1,408 research outputs found
Economic map of the Lake Elsinore Quadrangle: Supplement 2 from "I. Geology of the Southwest quarter of the Elsinore Quadrangle. II. Geochemical properties of the waters of the Elsinore Quadrangle [= Geology of the Lake Elsinore Quadrangle, California. Mineral deposits of Lake Elsinore Quadrangle, California]" (Thesis)
No full textThe Lake Elsinore quadrangle covers about 250 square miles and includes parts of the southwest margin of the Perris Block, the Elsinore trough, the southeastern end of the Santa Ana Mountains, and the Elsinore Mountains.
The oldest rocks consist of an assemblage of metamorphics of igneous effusive and sedimentary origin, probably, for the most part, of Triassic age. They are intruded by diorite and various hypabyssal rocks, then in turn by granitic rocks, which occupy over 40 percent of the area. Following this last igneous activity of probable Lower Cretaceous age, an extended period of sedimentation started with the deposition of the marine Upper Cretaceous Chico formation and continued during the Paloecene under alternating marine and continental conditions on the margins of the blocks. A marine regression towards the north, during the Neocene, accounts for the younger Tertiary strata in the region under consideration.
Outpouring of basalts to the southeast indicates that igneous activity was resumed toward the close of the Tertiary. The fault zone, which characterizes the Elsinor trough, marks one of the major tectonic lines of southem California. It separates the upthrown and tilted block of the Santa Ana Mountains to the south from the Perris Block to the north.
Most of the faults are normal in type and nearly parallel to the general trend of the trough, or intersect each other at an acute angle. Vertical displacements generally exceed the horizontal ones and several periods of activity are recognized.
Tilting of Tertiary and older Quaternary sediments in the trough have produced broad synclinal structures which have been modified by subsequent faulting.
Five old surfaces of erosion are exposed on the highlands.
The mineral resources of the region are mainly high-grade clay deposits and mineral waters.Cataloger's note: Engel, Rene. I. Geology of the Southwest quarter of the Elsinore Quadrangle (1933). No copies [of this thesis] have ever been presented to C.I.T. The thesis has been published under the title: Geology of the Lake Elsinore Quadrangle, California (in Bulletin no. 146 of the California Division of Mines).
…Bulletin 146, a book containing two papers: Geology and Mineral Deposits of the Lake Elsinore Quadrangle, California, prepared by Rene Engel, and Mineral Deposits of Lake Elsinore Quadrangle, California by• Rene Engel, Thomas E. Gay, Jr., and B. L. Rogers. The principal author, Dr. Engel, first began studying the geology of this area in detail in the 1920's; he has been working with it intermittently since then.
The second paper, which is primarily concerned with the economic mineral deposits of the area, was compiled by two staff members of the Division of Mines, Messrs. Gay and Rogers, working under the supervision of Dr. Engel….
7 plates included in the Bulletin have also been scanned and included as part
of this record
Geologic map of Alberhill Coal and Clay Company clay deposits, Riverside County, California: Supplement 6 from "I. Geology of the Southwest quarter of the Elsinore Quadrangle. II. Geochemical properties of the waters of the Elsinore Quadrangle [= Geology of the Lake Elsinore Quadrangle, California. Mineral deposits of Lake Elsinore Quadrangle, California]" (Thesis)
No full textThe Lake Elsinore quadrangle covers about 250 square miles and includes parts of the southwest margin of the Perris Block, the Elsinore trough, the southeastern end of the Santa Ana Mountains, and the Elsinore Mountains.
The oldest rocks consist of an assemblage of metamorphics of igneous effusive and sedimentary origin, probably, for the most part, of Triassic age. They are intruded by diorite and various hypabyssal rocks, then in turn by granitic rocks, which occupy over 40 percent of the area. Following this last igneous activity of probable Lower Cretaceous age, an extended period of sedimentation started with the deposition of the marine Upper Cretaceous Chico formation and continued during the Paloecene under alternating marine and continental conditions on the margins of the blocks. A marine regression towards the north, during the Neocene, accounts for the younger Tertiary strata in the region under consideration.
