Bulletin of the United States Geological SurveyThe Survey., 1896 |
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Página 13
... exposures of this substructure of Louisiana , and excluding the overlying later deposits , it repre- sents a ridge with steep hillsides and occasional high peaks with almost perpendicu- lar declivities . The Exogyra costata and the ...
... exposures of this substructure of Louisiana , and excluding the overlying later deposits , it repre- sents a ridge with steep hillsides and occasional high peaks with almost perpendicu- lar declivities . The Exogyra costata and the ...
Página 24
... exposures at Chopin . Thence the line has been traced to the Sabine River by Hopkins . After crossing the Red River , Hopkins says : Reappearing in the Cloutierville and Kisatchie hills , it ranges almost due west to the " Bad Hill ...
... exposures at Chopin . Thence the line has been traced to the Sabine River by Hopkins . After crossing the Red River , Hopkins says : Reappearing in the Cloutierville and Kisatchie hills , it ranges almost due west to the " Bad Hill ...
Página 56
Geological Survey (U.S.). Missouri , and no clearly marked exposures east of that stream have been found south of this . High buttes are numerous about the mouth of Grand River . The Fox Hills lie between the Moreau and the Big Cheyenne ...
Geological Survey (U.S.). Missouri , and no clearly marked exposures east of that stream have been found south of this . High buttes are numerous about the mouth of Grand River . The Fox Hills lie between the Moreau and the Big Cheyenne ...
Página
... exposures of ...... 56-57 Chamberlin , T. C. , letter of transmittal by .. cited 9 Pre - Glacial drainage and topography , form 11 of 57-58 Cleveland , section west of ( figured ) 41 Redfield , deposits near ... 46 Crow Creek region ...
... exposures of ...... 56-57 Chamberlin , T. C. , letter of transmittal by .. cited 9 Pre - Glacial drainage and topography , form 11 of 57-58 Cleveland , section west of ( figured ) 41 Redfield , deposits near ... 46 Crow Creek region ...
Página 5
... Exposures in Trents Reach .. Exposures on Dutch Gap Canal Exposures above Dutch Gap The cobblestone bed near Dutch Gap Exposures at Deep Bottom on the James The artesian well at Fort Monroe .... Exposure at Chaffins Bluff . Exposure at ...
... Exposures in Trents Reach .. Exposures on Dutch Gap Canal Exposures above Dutch Gap The cobblestone bed near Dutch Gap Exposures at Deep Bottom on the James The artesian well at Fort Monroe .... Exposure at Chaffins Bluff . Exposure at ...
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Términos y frases comunes
acid apatite augite beds biotite bluff Bull California Cambrian Carboniferous chlorite Claiborne clay balls Coal cobbles color Contains plagioclase County Creek Cretaceous deposits Describes the occurrence Devonian dike Discusses east Eocene erosion exposures feldspar figs folio fossils Geology Glacial gneiss gold granite gravel gray groundmass H₂O Harris hills hornblende Iowa iron Jour K₂O Kansas kaolin Keyes L. G. Eakins Lake layers lignite limestone London magnetite masses material Matthew Merrill miles Miller and Gurley minerals Missouri moraine mottled Mountain Newberry occur olivine orthoclase Paleontology-Continued Paleozoic Paris plagioclase Pleistocene porcelain portion Potomac formation pottery pre-Cambrian Proc quartz quartzite record region Rept Rhyolite River rocks sand sandstone sandy clay Scudder Silurian SiO2 species stones strata Surv Tertiary TiO2 Trace Trans Turner U. S. Geol Ulrich Undet Valley W. F. Hillebrand Weed and Pirsson Whiteaves Whitfield Winchell and Schuchert
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Página 29 - Friedel ° indicates a means for determining the true weight of water lost by minerals behaving like the zeolites, even without collecting the water lost, namely, by driving out of the dehydrated and weighed mineral, under proper precautions, any air it may have absorbed in the process of drying and cooling, and collecting and measuring this air and thus finding its weight, which, added to the apparent loss, gives the true contents in water.
Página 22 - CRUSHING. For accurate analyses the use of steel power crushers and mortars is out of the question because of the danger of contamination by particles of metal and the impossibility of cleansing the roughened surfaces after they have been in use a short time. Extraction, by the aid of a magnet, of steel particles thus introduced into the powder is quite inadmissible, since the rocks themselves, almost without exception, contain magnetic minerals.
Página 61 - If, therefore, on evaporation of the filtrate, much iron is indicated, the gelatinization may well be due to olivine alone or in part, and then the quantitative relation of silica to iron plus magnesium should be ascertained. It must also be borne in mind that any other very soluble silicates present will be more or less affected, and that apatite is largely or wholly dissolved. It is possible that still more dilute nitric or perhaps some other acid may exert a slighter solvent action on olivine...
Página 20 - Survey was there to be found in the light of modern methods, a satisfactory exposition of the procedures to be followed or the precautions to be observed, especially in the search for some of the rarer constituents or those which, without being rare, have been of late years recognized as occurring persistently in small amounts. It was not the intention to .make the chapter on rock analysis in...
Página 28 - It had regained 1J per cent of its original weight, although the desiccator was tightly closed and the crucible covered, showing apparently a drying power superior to that of the acid. A specimen of tyrolite was found on one occasion to lose 10.34 per cent at 280°, and on another occasion 14.33 per cent.
Página 49 - ... as ZrO2. Certainty as to its identity can be had by again bringing it into solution, precipitating by ammonia, dissolving in hydrochloric acid, evaporating to a drop or two, and testing with turmeric paper or by a microchemical reaction. With the very smallest amounts no color can be obtained by this turmeric-paper test, which, however, responds readily to as little as 1 milligram of dioxide and with proper care for as small an amount as 0.3 milligram (Dr.