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New Mexico Lobo, Volume 060, No 19, 10/11/1956, University Of New Mexico Oct 1956

New Mexico Lobo, Volume 060, No 19, 10/11/1956, University Of New Mexico

1956

New Mexico Lobo, Volume 060, No 19, 10/11/1956


New Mexico Lobo, Volume 060, No 18, 10/9/1956, University Of New Mexico Oct 1956

New Mexico Lobo, Volume 060, No 18, 10/9/1956, University Of New Mexico

1956

New Mexico Lobo, Volume 060, No 18, 10/9/1956


University Of New Mexico Board Of Regents Minutes For September 08, 1956, University Of New Mexico Board Of Regents Sep 1956

University Of New Mexico Board Of Regents Minutes For September 08, 1956, University Of New Mexico Board Of Regents

Board of Regents Meeting Minutes

Minutes from the 1956-09-08 Board of Regents Meeting


New Mexico Lobo, Volume 060, No 7, 8/2/1956, University Of New Mexico Aug 1956

New Mexico Lobo, Volume 060, No 7, 8/2/1956, University Of New Mexico

1956

New Mexico Lobo, Volume 060, No 7, 8/2/1956


Faculty Senate Meeting Minutes Index, 1956-1957, Unm Faculty Senate Aug 1956

Faculty Senate Meeting Minutes Index, 1956-1957, Unm Faculty Senate

Faculty Senate Documents

No abstract provided.


New Mexico Lobo, Volume 060, No 6, 7/26/1956, University Of New Mexico Jul 1956

New Mexico Lobo, Volume 060, No 6, 7/26/1956, University Of New Mexico

1956

New Mexico Lobo, Volume 060, No 6, 7/26/1956


New Mexico Lobo, Volume 060, No 5, 7/19/1956, University Of New Mexico Jul 1956

New Mexico Lobo, Volume 060, No 5, 7/19/1956, University Of New Mexico

1956

New Mexico Lobo, Volume 060, No 5, 7/19/1956


New Mexico Lobo, Volume 060, No 4, 7/12/1956, University Of New Mexico Jul 1956

New Mexico Lobo, Volume 060, No 4, 7/12/1956, University Of New Mexico

1956

New Mexico Lobo, Volume 060, No 4, 7/12/1956


Annual Report Of The University, 1955-1956, University Of New Mexico Jun 1956

Annual Report Of The University, 1955-1956, University Of New Mexico

UNM Annual Reports

TO THE GOVERNOR OF NEW MEXICO: THE PRESIDENT OF THE UNIVERSITY has the honor to submit to you, through the Board of Regents, his report for the academic year, 1955-1956. No attempt has been made to cover the entire range of the University's activities; rather, certain significant highlights have been singled out for attention in an effort to give a general picture of development and progress. Our goal continues to be that of a university, outstanding in the quality of its faculty, representative in its student body, and able to carry its full share of responsibility in providing for the …


New Mexico Lobo, Volume 060, No 3, 6/28/1956, University Of New Mexico Jun 1956

New Mexico Lobo, Volume 060, No 3, 6/28/1956, University Of New Mexico

1956

New Mexico Lobo, Volume 060, No 3, 6/28/1956


University Of New Mexico Board Of Regents Minutes For June 06, 1956, University Of New Mexico Board Of Regents Jun 1956

University Of New Mexico Board Of Regents Minutes For June 06, 1956, University Of New Mexico Board Of Regents

Board of Regents Meeting Minutes

Minutes from the 1956-06-06 Board of Regents Meeting


Faculty Senate Meeting Minutes, 06/04/1956, P 361-386, Unm Faculty Senate Jun 1956

Faculty Senate Meeting Minutes, 06/04/1956, P 361-386, Unm Faculty Senate

Faculty Senate Meeting Minutes, 1920 - 2013

No abstract provided.


The Vertical Gradients Of Ozone Concentration And Its Relation To The Eddy Coefficient Of Diffusion, Joseph Levine May 1956

The Vertical Gradients Of Ozone Concentration And Its Relation To The Eddy Coefficient Of Diffusion, Joseph Levine

Physics & Astronomy ETDs

The purpose of this thesis is to apply this method to a tentative evaluation of the eddy coefficient of diffusion. Actually the investigation was more specifically an attempt to relate the difference in ozone concentration between the two stations to the average wind shear and to the vertical thermal stability.


