Physical Sciences and Mathematics Commons^™

Relationships Oct-Nov 1965 Observation Well Measurements To Median Observed Ground Water Levels, E. C. Reed

Conservation and Survey Division

No abstract provided.

Dünya Enerji̇ İhti̇yaçlarinin Karşilanmasinda Atom Gücünün Rolü, Muammer Çeti̇nçeli̇k

Bulletin of the Mineral Research and Exploration

No abstract provided.

Satişi Üni̇te İle Yapilan Bazi Madenleri̇n İkti̇sadi̇li̇ği̇ Hakkinda Prati̇k Metod, Hüsnü Kale

Bulletin of the Mineral Research and Exploration

No abstract provided.

Die Braunkohlen Von Tozakli - Poyrali Und Die Geologie Der Umgebung Von Pinarhi̇sar, Mustafa Aslaner

Bulletin of the Mineral Research and Exploration

No abstract provided.

Geologie Der Phosphatführenden Schichtfolge Des Raumes Mardi̇n- Deri̇k –Mazidaği, Hans Beer

Bulletin of the Mineral Research and Exploration

No abstract provided.

The Pliocene And Quaternary Volganism In The Hasan Dağ-Melendi̇z Dağ Region, P. H. Beekman

Bulletin of the Mineral Research and Exploration

No abstract provided.

Cambrian Outcrops In Southeastern Turkey And Their Comparison With The Cambrian Of East Iran, İhsan Keti̇n

Bulletin of the Mineral Research and Exploration

No abstract provided.

Geology Of Eastern And Southeastern Anatolia, İ. Enver Altinli

Bulletin of the Mineral Research and Exploration

No abstract provided.

Chemical Staining Methods Used In The Identification Of Carbonate Minerals, Tamer Ayan

Bulletin of the Mineral Research and Exploration

No abstract provided.

Paléomagnétisme Du Permien D'Amasra (Anatolie Du Nord), C. B. Gregor, J. D. A. Zijderveld

Bulletin of the Mineral Research and Exploration

No abstract provided.

Geology Of Tunceli̇ - Bi̇ngöl Region Of Eastern Turkey, F. A. Afshar

Bulletin of the Mineral Research and Exploration

No abstract provided.

Observations Sur La Géologie Du Taurus Au Nord D'Alanya (Turquie), Philippe De Peyronnet

Bulletin of the Mineral Research and Exploration

No abstract provided.

Über Die Geologie Der Umgebung Nördlich Der Linie Aydin - Nazi̇lli̇, Mehmet Akartuna

Bulletin of the Mineral Research and Exploration

No abstract provided.

Avrupa'da Tabi̇i̇ Gaz İsti̇hsali̇ni̇n Bugünkü Durumu Hakkinda, Muammer Çeti̇nçeli̇k

Bulletin of the Mineral Research and Exploration

No abstract provided.

Geology Of Mianeh District Of Northwestern Iran, F. A. Afshar

Bulletin of the Mineral Research and Exploration

No abstract provided.

The Geology Of Ahlat-Adi̇lcevaz Area (North Of Lake Van), Erdoğan Demi̇rtaşli, Carlo Pisoni

Bulletin of the Mineral Research and Exploration

No abstract provided.

Precisions Sur Le Metamorphisme Du Massif De Menderes Le Long De Sa Bordure Meridionale (Sw De La Turquie), P. De Gragiansky

Bulletin of the Mineral Research and Exploration

No abstract provided.

Note Preliminaire Sur Le Silurien D'İstanbul, Fuat Baykal, Orhan Kaya

Bulletin of the Mineral Research and Exploration

No abstract provided.

Geology Of The Monte Cristo Area, Bear River Range, Utah, Robert B. Smith

All Graduate Theses and Dissertations, Spring 1920 to Summer 2023

The Monte Cristo area is a 7 1/2-minute quadrangle located in the southeastern. part of the Bear River Range, northern Utah. It is within the Middle Rocky Mountain province and is 10 miles east of the Basin and Range province. Previous to this investigation little was known about the detailed geology of the area except for a reconnaissance study and general geologic map of the Cache County part included in the Geologic Atlas of Utah, Cache County, published by Williams (1958).

The purposes of this investigation were as follows: (1) to determine the formations present in the area and their …

Paleozic Stratigraphy Of The James Peak Quadrangle, Utah, Harley D. King

All Graduate Theses and Dissertations, Spring 1920 to Summer 2023

General Statement

The James Peak quadrangle is a topographic map unit of the Geological Survey of the U. S. Department of Interior (Plate 1). It covers 7 1/2 minutes of latitude and longitude at a scale of 1:24, 000 or 1 inch to 2, 000 feet. It is bounded by lat 41°22'30" N. and lat 41°30' N. and long 111°45' W. and long 111 °52 '30" W The quadrangle includes 56 square miles and has maximum relief of about 4, 300 feet.

