By Professor Dr. Robert Young, Dr. Ann Young (auth.)

As only a few reviews on geomorphological elements of sandstones exist, this e-book demonstrates the importance of landforming procedures from geological, geochemical and dynamic issues of view. the global examples contain vintage components of sandstone study equivalent to the Colorado Plateau, Saxony, France and England, but additionally emphasize the sandstone lands of the southern hemisphere. The authors supply proof for climatic impacts on sandstone landforms, bearing in mind geochemical weathering approaches and targeted comparative reports, and a brand new type in accordance with structural and tectonic settings is printed. This entire examine, together with smooth options, could be urged not just to geomorphologists but in addition to sedimentologists and hydrologists.

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There is a marked change in morphology in the southern part, where the steep slopes below the cliffs are replaced by an uninterrupted chain of landslide deposits. These deposits, which form a belt up to 3 km wide, consist of individual rotational failures more than 1 km long, over 100 m high, and about 200 m wide at the base. The failures have occurred in the thick red clays of the Tilemsin Formation, but each of them has incorporated a section of the overlying Nubian Sandstone which now lies as a broken, inclined capping on the slumped mass.

6) is also widely used (Wylie 1980). The simple trigonometrical relationships expressed in the limiting equation for toppling shows clearly why the high and very slender towers carved from sandstones remain stable unless undercut at the base. The Old Man of Hoy, a 137 m high sea stack cut from the Old Red Sandstone of the Orkneys, is a case in point. Although its height exceeds its width by a factor of about six or seven, this stack would not topple until inclined to about 10° from the horizontal.

However he attributes the development of slickrock slopes from steep cliffs primarily to slab failure above "effective" partings in the bedding, that is above partings that are the sites of undercutting. These partings consist either of closely spaced bedding with highly fractured sandstone, or fissile shales. Below the partings are slickrock slopes which extend at the foot of the retreating cliffs. Oberlander presents convincing evidence of the control of changes in the position of the break in slope by variations in the dip of the effective partings or by their pinching out (Fig.

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