Librería: GreatBookPrices, Columbia, MD, Estados Unidos de America
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Librería: GreatBookPrices, Columbia, MD, Estados Unidos de America
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Añadir al carritoCondición: As New. Unread book in perfect condition.
Librería: art4us - Antiquariat, Bonn, Alemania
Original o primera edición
EUR 12,00
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Añadir al carritoOPp. Condición: Gut. 47 S., m. vornehml. ganzs. farb. Abb. wie neu K-05-34 9789081478816 Aufgrund der EPR-Regelung kann zur Zeit in folgende Länder KEIN Versand mehr erfolgen: Bulgarien, Griechenland, Luxemburg, Österreich, Polen, Rumänien, Schweden, Slowakei. Bitte beachten Sie: Auf Grund der vorgegebenen Versandkosten von AbeBooks / ZVAB kann es bei Büchern über 1 kg oder bei mehrbändigen Werken zu höheren Versandkosten kommen. Please note: Due to the shipping costs specified by AbeBooks / ZVAB, there may be higher shipping costs for books over 1 kg or for multi-volume works. Sprache: Niederländisch Gewicht in Gramm: 550.
Librería: Mooney's bookstore, Den Helder, Holanda
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Añadir al carritoCondición: New. Van De Beek, Mariëlla Ilustrador.
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Añadir al carritoCondición: New.
Librería: Mooney's bookstore, Den Helder, Holanda
EUR 16,47
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Añadir al carritoCondición: Very good. Van De Beek, Mariëlla Ilustrador.
EUR 26,65
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Añadir al carritoCondición: Very good.
Idioma: Alemán
Publicado por Herder GmbH u. Co. KG, Verlag, 2001
ISBN 10: 3451703645 ISBN 13: 9783451703645
Librería: Antiquariat ARS LIBRI, Andreas Lutz, Windeck, Alemania
EUR 6,80
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Añadir al carritoBilderbuch. Freiburg, Herder 2008. Ca. 20 Seiten m. zahlreichen Illustrationen. Orig. Hardcover, 4°. Sehr gut erhalten.
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Librería: Universitätsbuchhandlung Herta Hold GmbH, Berlin, Alemania
EUR 66,00
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Añadir al carrito1. Aufl. 21 x 28 cm. Hardcover. Versand aus Deutschland / We dispatch from Germany via Air Mail. Einband bestoßen, daher Mängelexemplar gestempelt, sonst sehr guter Zustand. Imperfect copy due to slightly bumped cover, apart from this in very good condition. Stamped. Sprache: Englisch.
Librería: Goodwill of Silicon Valley, SAN JOSE, CA, Estados Unidos de America
EUR 99,99
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Añadir al carritoCondición: good. Supports Goodwill of Silicon Valley job training programs. The cover and pages are in Good condition! Any other included accessories are also in Good condition showing use. Use can include some highlighting and writing, page and cover creases as well as other types visible wear.
Librería: McCord Books, NORWALK, IA, Estados Unidos de America
EUR 108,04
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Añadir al carritopaperback. Condición: Good. Light cover wear, text is unmarked.
EUR 45,53
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Añadir al carritoCondición: Very good.
EUR 131,50
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Añadir al carritoCondición: New. pp. 296 Index.
EUR 136,32
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Añadir al carritoCondición: New. pp. 296 Illus.
Librería: Ria Christie Collections, Uxbridge, Reino Unido
EUR 166,94
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Añadir al carritoCondición: New. In.
Librería: GreatBookPricesUK, Woodford Green, Reino Unido
EUR 166,92
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Añadir al carritoCondición: New.
Librería: GreatBookPrices, Columbia, MD, Estados Unidos de America
EUR 184,45
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Librería: GreatBookPricesUK, Woodford Green, Reino Unido
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Librería: Romtrade Corp., STERLING HEIGHTS, MI, Estados Unidos de America
EUR 188,96
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Añadir al carritoCondición: New. This is a Brand-new US Edition. This Item may be shipped from US or any other country as we have multiple locations worldwide.
Librería: GreatBookPrices, Columbia, MD, Estados Unidos de America
EUR 191,65
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Añadir al carritoCondición: New.
Librería: Ria Christie Collections, Uxbridge, Reino Unido
EUR 191,74
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Añadir al carritoCondición: New. In.
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Añadir al carritoCondición: New.
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Añadir al carritoCondición: New.
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Añadir al carritoCondición: New. 656.
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Añadir al carritoCondición: New. 656.
