Numerical modelling of natural rock formations to estimate stability using the example of a sandstone massif in Saxony / Numerische Modellierung natürlicher Felskomplexe zur Abschätzung der Standsicherheit am Beispiel des Wehltumkomplexes in der Sächsisch

2012 ◽  
Vol 5 (4) ◽  
pp. 379-388
Author(s):  
Martin Herbst ◽  
Heinz Konietzky
Eos ◽  
2011 ◽  
Vol 92 (38) ◽  
pp. 324-324
Author(s):  
Colin Schultz

1996 ◽  
Vol 15 (1) ◽  
pp. 3-24 ◽  
Author(s):  
Scott Montgomery

The first naturalistic drawings of geologic phenomena, particularly rock formations, are assumed by historians to have occurred early in the 19th century, when geology matured as a science. No less than three centuries earlier, however, the Netherlandish master, Jan Van Eyck, drew exposures of natural rock whose features are so remarkably accurate as to permit modern-day geologic analysis of their lithology, fossil content, sedimentary structures, and depositional environment. Van Eyck clearly studied, drew, and painted a specific outcrop "in the field," long before such practice had become common in art or science. As the first modern geologic "observer," Van Eyck greatly extended an existing tradition of naturalism with regard to organic phenomena (esp. plants, insects, human figures) fully into the realm of inorganic reality. In this, he far surpassed other scholar-artists, such as Leonardo da Vinci, who have been credited with similar achievements. Van Eyck's achievement proved exceptional. It was matched neither by later artists, scientists, or illustrators until the late 18th-early 19th century, when conventions in travel literature and landscape inspired new attention to the drawing of rock materials. The reasons for this historical gap have everything to do with the limitations of observation in early geological study, which show important parallels to those in art.


Author(s):  
John M. Wehrung ◽  
Richard J. Harniman

Water tables in aquifer regions of the southwest United States are dropping off at a rate which is greater than can be replaced by natural means. It is estimated that by 1985 wells will run dry in this region unless adequate artificial recharging can be accomplished. Recharging with surface water is limited by the plugging of permeable rock formations underground by clay particles and organic debris.A controlled study was initiated in which sand grains were used as the rock formation and water with known clay concentrations as the recharge media. The plugging mechanism was investigated by direct observation in the SEM of frozen hydrated sand samples from selected depths.


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