Report, Band 12Johns Hopkins Press, 1928 CONTENTS.--Vol. I (1897)--Vol. II (1898)--Vol. III (1899)--Vol. IV (1902)--Vol. V (1905)--Vol. VI (1906)--Vol. VII (1908)--Vol. VIII (1909)--Vol. IX (1911)--Vol. X (1918)--Vol. XI (1922)--Vol. XII (1928)--Vol. XIII (1937)--Vol. XIV (1941) |
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Seite 20
... olivine to serpentine .. The alteration of amphibole to serpentine .. The alteration of pyroxene to serpentine ... Rocks from which serpentine is derived .. Serpentinization .... Page 243 243 244 245 246 246 247 248 248 249 Physical ...
... olivine to serpentine .. The alteration of amphibole to serpentine .. The alteration of pyroxene to serpentine ... Rocks from which serpentine is derived .. Serpentinization .... Page 243 243 244 245 246 246 247 248 248 249 Physical ...
Seite 24
... olivine , 2. amphibole , and 3. pyroxene respectively ...... 247 9. Figure showing central cleavage lines of serpentine surrounded by magnesite ...... 275 PREFACE The present volume is the twelfth in the series 24 ILLUSTRATIONS.
... olivine , 2. amphibole , and 3. pyroxene respectively ...... 247 9. Figure showing central cleavage lines of serpentine surrounded by magnesite ...... 275 PREFACE The present volume is the twelfth in the series 24 ILLUSTRATIONS.
Seite 201
... olivine and pyroxene , with more or less magnetite ; the pyroxenite , of bronzite and diallage . Both of these rocks are generally much altered . The pyroxene , when it occurs alone , passes into secondary hornblende , and this in turn ...
... olivine and pyroxene , with more or less magnetite ; the pyroxenite , of bronzite and diallage . Both of these rocks are generally much altered . The pyroxene , when it occurs alone , passes into secondary hornblende , and this in turn ...
Seite 204
... olivine fragments and that there is evidence that it was derived from stratified rocks since the strikes and dips are approximately parallel to the neighboring gneiss which the serpentine overlies . The limestones occurring near this ...
... olivine fragments and that there is evidence that it was derived from stratified rocks since the strikes and dips are approximately parallel to the neighboring gneiss which the serpentine overlies . The limestones occurring near this ...
Seite 208
... olivine and not from a dolomite or an enstatite rock . The dark - green crystals which are often twinned , are speudomorphs after olivine . This serpentine lies wholly within the mica - schists southeast of the pre- cambrian gneiss . In ...
... olivine and not from a dolomite or an enstatite rock . The dark - green crystals which are often twinned , are speudomorphs after olivine . This serpentine lies wholly within the mica - schists southeast of the pre- cambrian gneiss . In ...
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Häufige Begriffe und Wortgruppen
30 feet Albany sand altered arbitrators award Baltimore County Baltimore gneiss BOND AND PERMEABILITY boundary line buddle Cecil County chlorite chromite Clay class Clay Sub cleavage Coarseness figure color commissioners compact Company Creek crystals deposits diabase diallage Dye Adsorption figure east epi-diorite farm feet deep feet long feet wide feldspar feldspar quarries fibrous FINENESS TEST flint formation gabbro Geol gneiss grade Grain class Grain fineness granite green Harford County hauled hill hornblende hypersthene hypersthene gabbro intrusive limestone located magnetite Marriottsville Maryland and Virginia masses material metamorphism mica mica schist microscope mile southeast mill mineral molding sand northeast occurs olivine opening outcrop pegmatite Pennsylvania peridotites PERMEABILITY TESTS pits plagioclase potash Potomac River pottery production pyroxene pyroxenites quarry Plate VII quartz railroad region road rock sample sand chrome schist schistose serpentine serpentine areas shows soapstone specimens Survey talc tremolite veins Virginia and Maryland width
Beliebte Passagen
Seite 36 - And be it enacted, That this Act shall take effect from the date of its passage.
Seite 36 - That the sum of four thousand and six hundred dollars be, and the same is hereby, appropriated, to be paid out of any money in the Treasury not otherwise appropriated...
Seite 24 - The citizens of each state respectively shall have full property in the shores of Potomack river adjoining their lands, with all emoluments and advantages thereunto belonging, and the privilege of making and carrying out wharves and other improvements, so as not to obstruct or injure the navigation of the river...
Seite 273 - A light-green chloritic rock somewhat schistose. Very soft and easily crushed by the hammer. There are some dark stains between the layers. Under the microscope the rock is seen to be made up of chlorite and actinolite. Cf . 69B. There is much magnetite in crystals, in beautiful cubes and octahedrons. There is a little quartz. The chlorite is green and pleochroic in slightly pleochroic blades with cross gashes. Extinction inclined.
Seite 33 - States, the Governor of this State be, and he is hereby authorized and empowered to appoint a...
Seite 17 - Beginning at the point on the Potomac River where the line between Virginia and West Virginia strikes the said river at low-water mark, and thence following the meanderings of said river by the low-water mark to Smith's Point, at or near the mouth of the Potomac, in the latitude 37° 53' 8
Seite 17 - Survey, we have come as near) to perfect mathematical accuracy as in the nature of things is possible. But in case of any inaccuracy in the described course or length of a line or in the latitude or longitude of a place the natural objects called for must govern.
Seite 18 - Virginia is entitled not only to full dominion over the soil to low-water mark on the south shore of the Potomae, but has a right to such use of the river beyond the line of low-water mark as may be necessary to the full enjoyment of her riparian ownership...
Seite 173 - ... 2.55 The ore minerals have the same appearance in Sample IV as in the others and they are made up either of a spinel molecule in which Cr2O3 has given way almost completely to A12O3 and Fe2O3 or a mixture of a spinel in which Cr2O3 has given way to much A12O3 with considerable magnetite. The percentage of titanium also indicates a higher percentage of ilmenite. In order to get a clearer idea of the nature of the ore particles in these concentrates and particularly in the case of the two samples...