The James Peak quadrangle is located in northern Utah between the Wasatch Range on the west and the …

Fusulinids From The Cyathophyllum Limestone, Central Vestspitsbergen, Charles A. Ross

Geology Faculty Publications

Thirteen species of fusulinids are illustrated and described from eleven collections within the Cyathophyllum Limestone of central Vestspitsbergen. The lower collections at Tempelfjorden and the collection from Mount Lykta contain Schubertella transitoria, Triticites arcticus, and Schwageriiia anderssoni and other species typical of the Carboniferous zones C₃C through C₃E of the Ural region of the U.S.S.R. It is suggested that “Fusulinella" usvae is a species of Waeringella. Higher collections at Tempelfjorden include Parafusulina furnishi n. sp. and Pseudofusulinella tempelensis n. sp. and a loose block from higher in the succession includes Schwagerina …

Water Levels In Observation Wells In Nebraska, 1964, Philip A. Emery, Mildred M. Malhoit

Conservation and Survey Division

No abstract provided.

A Detailed Economic Investigation Of Geochemical And Aeromagnetic Anomalies North Central Maine, W. F. Stickney, R. S. Young, L. A. Wing

Maine Collection

A Detailed Economic Investigation of Geochemical and Aeromagnetic Anomalies North Central Maine

W.F.Stickney, R.S.Young and L.A.Wing

Special Economic Series No.4, Maine Geological Survey, Department of Economic Development, Augusta, Maine (March 1965).

Contents: Foreword / Part I - Geology (W.F. Stickney) / Part II - Geophysics (R.S. Young) / Part III - Geochemistry (L.A. Wing) / References

Possible Late Pleistocene Uplift, Chesapeake Bay Entrance, W. Harrison, Rj Malloy, Ga Rusnak, J Terasmae

VIMS Articles

Paleontological and lithological studies of engineering borings and boring logs subaerial erosion surface of Pliocene (?)-Pleistocene age cuts across clastic sediments of pre-Yorktownian Miocene age in the subsurface and subbottom of the lower Chesapeake Bay area. When the bore-hole data are coupled with the results of subbottom echo profiling and piledriving records, it is possible to construct accurate cross sections of the buried Miocene-Pleistocene contact. The cross sections show "lows" in the erosion surface that may be correlated with the buried channels of the Pleistocene Elizabeth, James, York, and Susquehanna river valleys. Probable channel depths below mean low water at …

Monadnocks, Divides And Ozark Physiography, James Harrison Quinn

Journal of the Arkansas Academy of Science

No abstract provided.

Report On Some Iron And Nickel Minerals From The Soapstone Deposits Of Saline County, Arkansas, Phillip Wicklein, Alden B. Carpenter

Journal of the Arkansas Academy of Science

No abstract provided.

Precambrian Geology In Humboldt Township, Marquette County, Michigan, Peter D. Rowley

Journal of the Minnesota Academy of Science

ABSTRACT-The present study involved investigation of gneissic granite, migmatite, basic dikes, and faults in part of the Southern Complex of Michig.an. The average strike of the foliation of the gneissic granite based upon the orientation of feldspar phenocrysts is N. 60° w·;, the strike of the major dike set is between N. 30° W. and N. 60° W., the average strike of the fault zones-is N. 52° W., and a two-mile long body of migmatite trends about N. 57° W. The known history starts in the early Precambrian, when gneissic granite was emplaced and formed migmatites by incorporation of wall-rock …

Marine Geology, Preston E. Cloud Jr.

Journal of the Minnesota Academy of Science

Were the average temperature of the earth a few tens of degrees less than it is, ice would be the most common crustal rock. The fact that it occurs in its liquid phase over 71 per cent of the earth's surface should not obscure the fact that the oceans are geologic features, particularly in their substructure, their boundary relations, and their history.

Geology Of The Lamy-CañOncito Area, Santa Fe County, New Mexico, Robert S. Goolsby

Earth and Planetary Sciences ETDs

The area studied lies in the vicinity of Lamy and Canoncito in Santa Fe County, about 17 miles southeast of Santa Fe, New Mexico.

The rocks range in age from Precambrian through Quaternary, Precambrian rocks include dark schist and pink gneiss, with minor amounts of greenstone and quaritzite, Overlying the Precambrian rocks is a sequence of sandy limestone called the Basal Limestone, of Mississippian and possibly Devonian age. The Pennsylvanian System is represented by the Sandia formation and Madera Limestone, which are dominantly dark shale and fossiliferous limestone. The Sangre de Cristo and Yeso Formations, Glorieta Sandstone, San Andres Linestone, …

Geology Of The San Mateo Peak Area, Socorro County, New Mexico., James W. Furlow

Earth and Planetary Sciences ETDs

The San Mateo Mountains of south-central New Mexico consist of an uplifted block of Tertiary volcanics 20 miles wide by 4 miles ling. The San Mateo uplift is one of the bounding uplifts along the western side of the Rio Grande depression.

The basement rock as exposed just east of the San Mateos is a Precambrian granite; it is overlain in order by the Cambrian Bliss formation, the Ordovician Sierrite Limestone, Cable canyon sandstone, and Upham Dolomite, the Pennsylvanian Magdalena Group, and the Permian Abo Formation. These sedimentary rocks are unconformably overlain by Tertiary volcanic rocks of the Lower volcanic …