An Experimental Investigation Of Computational Error In Complex Arithmetical Tasks, James L. Evans May 1956

An Experimental Investigation Of Computational Error In Complex Arithmetical Tasks, James L. Evans

Psychology ETDs

It was the purpose of this study (1) to investigate the nature of the computational errors made by mathematically trained college students when they solved complex arithmetical problems under normal conditions, i.e., comfortable working conditions without stress; and (2) to investigate experimental conditions which might reduce the incidence of computational error.


Geology And Ground-Water Resources Of The Portales Valley Area, Roosevelt And Curry Counties, New Mexico, Sherman E. Galloway May 1956

Geology And Ground-Water Resources Of The Portales Valley Area, Roosevelt And Curry Counties, New Mexico, Sherman E. Galloway

Earth and Planetary Sciences ETDs

Since 1910, and particularly since the closing years of World War II, considerable development of the ground water occurring in the valley fill has been made for irrigation purposes. This increase in development has resulted in a progressive decline of the water levels in this area. The results of this study indicate that the water occurring in the valley fill is the only water of good chemical quality occurring in the Portales Valley that can be obtained in quantities that are sufficient for normal irrigation, municipal, industrial, stock, and domestic uses, and that if the present rate of ground water …


Geology Of The Rinconada Canyon Area, Valencia County, New Mexico., John Mohar Jr. May 1956

Geology Of The Rinconada Canyon Area, Valencia County, New Mexico., John Mohar Jr.

Earth and Planetary Sciences ETDs

Within this area are found two small domes superimposed upon the McCarty syncline. North dome, the larger of the two, is located at the head of Rinconada Canyon. South dome is located in the southern part of the area near the mouth of the canyon. Thus far the mineral resources of the area have been of little economic value. There are, however, large deposits of commercial uranium deposit at depth which cannot be disregarded.


A Study Of Isotopic Exchange Between Potassium Iodide And Benzyl Iodide. Solvent Effects, Joseph A. Leary May 1956

A Study Of Isotopic Exchange Between Potassium Iodide And Benzyl Iodide. Solvent Effects, Joseph A. Leary

Chemistry and Chemical Biology ETDs

The kinetics of nucleophilic aliphatic substitution reactions has been studied by numerous investigators during the past fifteen years. Included in this type of reaction are well-known general reactions such us (1) the Finkelstein reaction, (2) the Menschutkin reaction, (3) the alcoholysis of alkyl halides, and (4) various isotopic exchange reactions.


Beta And Gamma Distributions, Calvin Rogers May 1956

Beta And Gamma Distributions, Calvin Rogers

Mathematics & Statistics ETDs

The purpose of this paper is to exhibit the main properties of Gamma and Beta distributions and show their relation to certain well known distributions.

In chapter II the Gamma and Beta distributions are defined in terms of Gamma and Beta functions. The moments of these distributions are calculated, and the moment generating function and cumulant generating function for the Gamma distribution are obtained. The curves are classified with respect to parameter values and the curves are graphically illustrated in Figures 1, 2, and 3. The exponential distribution, as a special case of interest, is shown to be a Gamma …


Geology Of The Central Front Of The Fra Cristobal Mountains, Sierra County, New Mexico, Richard C. Jacobs May 1956

Geology Of The Central Front Of The Fra Cristobal Mountains, Sierra County, New Mexico, Richard C. Jacobs

Earth and Planetary Sciences ETDs

This report includes about seven square miles of the central front of the Fra Cristobal Mountains. The area contains rocks from Precambrian, Cambrian, Pennsylvanian, and Quaternary Age. Fragmentary exposures of the Permian sedimentary rocks are also present.


Geology Of The White Rock Mountain Area, Gunnison County, Colorado, David L. Gaskill May 1956

Geology Of The White Rock Mountain Area, Gunnison County, Colorado, David L. Gaskill

Earth and Planetary Sciences ETDs

The White Rock Mountain area in central-western Colorado is included in the northwest corner of the Crested Butte quadrangle and the extreme southwest corner of the Aspen quadrangle. Mineral deposits were recognized in the early seventies, and in the literature the area is referred to as the Elk Mountain District.


An Indicator Of Position With Respect To The Earth's Magnetic Field, Lloyd C. Nielsen May 1956

An Indicator Of Position With Respect To The Earth's Magnetic Field, Lloyd C. Nielsen

Physics & Astronomy ETDs

A large amount of experimental research in the field of atmospheric physics involves carrying apparatus aloft by means of balloons. Data from balloon-borne instruments may be obtained either by recovery of the apparatus or by radio telemetering during the flight. Of these two methods, the latter is of course the more convenient and reliable, since recovery of the apparatus is time-consuming and often impossible.