Outpouring of basalts to the southeast indicates that igneous activity was resumed toward the close of the Tertiary. The fault zone, which characterizes the Elsinor trough, marks one of the major tectonic lines of southem California. It separates the upthrown and tilted block of the Santa Ana Mountains to the south from the Perris Block to the north.
Most of the faults are normal in type and nearly parallel to the general trend of the trough, or intersect each other at an acute angle. Vertical displacements generally exceed the horizontal ones and several periods of activity are recognized.
Tilting of Tertiary and older Quaternary sediments in the trough have produced broad synclinal structures which have been modified by subsequent faulting.
Five old surfaces of erosion are exposed on the highlands.
The mineral resources of the region are mainly high-grade clay deposits and mineral waters.Cataloger's note: Engel, Rene. I. Geology of the Southwest quarter of the Elsinore Quadrangle (1933). No copies [of this thesis] have ever been presented to C.I.T. The thesis has been published under the title: Geology of the Lake Elsinore Quadrangle, California (in Bulletin no. 146 of the California Division of Mines).
…Bulletin 146, a book containing two papers: Geology and Mineral Deposits of the Lake Elsinore Quadrangle, California, prepared by Rene Engel, and Mineral Deposits of Lake Elsinore Quadrangle, California by• Rene Engel, Thomas E. Gay, Jr., and B. L. Rogers. The principal author, Dr. Engel, first began studying the geology of this area in detail in the 1920's; he has been working with it intermittently since then.
The second paper, which is primarily concerned with the economic mineral deposits of the area, was compiled by two staff members of the Division of Mines, Messrs. Gay and Rogers, working under the supervision of Dr. Engel….
7 plates included in the Bulletin have also been scanned and included as part
of this record
Geologic map and sections of the southern Temescal Valley region: Supplement 5 from "I. Geology of the Southwest quarter of the Elsinore Quadrangle. II. Geochemical properties of the waters of the Elsinore Quadrangle [= Geology of the Lake Elsinore Quadrangle, California. Mineral deposits of Lake Elsinore Quadrangle, California]" (Thesis)
No full textThe Lake Elsinore quadrangle covers about 250 square miles and includes parts of the southwest margin of the Perris Block, the Elsinore trough, the southeastern end of the Santa Ana Mountains, and the Elsinore Mountains.
The oldest rocks consist of an assemblage of metamorphics of igneous effusive and sedimentary origin, probably, for the most part, of Triassic age. They are intruded by diorite and various hypabyssal rocks, then in turn by granitic rocks, which occupy over 40 percent of the area. Following this last igneous activity of probable Lower Cretaceous age, an extended period of sedimentation started with the deposition of the marine Upper Cretaceous Chico formation and continued during the Paloecene under alternating marine and continental conditions on the margins of the blocks. A marine regression towards the north, during the Neocene, accounts for the younger Tertiary strata in the region under consideration.
Outpouring of basalts to the southeast indicates that igneous activity was resumed toward the close of the Tertiary. The fault zone, which characterizes the Elsinor trough, marks one of the major tectonic lines of southem California. It separates the upthrown and tilted block of the Santa Ana Mountains to the south from the Perris Block to the north.
Most of the faults are normal in type and nearly parallel to the general trend of the trough, or intersect each other at an acute angle. Vertical displacements generally exceed the horizontal ones and several periods of activity are recognized.
Tilting of Tertiary and older Quaternary sediments in the trough have produced broad synclinal structures which have been modified by subsequent faulting.
Five old surfaces of erosion are exposed on the highlands.
The mineral resources of the region are mainly high-grade clay deposits and mineral waters.Cataloger's note: Engel, Rene. I. Geology of the Southwest quarter of the Elsinore Quadrangle (1933). No copies [of this thesis] have ever been presented to C.I.T. The thesis has been published under the title: Geology of the Lake Elsinore Quadrangle, California (in Bulletin no. 146 of the California Division of Mines).
…Bulletin 146, a book containing two papers: Geology and Mineral Deposits of the Lake Elsinore Quadrangle, California, prepared by Rene Engel, and Mineral Deposits of Lake Elsinore Quadrangle, California by• Rene Engel, Thomas E. Gay, Jr., and B. L. Rogers. The principal author, Dr. Engel, first began studying the geology of this area in detail in the 1920's; he has been working with it intermittently since then.
