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- W75297310 abstract "This chapter describes the structure of hard rock. Rocks such as granite, basalt, and tuff contain natural fractures and systems of joints. Sedimentary rocks—such as sandstone and limestone—generally contain connected voids or pores, but comparatively few fractures and joints. Shales have both pores, but poorly connected, and fractures. This is also the case with tuff. In granite, the natural fractures and joints are the main conduits for water flow as the pores are usually small and not well connected. The welded tuff is formed when very hot solid particles from volcanic eruptions settle onto the surface and weld together. The chapter illustrates a figure in which the loadings of past geologic time have created faults, fractures, joints, and crushed zones in the rock. The joints are really regular systems of fracture planes with preferred directions in different areas. However, there has been no visible movement of one wall of the joint with respect to the other. The crushed zones are localized regions in the rock in which fractures and joints are highly abundant." @default.
- W75297310 created "2016-06-24" @default.
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- W75297310 date "1982-01-01" @default.
- W75297310 modified "2023-09-26" @default.
- W75297310 title "The Structure of Hard Rock" @default.
- W75297310 doi "https://doi.org/10.1016/b978-0-08-027608-3.50011-x" @default.
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