Preliminary Geologic Map of the Mint Canyon 7.51 Quadrangle Southern
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Oreodonts of the Tick Canyon Formation , Southern California
PALE0B10s Contributions from the University of California Museum of Paleontology, Berkeley No. I June 15, 1967 OREODONTS OF THE TICK CANYON FORMATION , SOUTHERN CALIFORNIA by David P. Whistler OREODONTS OF THE TICK CANYON FORMATION, SOUTHERN CALIFORNIA BY DAVID P. WHISTLER In 1940, Richard H. Jahns reviewed the stratigraphy of the nonmarine Mint Canyon Formation in the eastern part of the Ventura Basin and separated from it a new formation and fauna. Previous to this work, a controversy existed as to the age of the Mint Canyon Formation, for it contained vertebrates considered indicative of both the Miocene and Pliocene (Kew, 1924, Maxson, 1930, and Stirton, 1933). As a partial solut,ion to this controversy, Jahns demonstrated the presence of an erosional unconformity low in the nonmarine sequence which indicated a shift in source area. He redefined the beds below the unconformity as the Tick Canyon Formation (Jahns, 1940, pp. 163-66). Additional fossils discovered in the Tick Canyon Formation since Maxson's work, and certain of the forms described by Maxson, comprise the Tick Canyon fauna. Only two specimens described by Maxson are from the Tick Canyon Formation, UCMP 30046, the type of Miolabis californicus and UCMP 23852, a dentary fragment of a Parahippus. Neither of these permitted a definitive age determination. The additional fauna described by Jahns indicates an Arikareean mammalian age (early Miocene), and there is a noteworthy temporal hiatus between the Tick Canyon fauna and the over lying Mint Canyon fauna. In addition, faunas comprising three mammalian ages, late Barstovian, and earlier and late Clarendonian, are now recognized from the Mint Canyon Formation, but this is not the principal concern of this paper. -
Barren Ridge FEIS-Volume IV Paleo Tech Rpt Final March
March 2011 BARREN RIDGE RENEWABLE TRANSMISSION PROJECT Paleontological Resources Assessment Report PROJECT NUMBER: 115244 PROJECT CONTACT: MIKE STRAND EMAIL: [email protected] PHONE: 714-507-2710 POWER ENGINEERS, INC. PALEONTOLOGICAL RESOURCES ASSESSMENT REPORT Paleontological Resources Assessment Report PREPARED FOR: LOS ANGELES DEPARTMENT OF WATER AND POWER 111 NORTH HOPE STREET LOS ANGELES, CA 90012 PREPARED BY: POWER ENGINEERS, INC. 731 EAST BALL ROAD, SUITE 100 ANAHEIM, CA 92805 DEPARTMENT OF PALEOSERVICES SAN DIEGO NATURAL HISTORY MUSEUM PO BOX 121390 SAN DIEGO, CA 92112 ANA 032-030 (PER-02) LADWP (MARCH 2011) SB 115244 POWER ENGINEERS, INC. PALEONTOLOGICAL RESOURCES ASSESSMENT REPORT TABLE OF CONTENTS 1.0 INTRODUCTION ........................................................................................................................... 1 1.1 STUDY PERSONNEL ....................................................................................................................... 2 1.2 PROJECT DESCRIPTION .................................................................................................................. 2 1.2.1 Construction of New 230 kV Double-Circuit Transmission Line ........................................ 4 1.2.2 Addition of New 230 kV Circuit ......................................................................................... 14 1.2.3 Reconductoring of Existing Transmission Line .................................................................. 14 1.2.4 Construction of New Switching Station ............................................................................. -
Geological Considerations in Dams Failure Teodora Barbuntoiu A
Geotechnical Hazards | Geological Considerations in Dams Failure Teodora Barbuntoiu A Thesis in the Field of GeoEngineering For the Degree of Bachelor of Applied Earth Science Supervisors: Dr.Ir. W. Broere Dr.Ir. D.J.M. Ngan-Tillard Delft University of Technology July 2019 Teodora Barbuntoiu | Geological considerations in dams failure | AESB3400 Bachelor Thesis Abstract Dams and reservoirs pose safety concerns to society worldwide. In case of a disaster, the water impounded in the reservoir escapes and destroys everything in its path. Reasons for failure range from geology, hydrology and seismicity, to design problems, lack of maintenance and poor field investigation. Prior cases show that various dams gave away mainly due to geological causes, so there is a particular interest to see