Titlebook: Geology and Water; An introduction to f Richard E. Chapman Book 1981 Martinus Nijhoff / Dr. W. Junk Publishers bv, The Hague 1981 Deformati

Carminative

Pore Water and Sliding,eology of the Alps, north-west Scotland, and Scandinavia was being unravelled, evidence emerged of lateral displacements of blocks many tens of kilometres long in the direction of movement. For example, Tornebohm (1896, p. 194) postulated movement of blocks at least 130 km long on Caledonian thrusts

ADAGE

Native and Transplanted Kidneys,xamine, in outcrop or in hand speciment, are dry. We are apt to forget that, at depths below only a few metres from the surface, almost all rocks in nature are saturated with water (exceptionally and locally, also oil or gas). Some of this water is important to us as a source of fresh water for drin

隱藏

aptitude

Crayon

Dirk-Jan F. Kamann,Peter Nijkampwater, streams, and occasionally by rain-water runoff during and after storms: perennial streams are fed by ground water, smaller streams, and occasional runoff: the source is a spring or a zone of seepage, and is the highest intersection of the ground surface with the water- table. Common causes of

aerobic

只有

Marion M?hle,Dorothea M. Hartmann that important deformation occurs in sedimentary basins while they are accumulating sediment on a subsiding sedimentary column — particularly in the terminal regressive sequence. The regressive sequence itself is due to a neighbouring orogeny outside the sedimentary basin: the creation of mountains

損壞

monologue

傻瓜

https://doi.org/10.1007/978-3-8349-9911-5We revert in conclusion to the central theme of this book — the movement of water in the subsurface. The principles we have developed and discussed can be applied to a range of geological problems either as qualitative or as semi-qualitative arguments. We take one of each for illustrative purposes.