The second paper, which is primarily concerned with the economic mineral deposits of the area, was compiled by two staff members of the Division of Mines, Messrs. Gay and Rogers, working under the supervision of Dr. Engel….
7 plates included in the Bulletin have also been scanned and included as part
of this record
Geologic map of the Lake Elsinore Quadrangle: Supplement 1 from "I. Geology of the Southwest quarter of the Elsinore Quadrangle. II. Geochemical properties of the waters of the Elsinore Quadrangle [= Geology of the Lake Elsinore Quadrangle, California. Mineral deposits of Lake Elsinore Quadrangle, California]" (Thesis)
No full textThe Lake Elsinore quadrangle covers about 250 square miles and includes parts of the southwest margin of the Perris Block, the Elsinore trough, the southeastern end of the Santa Ana Mountains, and the Elsinore Mountains.
The oldest rocks consist of an assemblage of metamorphics of igneous effusive and sedimentary origin, probably, for the most part, of Triassic age. They are intruded by diorite and various hypabyssal rocks, then in turn by granitic rocks, which occupy over 40 percent of the area. Following this last igneous activity of probable Lower Cretaceous age, an extended period of sedimentation started with the deposition of the marine Upper Cretaceous Chico formation and continued during the Paloecene under alternating marine and continental conditions on the margins of the blocks. A marine regression towards the north, during the Neocene, accounts for the younger Tertiary strata in the region under consideration.
Outpouring of basalts to the southeast indicates that igneous activity was resumed toward the close of the Tertiary. The fault zone, which characterizes the Elsinor trough, marks one of the major tectonic lines of southem California. It separates the upthrown and tilted block of the Santa Ana Mountains to the south from the Perris Block to the north.
Most of the faults are normal in type and nearly parallel to the general trend of the trough, or intersect each other at an acute angle. Vertical displacements generally exceed the horizontal ones and several periods of activity are recognized.
Tilting of Tertiary and older Quaternary sediments in the trough have produced broad synclinal structures which have been modified by subsequent faulting.
Five old surfaces of erosion are exposed on the highlands.
The mineral resources of the region are mainly high-grade clay deposits and mineral waters.Cataloger's note: Engel, Rene. I. Geology of the Southwest quarter of the Elsinore Quadrangle (1933). No copies [of this thesis] have ever been presented to C.I.T. The thesis has been published under the title: Geology of the Lake Elsinore Quadrangle, California (in Bulletin no. 146 of the California Division of Mines).
…Bulletin 146, a book containing two papers: Geology and Mineral Deposits of the Lake Elsinore Quadrangle, California, prepared by Rene Engel, and Mineral Deposits of Lake Elsinore Quadrangle, California by• Rene Engel, Thomas E. Gay, Jr., and B. L. Rogers. The principal author, Dr. Engel, first began studying the geology of this area in detail in the 1920's; he has been working with it intermittently since then.
The second paper, which is primarily concerned with the economic mineral deposits of the area, was compiled by two staff members of the Division of Mines, Messrs. Gay and Rogers, working under the supervision of Dr. Engel….
7 plates included in the Bulletin have also been scanned and included as part
of this record
Geologic sections, Lake Elsinore Quadrangle, California: Supplement 3 from "I. Geology of the Southwest quarter of the Elsinore Quadrangle. II. Geochemical properties of the waters of the Elsinore Quadrangle [= Geology of the Lake Elsinore Quadrangle, California. Mineral deposits of Lake Elsinore Quadrangle, California]" (Thesis)
No full textThe Lake Elsinore quadrangle covers about 250 square miles and includes parts of the southwest margin of the Perris Block, the Elsinore trough, the southeastern end of the Santa Ana Mountains, and the Elsinore Mountains.
The oldest rocks consist of an assemblage of metamorphics of igneous effusive and sedimentary origin, probably, for the most part, of Triassic age. They are intruded by diorite and various hypabyssal rocks, then in turn by granitic rocks, which occupy over 40 percent of the area. Following this last igneous activity of probable Lower Cretaceous age, an extended period of sedimentation started with the deposition of the marine Upper Cretaceous Chico formation and continued during the Paloecene under alternating marine and continental conditions on the margins of the blocks. A marine regression towards the north, during the Neocene, accounts for the younger Tertiary strata in the region under consideration.