how the local terrain features could influence the longevity of the structure. Three historical case studies are discussed in order to emphasize the impact of geology regarding dam failure. The Saint Francis Dam is a prime example of poor site investigation, where the lack of knowledge on the foundation rock led to the rupture of the gravity dam. The Malpasset Dam gave away predominantly due to underestimated effects of the uplift, nevertheless, the geologists were unaware of an active fault system and the mechanical properties of the rock mass. The Baldwin Hills Reservoir comes with a more thorough site investigation, yet still, due to earth movements, the water from the reservoir infiltrated through the embankment. Therefore, geological features at the site need to be included in the design options of the dam in order to ensure a safe, feasible and economical project. -
31762102033147.Pdf (8.743Mb)
Sedimentology, provenance, and tectonic setting of the Miocene Horse Camp Formation (Member 2), east-central Nevada by Brian Keith Horton A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences Montana State University © Copyright by Brian Keith Horton (1994) Abstract: A study of the sedimentology, compositional trends, and modem tectonic setting of a 1600 m-thick sedimentary succession provides information on the late Cenozoic paleogeography and tectonics of an extensional basin and adjacent orogen in the Basin and Range province of east-central Nevada. Interpretations of depositional environments and reconstructions of paleogeography utilize detailed sedimentologic analyses of fourteen distinct facies and four facies associations from nine measured stratigraphic sections. Conglomerate compositional data and considerations of modern tectonic setting and local geologic structures provide constraints on the tectonic development of the extensional basin and orogen. Within the Miocene Horse Camp Formation (Member 2), four facies associations are defined by specific combinations of fourteen potential facies and attributed to processes characteristic of particular depositional environments. Subaerial and subaqueous fan-delta environments were characterized by deposition of sediment gravity flows and an absence of fluvial processes. A nearshore lacustrine facies association recorded wave-influenced sedimentation near a lake shoreline. Quiet-water deposition and limited sediment gravity flows characterized an offshore lacustrine environment. Lateral facies variations and stratal thinning and fining trends suggest a sediment source terrane to the south/southeast in the northern Grant Range. Simulated unroofing of this source terrane generated a hypothetical clast composition suite that is similar to actual conglomerate compositional data from Member 2. -
GEOLOGY of the TICK CANYON AREA May 23, 1952
GEOLOGY OF THE TICK CANYON AREA J. Richard Woodcock California Institute of ·rechnology May 23, 1952 Table of Cantents. Abstract •••••••••••••••••••••••••••••••••••••••••••••••••••••••••• 1 Introdttction . • . • . • . • • . • • . • . • . • • • . • . • • • . • . • • • • • • • • . • • • • • . • • • • • • • L. Aknowledgm.ents • • •• • • • ••••••••••• • •• e ••••••••••••••• • •••••••• • ••••••• • • 5 General Geography••••••••••••••••••••••••••••••••••••••••••••••••••••• 6 Statigraphy and Lithology ••••••••••••••••••••••••••••••••••••••••••••• 8 Basement Complex •••••••••••••·••••••••••••••••••••••••••••••••••· 9 Vasq.uez FO:rmation • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • 9 General (Vasquez Formation) ...................................... 19 Tick Canyon Formation .............•.....•..••.•..•............•.. 19 Mint Canyon Formation ............................................ 20 Whonoz Formation ••••••••••••••••••••••••••••••••••••••••••••••••• 20 General (Tick Canyon and Mint Canyon Formations) ................. 21 Structure ............................................................. 22 Geomorphology••••••••••••••••••••••••••••••••••·•••••••••••••••••••••• 2L Drainage • . • • • • • • • • • • . • • • . • • • • • • . • • • . • • • • • • . • • . • • . • • . • • • • • • • • • • • 2 h Relief ........................................................... 24 Geologic History •••••••••••••••••••••••••••••••••••••••••••••••••••••• 26 Illustrations: Figure: 1. Index l~p •••••••••••••••·••••••••••••••••••••••••••••••••••••• -
A Tertiary Mammalian Fauna from the Mint Canyon Formation (Maxson