The Motion Of A Charged Particle In Homogenous Time-Varying Magnetic Field, Thomas R. Bates May 1956

The Motion Of A Charged Particle In Homogenous Time-Varying Magnetic Field, Thomas R. Bates

Physics & Astronomy ETDs

This paper will discuss the motion of a non-relativistic, non-radiating charged particle in an infinite homogeneous magnetic field which varies linearly with time. We shall assume the motion to be confined to a plane perpendicular to the magnetic field.


Geology Of The Canjilon Cauldron Sink Near Bernalillo, Sandoval County, New Mexico, Felix E. Mutschler May 1956

Geology Of The Canjilon Cauldron Sink Near Bernalillo, Sandoval County, New Mexico, Felix E. Mutschler

Earth and Planetary Sciences ETDs

Canjilon Hill is located on the west side of the Rio Grande, about 2 3/4 miles north-northwest of Bernalillo. Exposed on the hill is a local unit of breccia, conglomerate, and sandstone, which forms an elongate saucer-shaped body 4100 feet long, 2200 feet wide and 280 to 500+ feet thick. Unlike the underlying Santa Fe formation these strata contain an abundance of large angular basalt pebbles, cobbles, and boulders. In this paper these strata are termed the Canjilon formation of the Santa Fe group. Structural and sedimentological evidence suggest that the Canjilon formation was deposited in a subsidence depression initiated …


The Use Of Kamke's Transformation In Approximating The Zeros Of Orthogonal Polynomials, Robert L. Daniels May 1956

The Use Of Kamke's Transformation In Approximating The Zeros Of Orthogonal Polynomials, Robert L. Daniels

Mathematics & Statistics ETDs

The importance of the classical orthogonal polynomials has long been acknowledged. It has not been possible, however, to represent them in such a way that all of their important properties are immediately evident. In particular, the location of the zeros of these polynomials is of considerable interest.

This thesis is primarily concerned with a different technique in which Kamke's transformation is applied to the differential equations frequently used to define these polynomials. The resulting trigonometric differential equations cannot be explicitly solved either, but certain characteristics of these solutions facilitate the derivation of approximations to the zeroes of the solutions.


Paleozoic Stratigraphy Of The Mud Springs Mountains, Sierra County, New Mexico, John Davis Hill May 1956

Paleozoic Stratigraphy Of The Mud Springs Mountains, Sierra County, New Mexico, John Davis Hill

Earth and Planetary Sciences ETDs

This thesis gives a history of the terminology of each of the formations found in the Mud Springs Mountains as well as a discussion of the characteristics of each. The Mud Springs Mountains Section of Paleozoic rocks is 3660 feet thick. Parts of all the Paleozoic systems are represented except the Silurian and Mississippian. The Bliss sandstone is 145 feet thick, the lower 65 feet being late Cambrian and the upper 80 feet being early Ordovician. The El Paso limestone of early Ordovician age is 460 feet thick.


The Instability Of Folded Structures, Robert Del Mar May 1956

The Instability Of Folded Structures, Robert Del Mar

Earth and Planetary Sciences ETDs

Folded structures are not necessarily stable through geologic time. "Unfolding" is defined as the changes in attitude through with folded structures go subsequent to their creation by tectonic means, other than by faulting alone. The principal types of unfolding, together with their causes, are: (1) the effect of gravity on isolated structures, and the effects of loading and unloading insofar as the gravitational force is concerned; (2) basining action and its effect on unloading; (3) the action of vertical forces on folded structures; (4) migrating or "wave" folds in relation to unfolding.


Faculty Senate Meeting Minutes, 05/15/1956, P 319-360, Unm Faculty Senate May 1956

Faculty Senate Meeting Minutes, 05/15/1956, P 319-360, Unm Faculty Senate

Faculty Senate Meeting Minutes, 1920 - 2013

No abstract provided.


Faculty Senate Meeting Minutes, 04/24/1956, P 290-318, Unm Faculty Senate Apr 1956

Faculty Senate Meeting Minutes, 04/24/1956, P 290-318, Unm Faculty Senate

Faculty Senate Meeting Minutes, 1920 - 2013

No abstract provided.


New Mexico Lobo, Volume 059, No 79, 4/13/1956, University Of New Mexico Apr 1956

New Mexico Lobo, Volume 059, No 79, 4/13/1956, University Of New Mexico

1956

New Mexico Lobo, Volume 059, No 79, 4/13/1956


New Mexico Lobo, Volume 059, No 78, 4/12/1956, University Of New Mexico Apr 1956

New Mexico Lobo, Volume 059, No 78, 4/12/1956, University Of New Mexico

1956

New Mexico Lobo, Volume 059, No 78, 4/12/1956