always loved the job. With the Cape May Beach Patrol, he thrives on the ocean, the responsibility, and the physical demands of guarding. Still, he struggles to see himself as a true leader, weighed down by his family's belief that lifeguarding isn't a "real" career. So, when Caroline arrives-confident, unapologetically proud, and razor-sharp-he's intrigued, but every attempt to connect with her seems to backfire.As the team works, trains, and competes together, Jason catches glimpses of the woman beneath the tough exterior, and her opinions start to reshape how he views himself. For Caroline, the past constantly threatens the progress she's trying to make. To truly move forward, she'll have to learn to trust-and risk opening her heart again-or watch all she's worked for slip away. Caroline needs to ditch her past. Jason needs to believe in his future. In this enemies-to-lovers romance, these two lifeguards compete as they work and learn to trust themselves and what they can be together. This item is printed on demand. Shipping may be from our UK warehouse or from our Australian or US warehouses, depending on stock availability.
- Tapa blanda
- Impresión bajo demanda
Librería: CitiRetail, Stevenage, Reino UnidoCitiRetail
Contactar con el vendedorVendedor de 5 estrellasCondición: Nuevo
EUR 30,76
Envío por EUR 43,35Se envía de Reino Unido a Estados Unidos de AmericaCantidad disponible: 1 disponibles
Paperback. Condición: new. Paperback. She's writing the next chapter of her life story one decision at a time.and overthinking all of them. Lucy Torres is stuck. Don't misunderstand-she loves her friends, her town, her work; she even loves having her mom as her roomie. Life is comfortable. Predictable. Safe. But now her mom want…s to downsize to a condo of her own, and Lucy has to face that her "temporary" living situation has lasted a little too long. It's time for change. The trouble is, Lucy's been waiting. For the spark her grandmother swore would come in her twenty-sixth year-this year-the magic that would point her toward what's supposed to come next in her life. Lucy wants to move forward, but only with purpose. She wants direction. A nudge from the universe. Some sort of a sign, but she hasn't yet seen one. So when a charming newcomer sweeps her off her feet, Lucy dares to believe the moment has arrived. Maybe this is the sign she's been holding out for. But the more she chases a different life, the harder it gets, and she risks overlooking the quiet truth that's been unfolding around her all along. In the end, Lucy will have to dig deep and decide what is worth trusting: magic that dazzles, or love that lasts. This item is printed on demand. Shipping may be from our UK warehouse or from our Australian or US warehouses, depending on stock availability.