Outpouring of basalts to the southeast indicates that igneous activity was resumed toward the close of the Tertiary. The fault zone, which characterizes the Elsinor trough, marks one of the major tectonic lines of southem California. It separates the upthrown and tilted block of the Santa Ana Mountains to the south from the Perris Block to the north.
Most of the faults are normal in type and nearly parallel to the general trend of the trough, or intersect each other at an acute angle. Vertical displacements generally exceed the horizontal ones and several periods of activity are recognized.
Tilting of Tertiary and older Quaternary sediments in the trough have produced broad synclinal structures which have been modified by subsequent faulting.
Five old surfaces of erosion are exposed on the highlands.
The mineral resources of the region are mainly high-grade clay deposits and mineral waters.Cataloger's note: Engel, Rene. I. Geology of the Southwest quarter of the Elsinore Quadrangle (1933). No copies [of this thesis] have ever been presented to C.I.T. The thesis has been published under the title: Geology of the Lake Elsinore Quadrangle, California (in Bulletin no. 146 of the California Division of Mines).
…Bulletin 146, a book containing two papers: Geology and Mineral Deposits of the Lake Elsinore Quadrangle, California, prepared by Rene Engel, and Mineral Deposits of Lake Elsinore Quadrangle, California by• Rene Engel, Thomas E. Gay, Jr., and B. L. Rogers. The principal author, Dr. Engel, first began studying the geology of this area in detail in the 1920's; he has been working with it intermittently since then.
The second paper, which is primarily concerned with the economic mineral deposits of the area, was compiled by two staff members of the Division of Mines, Messrs. Gay and Rogers, working under the supervision of Dr. Engel….
7 plates included in the Bulletin have also been scanned and included as part
of this record
Geologic map and sections of Los Angeles Brick and Clay Products Company no.1 clay pit, Alberhill, Riverside Co., California: Supplement 7 from "I. Geology of the Southwest quarter of the Elsinore Quadrangle. II. Geochemical properties of the waters of the Elsinore Quadrangle [= Geology of the Lake Elsinore Quadrangle, California. Mineral deposits of Lake Elsinore Quadrangle, California]" (Thesis)
No full textThe Lake Elsinore quadrangle covers about 250 square miles and includes parts of the southwest margin of the Perris Block, the Elsinore trough, the southeastern end of the Santa Ana Mountains, and the Elsinore Mountains.
The oldest rocks consist of an assemblage of metamorphics of igneous effusive and sedimentary origin, probably, for the most part, of Triassic age. They are intruded by diorite and various hypabyssal rocks, then in turn by granitic rocks, which occupy over 40 percent of the area. Following this last igneous activity of probable Lower Cretaceous age, an extended period of sedimentation started with the deposition of the marine Upper Cretaceous Chico formation and continued during the Paloecene under alternating marine and continental conditions on the margins of the blocks. A marine regression towards the north, during the Neocene, accounts for the younger Tertiary strata in the region under consideration.
Outpouring of basalts to the southeast indicates that igneous activity was resumed toward the close of the Tertiary. The fault zone, which characterizes the Elsinor trough, marks one of the major tectonic lines of southem California. It separates the upthrown and tilted block of the Santa Ana Mountains to the south from the Perris Block to the north.
Most of the faults are normal in type and nearly parallel to the general trend of the trough, or intersect each other at an acute angle. Vertical displacements generally exceed the horizontal ones and several periods of activity are recognized.
Tilting of Tertiary and older Quaternary sediments in the trough have produced broad synclinal structures which have been modified by subsequent faulting.
Five old surfaces of erosion are exposed on the highlands.
The mineral resources of the region are mainly high-grade clay deposits and mineral waters.Cataloger's note: Engel, Rene. I. Geology of the Southwest quarter of the Elsinore Quadrangle (1933). No copies [of this thesis] have ever been presented to C.I.T. The thesis has been published under the title: Geology of the Lake Elsinore Quadrangle, California (in Bulletin no. 146 of the California Division of Mines).