A TERTIARY MAMMALIAN FAUNA FROM THE MINT CANYON FORMATION, SOUTHERN CALIFORNIA by John H. Maxson In Partial Fulfillment of the Requirements for the Degree of Master of Science California Institute of Technology Pasadena, California 1928 CONTENTS Page Introduction -----------------------------------------• 1 Acknowledgements ---------------------------------------- 1 Geography and Distribution ------------------------------ 4 Geologic Features ------------------- ---- ------------- 4 Nature of the Pa.leontologic li;a.terial ------------------- 9 Mint Canyon Fauna -------------------------------------- 10 Faunal List ---------------------------------------- 10 Pa.rahippus, sp. - ---------------------------------- 10 Merychippus califoraicus 1..Cerria.m -------------------- 11 Merychippus intermonta.nus Merriam------------------- 12 Protohippus7 ,.sp. ----------------------------------- 14 Miola.bis californicus, sp. nov. -------------------- 16 Merycodus?, sp. ------------------------------------ 20 Anti locapr id'i' ----------- ------------------------ 20 Archeolagus?, sp. or Hypolagus?, sp. -------------- 20 Mastodon remains 21 Avian remains ------------------------------------- 21 Testudinate remains ------------------------------- 21 Faunal Relationships 22 References 24 Explanation of Plates 25 ILLUSTRATIONS Page Fig. l. Index Map of Southern California ------------- 2 Fig. 2. Typical exposure of Mint Canyon beds --------- 3 Fig. 3. Pa.ra.hippus locality--------------------------- 5 Fig. 4. Qua.ternary terrace gravels-------------------- -
Deposition and Deformation in the Northern Soledad Basin (Muehlberger 1954)
DEPOSITION AND DEFORMATION IN THE NOR THE RN SOLEDAD BASIN, LOS ANGELES COUNTY, CALIFORNIA Thesis by William Rudolf Muehlberger In Partial Fulfillment of the Requirements for the degree of Doctor of Philosophy California Institute of Technology Pasadena, California 1954 -1- ACKNOWLEDGMENTS The writer wishes to express his gratitude to Dr. R. H. Jahns of the California Institute of Technology not only for suggesting this study of the Soledad basin, but also for his guidance and helpful criticism during the progress of the work. Discussions with Drs. J. P. Buwalda, A. E. J. Engel, L. C. Pray, and R. P. Sharp, all of the California Institute of Technology, have aided in clarifying several aspects of the study. The writer also has benefited from discussions of the regional aspects of the problem with several fellow students who have worked in parts of the area shown in Plate 1. Among these men are C. R. Allen, R. B. Campbell, L. A. Carlson, R. 0. Castle, G. P. Eaton, Ross Ellis, M. F. Meier, Carel Otte, Jr., Jesus Ruiz Elizondo, and L. T. Silver. The officials of the U. S. Forest Service and the numerous residents of the region aided in the rapid completion of the field studies by allowing the writer free access to their lands. The field work was supported in part by a research grant from the Division of Geological Sciences of the California Institute of Tech nology. The use of the equipment and facilities of the Division also was very helpful. The writer is much indebted to his wife, Sally P. -
WARD's Natural Science Establishment, Inc
MANUAL FOR WARD'S COLLECTION OF CLASSIC NORTH AMERICAN ROCKS 45 E 7217 Ward's is indebted to Dr. E. William Heinrich, Professor of Mineralogy, The University of Michigan, for the classification ofthe rocks in the new col ledion, for the descriptions of Thin Sedions and for editorial assistance in the preparation of the manual that accompanies the colledion. Since the geology of the region in which the rock is found and other relevant data in the literature may be of considerable interest, brief references to pertinent literature is provided for each rock. A bibliography of petrologic literature is also provided. WARD'S Natural Science Establishment, Inc. Copyright1970;Aev.1990 Printed in U.SA WARD'S COLLECTION OF CLASSIC NORTH AMERICAN ROCKS BIBLIOGRAPHY Allen, J.B. and ~harsley: NEPHELINE-SYENITE AND PHONOLITE Alling, H.L.: INTERPRETATIVE PETROGRAPHY OF THE IGNEOUS ROCKS Barth, T.F.W.: THEORETICAL PETROLOGY Daly, R.A.: IGNEOUS ROCKS AND THE DEPTHS OF THE EARTH Dana, E.S.: DANA'S TEXTBOOK OF MINERALOGY, 4th Ed. Revised by W.E. Ford Fairbairn, H.W.: STRUCTURAL PETROLOGY OF DEFORMED ROCKS Grout, F.F.: PETROLOGY AND PETROGRAPHY Harker, A.: PETROLOGY FOR STUDENTS Hatch, F.H. and Rastall, R.H.: PETROLOGY OF THE SEDIMENTARY ROCKS Heinrich, W.E.: MICROSCOPIC PETROGRAPHY THE GEOLOGY OF CARBONATITES Hess, H.H. and Poldervaart, A.: BASALTS, Vols. 1 and 2 Holmes, Arthur: PETROGRAPHIC METHODS AND CALCULATIONS Iddings, J.P.: ROCK MINERALS IGNEOUS ROCKS, Vols. I, II Johannsen, Albert: MANUAL OF PETROGRAPHIC METHODS A DESCRIPTIVE PETROGRAPHY OF THE IGNEOUS ROCKS Vol. I Introduction, Textures, Classifications and Glossary Vol. -