Librería: Rarewaves.com USA, London, LONDO, Reino Unido
EUR 234,82
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Añadir al carritoPaperback. Condición: New. 1st ed. Softcover of orig. ed. 2008. This chapter describes the processes involved in the transport of material over hillslopes. Hillslopes provide the gradients enabling material to be transported from the slopes themselves towards the valley bottoms, directly by gravity alone, or by water flowing down over the surface. Gravity has the potential to transfer material downslope if the material resistance to counteact it is insufficient. Similarly, water and wind flowing along the surface exert a drag on soil particles and have the potential to entrain material. After the gradient has fallen below a critical threshold to keep the material in tra- port, deposition occurs. Conventionally, slope processes in which gravity alone is the dominant transporting agent are called mass movements (Brunsden 1984). Processes in which other agents dominate are called erosion, e.g. wind or water erosion. Flowing water is an important transporting agent on which the emphasis is placed here. Although mass wasting is a natural process its incidence and impact may be exacerbated by human activities (Crozier 1986; Morgan 2005). A situation may ultimately arise in which human interests become unsafe or unsustainable. This impact is not only directly felt in the areas where material is removed or deposited and indirectly mass wasting may have an effect on soil and water quality in areas located further downstream. In the following sections a brief overview is given of the mechanisms, morphology, causes and consequences of mass movements and erosion.
EUR 180,97
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Añadir al carritoGebunden. Condición: New. New scientific research and practical advice in the field of slope stability and erosion controlA holistic approach to the revegetation of degraded slopesInteraction between substrate movement and vegetation discussed by geotechnical engine.
Idioma: Inglés
Publicado por Springer Netherlands, Springer, 2010
ISBN 10: 9048176964 ISBN 13: 9789048176960
Librería: AHA-BUCH GmbH, Einbeck, Alemania
EUR 168,73
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Añadir al carritoTaschenbuch. Condición: Neu. Druck auf Anfrage Neuware - Printed after ordering - This chapter describes the processes involved in the transport of material over hillslopes. Hillslopes provide the gradients enabling material to be transported from the slopes themselves towards the valley bottoms, directly by gravity alone, or by water flowing down over the surface. Gravity has the potential to transfer material downslope if the material resistance to counteact it is insufficient. Similarly, water and wind flowing along the surface exert a drag on soil particles and have the potential to entrain material. After the gradient has fallen below a critical threshold to keep the material in tra- port, deposition occurs. Conventionally, slope processes in which gravity alone is the dominant transporting agent are called mass movements (Brunsden 1984). Processes in which other agents dominate are called erosion, e.g. wind or water erosion. Flowing water is an important transporting agent on which the emphasis is placed here. Although mass wasting is a natural process its incidence and impact may be exacerbated by human activities (Crozier 1986; Morgan 2005). A situation may ultimately arise in which human interests become unsafe or unsustainable. This impact is not only directly felt in the areas where material is removed or deposited and indirectly mass wasting may have an effect on soil and water quality in areas located further downstream. In the following sections a brief overview is given of the mechanisms, morphology, causes and consequences of mass movements and erosion.
Librería: AHA-BUCH GmbH, Einbeck, Alemania
EUR 168,73
Cantidad disponible: 2 disponibles
Añadir al carritoBuch. Condición: Neu. Druck auf Anfrage Neuware - Printed after ordering - This chapter describes the processes involved in the transport of material over hillslopes. Hillslopes provide the gradients enabling material to be transported from the slopes themselves towards the valley bottoms, directly by gravity alone, or by water flowing down over the surface. Gravity has the potential to transfer material downslope if the material resistance to counteact it is insufficient. Similarly, water and wind flowing along the surface exert a drag on soil particles and have the potential to entrain material. After the gradient has fallen below a critical threshold to keep the material in tra- port, deposition occurs. Conventionally, slope processes in which gravity alone is the dominant transporting agent are called mass movements (Brunsden 1984). Processes in which other agents dominate are called erosion, e.g. wind or water erosion. Flowing water is an important transporting agent on which the emphasis is placed here. Although mass wasting is a natural process its incidence and impact may be exacerbated by human activities (Crozier 1986; Morgan 2005). A situation may ultimately arise in which human interests become unsafe or unsustainable. This impact is not only directly felt in the areas where material is removed or deposited and indirectly mass wasting may have an effect on soil and water quality in areas located further downstream. In the following sections a brief overview is given of the mechanisms, morphology, causes and consequences of mass movements and erosion.