The Rift in the Rock. A Tale PDF Download
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Author: Mrs. S. C. Hall
Publisher:
ISBN:
Category :
Languages : en
Pages :
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Author: Mrs. S. C. Hall
Publisher:
ISBN:
Category :
Languages : en
Pages :
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Book Description
Author: Mrs. S. C. Hall
Publisher:
ISBN:
Category :
Languages : en
Pages : 180
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Author: Mrs. S. C. Hall
Publisher:
ISBN:
Category :
Languages : en
Pages : 96
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Author: Edgar La Verne Vincent
Publisher:
ISBN:
Category :
Languages : en
Pages : 218
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Author: Walter Jon Williams
Publisher: Walter Jon Williams
ISBN: 0988901749
Category : Fiction
Languages : en
Pages : 1048
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"The Rift would be a very good beach book, if you could put it down long enough to get into the water." —— The San Diego Union Tribune FRACTURE LINES PERMEATE THE CENTRAL UNITED STATES. Some comprise the New Madrid fault, the most dangerous earthquake zone in the world. Other fracture lines are social—— economic, religious, racial, and ethnic. What happens when they all crack at once? Caught in the disaster as cities burn and bridges tumble, young Jason Adams finds himself adrift on the Mississippi with African-American engineer Nick Ruford. A modern-day Huck and Jim, they spin helplessly down the river and into the widening faults in American society, encountering violence and hope, compassion and despair, and the primal wilderness that threatens to engulf not only them, but all they love... " A breakout book that you'll swear the author lived" —— SF Age "I don't like disaster novels. I would not have even glanced at The Rift if it weren't backed by Walter Jon Williams' reputation for excellence. And I definitely would not have kept reading if Williams hadn't demonstrated on every page that he deserves his reputation. The result? I was so engrossed in—— and engaged by ——The Rift that I forgot that I don't like disaster novels. This book is an impressive achievement.” —— Stephen R. Donaldson, New York Times bestselling author of The Chronicles of Thomas Covenant "The Rift is bloody wonderful! Williams brings an historic disaster back for an encore and metaphorically flattens it again. This is the stuff for which sleep is lost--and awards are made." —— Dean Ing "The Rift shakes up the world like it's never been shaken before." —— Fred Saberhagen "[For fans of the disaster novel] Williams delivers the requisite thrills and setpieces—— but he also, to paraphrase Conrad, offers a bit of that truth for which they forgot to ask." —— Locus
Author: Edgar L. (Edgar La Verne) 1851 Vincent
Publisher:
ISBN: 9781371804466
Category : History
Languages : en
Pages : 230
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Author: Edgar L. Vincent
Publisher: Forgotten Books
ISBN: 9780483417076
Category : Poetry
Languages : en
Pages : 228
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Book Description
Excerpt from In the Rift of the Rock Very little of beauty did the people see in the rock as they stood in its Shadow that day. Their only thought now was that they and their little ones were dying for lack of water. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
Author: United States. Census Office. 11th census, 1890
Publisher:
ISBN:
Category : Mineral industries
Languages : en
Pages : 1076
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Author: Daniel Harlov
Publisher: Springer Science & Business Media
ISBN: 3642283934
Category : Science
Languages : en
Pages : 804
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Book Description
Fluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to occur. Coupled with igneous and tectonic processes, metasomatism has played a major role in the formation of the Earth’s continental and oceanic crust and lithospheric mantle as well as in their evolution and subsequent stabilization. Metasomatic processes can include ore mineralization, metasomatically induced alteration of oceanic lithosphere, mass transport in and alteration of subducted oceanic crust and overlying mantle wedge, which has subsequent implications regarding mass transport, fluid flow, and volatile storage in the lithospheric mantle overall, as well as both regional and localized crustal metamorphism. Metasomatic alteration of accessory minerals such as zircon or monazite can allow for the dating of metasomatic events as well as give additional information regarding the chemistry of the fluids responsible. Lastly present day movement of fluids in both the lithospheric mantle and deep to mid crust can be observed utilizing geophysical resources such as electrical resistivity and seismic data. Such observations help to further clarify the picture of actual metasomatic processes as inferred from basic petrographic, mineralogical, and geochemical data. The goal of this volume is to bring together a diverse group of geologists, each of whose specialities and long range experience regarding one or more aspects of metasomatism during geologic processes, should allow them to contribute to a series of review chapters, which outline the basis of our current understanding of how metasomatism influences and helps to control both the evolution and stability of the crust and lithospheric mantle.
Author: John Gerrard
Publisher: Springer Science & Business Media
ISBN: 9401159831
Category : Science
Languages : en
Pages : 286
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Book Description
Geomorphology can be defined simply as the study of landforms. Landforms are the result of the interaction between what Ritter (1978) has called the driving and resisting forces. The driving forces or processes are the methods by which energy is exerted on earth materials and include both surface, geomorphological or exogenous processes and subsurface, geological or endogenous processes. The resisting forces are the surface materials with their inherent resistances determined by a complex combination of rock properties. Stated in these simple terms it would be expected that both sides of the equation be given equal weight in syntheses of landform evolution. However, this has not been the case. Until about the 1950s, geomorphology was mainly descriptive and concerned with producing time-dependent models of landscape evolution. Although the form of the land was the main focus, there was little detailed mention of process and scant attention to the properties of surface materials. There were, of course, exceptions. In the late 19th century G.K. Gilbert was stressing the equilibrium between landforms and processes. Many hydrologists were examining the detailed workings of river 'systems and drainage basins, culminating in the classic paper of Horton (1945).
