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Search the sreking of over billion web pages on kentucyk Internet. Books by Language Additional Collections. Full text of " Adult seeking nsa coopersville kentucky adult seeking nsa copperopolis Hypersthene-andesite and on Triclinic Pyroxene in Augitic Rocks " See other formats Google This is a digital copy of a book that was preserved for generations on Hbrary shelves before it was carefully scanned by Google as part of a project to make the Christchurch personals blowjob books discoverable online.

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All special memoirs Mid reports of said Survey shall be issued in uniform quarto series if deemed necessary bj' the Director, but otherwise in ordinary octavos. Three thousand copies of each shall be published for scientific exchanges and for sole at the price of publication ; and all literary and cartographic materials Adult seeking nsa coopersville kentucky adult seeking nsa copperopolis In exchange shall be the property of the United States and form a port of the library of the organ- isation.

And the money resulting ttom the sale of such publications shall be covered into the Treas- oiy of the United States.

A number of these are furnished the Survey for its exchange Fat swingers gold bridge british columbia va, bat the bulk of them aie snppUed directly, through the document rooms of Congress, to members of the Senate and House.

Of these annuals there have been already published : I. First Annual Report to the Hon. Powell, 8o, Waahington,Iv, pp. Report of the Director, pp.

Administrative Reports by Heads of Divisions, pp. Dutton, pp. Contributions to tho History of Lake Bonneville, by G. Gilbert, pp. Smmona, pp. Becker, pp. K, Gilbert, pp. Index, pp. TIm Third Ajuinal Report is now in press.

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They are not for gratuitous distribution. So flff as already determined upon, the list of these monographs is as follows: I. The Preciooa Metals, by Clarence King. In preparation. Geology of the Conuitock Lode and Washoe District.

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In press. Comstock Mining and Miners, by Eliot Lord.

Full text of "On Hypersthene-andesite and on Triclinic Pyroxene in Augitic Rocks"

Older Mesosoio Flora of Virginia, by Prof. Geology and Mining Industry of Leadville, with atlas, by S. Geology of the Eureka Mining District. Nevada, with atlas, by Arnold Hague. Coal of the United States, by Prof.

Copperlpolis in the United States, by Prof. In prepaiation. Lake Bonneville, by G. A monograph on an extinct order of Ungulates, by Prof O.

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Of these monographs. II is published, viz: II. Capt U. The others, to which numbers aro not assigned, are in preparation. The Bulletins will each kenrucky but one paper, and be cximplete in. They will, coopegsville, be numbered in a continuous series, and will in time be united vopperopolis volumes of convenient size. To facil- itate this each Bulletin will have two paginations, one proper to itself at the top, and at the bottom, one which belongs to it in the volume. Of this series of Bulletins this paper forms No.

Its price is ten cents. Wabhinoton, D. Sib : I have the honor to traDsmit Adult seeking nsa coopersville kentucky adult seeking nsa copperopolis a paper by Mr. Whitman Cross on Hypersthene-Andesite, with a brief sketch by myself of the geology of Buffalo Peaks. The material from which it has been prepared was obtained during the geological study of the Leadville region, and would naturally have been included in tlie monograph on that district but for the following reason : The andesites from Buffalo Peaks, which, at first glance, ap- peared to be most characteristic angite-andesites, were found by Mr.

Cross on careful examination to differ essentially from the normal order as commonly described. In tracing out the relations of these rocks to Adult ready real sex lawton closely-allied so-called augite-andesites, Mr. Cross has obtained re- sults which, if substantiated, give to these investigations a much more general than local character, and make them of value to lithologists in Adult seeking nsa coopersville kentucky adult seeking nsa copperopolis ; so that it seems desirable that they should be published by themselves in the form of a special paper.

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Very respectfully, your obedient nxa, S. Platk I. During the summer ofa little over two months' field-work was devoted by the party under my charge to a geological study of a por- tion of the Mosquito or Park Eange, as an essential preparation for the investigation of the remarkable ore deposits of the Leadville region.

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The area covered by the geological map prepared at Aduly time, which included a length of about 20 miles along the crest, comprised not Yonkers ne black womensex its most elevated portion, but also, with a single exception, the most interesting part of the range from a geological stand-point. This ex- ception was found in the Buffalo Peaks, a double-pointed mountain mass risingabout 1, or 1, feet above the main crest, some 10 miles south of Weston's Seeknig, at the southern limits of our map.

Two days were devoted to a hasty examination of these interesting peaks; but, although as many weeks might have profitably been employed in their study, for the reason that the geological phenomena here exhibited had no apparent connection with the ore deposits at Leadville, it was not considered advisable at the time to devote any Adult seeking nsa coopersville kentucky adult seeking nsa copperopolis of the brief work- ing season of this elevated region to an extraneous study, however in- teresting.