…Bulletin 146, a book containing two papers: Geology and Mineral Deposits of the Lake Elsinore Quadrangle, California, prepared by Rene Engel, and Mineral Deposits of Lake Elsinore Quadrangle, California by• Rene Engel, Thomas E. Gay, Jr., and B. L. Rogers. The principal author, Dr. Engel, first began studying the geology of this area in detail in the 1920's; he has been working with it intermittently since then.
The second paper, which is primarily concerned with the economic mineral deposits of the area, was compiled by two staff members of the Division of Mines, Messrs. Gay and Rogers, working under the supervision of Dr. Engel….
7 plates included in the Bulletin have also been scanned and included as part
of this record
The Negro in the novels of Rene Maran, 1940
No full textThis study of the Negro in the novels of Rene Maran, Frances most prominent contemporary Negro author, is one of several being made at Atlanta University on the Negro in French literature. This attempt to-show how a Negro, the only one ever to receive the Prix Goncourt, portrays his African brothers, is the first American study of Rene Maran's novels. It is hoped that it will be a modest contribution to an almost unexplored field in French literature and that other students of France and her culture will be inspired to make a more extensive study of Rene Maran and his works. The first chapter is devoted to the life of Rene Maran and a discussion of his style and most important works. The second chapter presents the physical characteristics of the Negro as portrayed by Rene' Maran. Emphasis is placed on physical appearance, tribal marks, dress, disease and odors which seem to be especially characteristic of the Negro. The third chapter is devoted to the social characteristics of the Negro with emphasis on home life, food, religion, feasts, and governments. The last chapter will present a summary of the findings of this study. The appendix includes short synopses of each of the novels with Negro characters, and a latter from Monsieur Maran to the writer. aIt is to be regretted that such a small amount of material has been written on Rene Maran. Because of his modesty he has written even less about himself. Biographical material consists principally of Leon Bocquet's "Preface" to le Petit Roi de Chimerie, a fairy story by Rene Maran; le Coeur serre, an autobiography written as a novel; several articles which have appeared in periodicals and the forementioned letter from Monsieur Maran. First editions of all novels, with exception of Le Livre de la brousse, were used. As the latter was unavailable, the second edition (1937) was used. Rene Maran's most important novels on Africa, Batouala, Djouma, Chien de brousse, Le Journal sans date end le Livre de la brousse have been studied. The novelettes Bokorro and Bassarragba have also been used as references but the longer novels have constituted our major interest. Le Petit Roi de Chimerie , though it contains no Negro characters, was quoted because of one excellent example of Rene Maran's style. Less stress has been placed on Le Journal sans date because only one of its characters is a Negro. The writer sincerely appreciates the kindness and help of Rene Maran, whose letter was a source of constant encouragement
On the Foreign-Exchange Risk Premium in Sticky-Price General Equilibrium Models
No full textThis paper investigates the behavior of the foreign exchange risk premium in two recent two-country intertemporal-optimizing general equilibrium models with sticky nominal prices: Obstfeld-Rogoff (1998) and Devereux-Engel (1998). The foreign exchange risk premium in any general equilibrium model arises from the correlation of the exchange rate with consumption. In flexible price models, that requires correlation of monetary and output supply shocks. In sticky-price models, the correlation arises endogenously because monetary shocks cause output and consumption to change. The size of the risk premium depends on how prices are set (in producers' currencies versus consumers' currencies), and on the form of the money demand function. In some cases, the risk premium generated by the model is quite large.
Investigation of ion-dioffusion in Perovksite Solar Cells
No full textAuthor Rene Zahrhuber, BScMasterarbeit Johannes Kepler Universität Linz 2024Arbeit gesperr
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A survey of Rene Touzet's piano compositions
No full textThis essay presents a survey of published and unpublished compositions for piano written by Cuban composer Rene Touzet. The survey includes information, such as the date of the composition, publishing information, length, tempo indications, information about recordings of the piece, and any published comments. The author further provides a brief description of each composition as well as any pertinent comments. A performer's guide of Mr. Touzet's Sonata Romantica is presented at the end of the thesis. This essay also contains Rene Touzet's biography. The author has compiled most of this information from a series of interviews with Mr. Touzet conducted between the years of 2001 and 2003.</p
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