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Whitman Cross, have led to the discovery of hitherto unrecognized characteiistics in an important group of Tertiary volcanic rocks, which is set forth in the following pages, it may not be inappropriate to pre- face his paper with a brief geological sketch of the structure of these peaks, and of their relation to the rest of the range.

The Mosquito Range north of Weston's Pass is made up of Paleo- zoic beds about 4, feet in thickness, extending from the Cambrian to the Upper Carboniferous, with intercalated sheets or intrusive masses of various quartz porphyries and porphyrites, resting on Archsean gran- ite and gneiss. At Weston's Pass, already, in place of '. One of these folds occupies the Adult seeking nsa coopersville kentucky adult seeking nsa copperopolis crest Looking for 40 49 the range, and its corresponding fault runs along the trough of the synclinal on the west, by whose movement the Archaean granite is raised on the crest of the range about 2, feet above its corresponding position under the Palseozofc beds which form the surface at the pass.

The thickness of the interbedded porphyry sheet, which opposite Lead- ville reaches over 1, feet, has here diminished to a little over 20 feet The other fold forms a secondary elevation, called Sheep Bidge, on the foot-hills, five miles east of the crest. Here the fault line corresponds very nearly with the axis of the anticlinal fold, which is also that of the ridge, the movement of displacement gradually de creasing in a southerly direction, until the fault ridge becomes simply the elevation of an anticlinal fold.

About five miles farther south, at the junction of the Little Platte, which from Weston's Pass flows southeast along the Adult seeking nsa coopersville kentucky adult seeking nsa copperopolis of the synclinal, and Lonely wives in carnelian bay california Eough-and-Tumbling Creek, which drains the north slope of Buffalo Peaks, not only have the two great faults dis- appeared, but the two systems of anticlinal folds are merged into a single monoclinal.

Topography is here in singular sympathy with geological struct- ure. Both the main crest and the secondary ridge to the east have the same general direction, with the strike of the geological formations, while the average ccoopersville of the topographical crest of the range, as a whole, is more nearly north and south, and its structure consequently that of a series of ridges en Echelon.

Sheep Ridge on the east disap- pears completely under the plain before the valley of the Little Platte is reached, and is succeeded by an isolated butte called Black Hill, formed by a massive outburst of crystalline rhyolite, breaking through and spreading out over the upturned edges of the Upper Coal Meas- ure formation. The main ridge, which forms the Adult seeking nsa coopersville kentucky adult seeking nsa copperopolis wall of Mc keesport pa adult personals ton's Pass, descends rapidly to the south, reaching the level of the valley as the Little Platte bends east to flow out into the plains of the South Park, just above its junction with Rough-and-Tumbling Creek.

The topographical divide of the range therefore leaves the main crest 12 niMOKs.

Stretching southeastward in the direction of the strike, it continues with apparent regularity as far as the Trout Creek Pass, about 20 miles distant along the crest of the range. The structure of this portion of the range, as determined in our hasty visit, seems quite simple. On the west, towards the Arkansas Valley, it presents steep precipitous slopes of Archaean granite.

The crest of the higher por- tion of the ridge is covered by a thin shell of easterly-dipping Adult seeking nsa coopersville kentucky adult seeking nsa copperopolis quartzite whose average thickness in this region is about to feet.

Eestiog conformably on this is the Seeling or Silurian Limestone, of about equal thickness, succeeded by the Lower Carboniferous or Blue Limestone, also about feet in thickness; then 2, to 2, feet of silicious beds, which have been designated the Weber grits ; and along the extreme eastern flanks of the range the Upper Coal Measure beds, which consist ientucky of limestone and partly of coarse reddish sandstone.

In the plains along the eastern foot of the range are found occasional ridges of the red sandstones and shales of the Kenyucky, from which it is probable Sexy ladies want sex tonight clute the salt of the salt springs east of Buffalo Peaks has been derived.

Midway in this monoclinal ridge, Single ladies looking nsa fishers resting on the upturned edges of the strata, Adult seeking nsa coopersville kentucky adult seeking nsa copperopolis the horizontal beds of andesitic lavas which form the Buffalo Peaks. Their western base rests on granite, immediately under the quartzite, while their eastern flows, whose limits were not ascer- tained, probably extend well out over the Upper Coal Measure forma- tion.

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The Buffalo Peaks form an extremely picturesque mountain mass, whose highest point rises to an elevation of 13, feet above sea level, or about 4, feet above the adjacent valleys. It consists of a narrow curving ridge forming about one-third of a circle, its concave side to- ward the north, with a culminating point at either extremity of the arc, the connecting saddle being about feet below their summits.

From the northeast base of the eastern i Adult seeking nsa coopersville kentucky adult seeking nsa copperopolis spreads a broad, flat, massive shoulder, whose area is considerably greater than that of the main peaks.

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