Signature Redacted for Privacy. Robeqs. Yeats
AN ABSTRACT OF THE DISSERTATION OF Barbara Jean Ellis for the degree of Doctor of Philosophy in Geology presented on May 12, 1994, Title: Changing Tectonic Regimes in the Southern Salinian Block: Extension, Strike-Slip Faulting. Compression and Rotation in the Cuyama Valley, Ca1ifornia ,.Signature redacted forprivacy. Abstract approved: RobeqS.Yeats During the Cenozoic, tectonics in the Cuyama basin of the southeastern Salinian block changed from extension to strike-slip faulting to compression and rotation. During the Oligocene-early Miocene, the Cuyama basin was adjacent to the southern Mojave region and part of that extensional tectonic regime. Many present-day reverse faults have an extensional history. At -P23 Ma, strike-slip faulting began, and the Cuyama basin was part of a zone of distributed shear between the North American and Pacific plates. The Russell fault, which is the oldest documented right-lateral fault in the region, began movement at -P23 Ma which continued until 4 Ma. Tracing its 29 km of slip south of the Big Pine fault is problematic.It may connect with the Blue Rock fault below the Cuyama Badlands, and then correlate with the Clemens Well-Fenner-San Francisquito fault segments, another early strand of the San Andreas fault system to the south. An associated left-lateral fault is proposed to underlie the southeast Caliente Range. The Cox normal fault, which was active during deposition of the Saltos Shale member of the Monterey Formation, is another structure associated with the early right-lateral shear. Compressional tectonics have occurred more recently. The Caliente Range is moving south on the Whiterock and Morales thrusts; the Sierra Madre is moving north on the South Cuyama and Ozena faults. -
Geology of Southeastern Ventura Basin Los Angeles County California
Geology of Southeastern Ventura Basin Los Angeles County California By E. L. WINTERER and D. L. DURHAM SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 334-H A study of the stratigraphy, structure, and occurrence of oil in the late Cenozoic Ventura basin UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEW ART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Page Abstract ____________________________________________ 275 Stratigraphy Continued Introduction.______________________________________ 276 Tertiary system Continued Purpose and scope.------_______________________ 276 Pliocene series..._________------__---__----- 308 Fieldwork __ __________________________________ 276 Pico formation.____________-_----_-_-_- 308 Acknowledgments. _ _----_-_-.________________- 276 Stratigraphy and lithology___________ 309 Geography. _________________________________________ 278 Newhall-Potrero area__________ 309 Climate- ______--_-__-_-__-_--_-_____________-_ 278 Newhsll-Potrero oil field to East Vegetation.____________________________________ 278 Canyon____________________ 310 Santa Clara River______________________________ 278 Mouth of East Canyon to San Fer Relief. __.._.._._._________---_-_--_________ 278 nando Pass__-----_-_-------- 311 Human activities----_------__--________________ 278 San Fernando Pass to San Gabriel Physiography_ _____________________________________ 278 fault..____-__-__-_------.--_ 311 Structural and lithologic control of drainage______ 279 Santa Clara River to Del Valle River terraces and old erosion surfaces-__ _________ 279 fault.___----.--_-_---------_ 312 Present erosion cycle.___________________________ 281 Del Valle fault to Holser fault__ 312 Landslides- ___--.-------_-_--___________________ 281 Area north of Holser fault- ______ 312 Stratigraphy.______________________________________ 281 Fossils.. -
Geology of Vasquez Rocks Researched and Compiled by Sarah Brewer
Geology of Vasquez Rocks Researched and Compiled by Sarah Brewer Aerial view of the majority of Vasquez Rocks Natural Area Park, with State Route 14 Freeway visible in the lower right and Escondido Canyon Road (the road used to access the park) visible in the upper left. Note clearly visible sandstone layers which form the unique and dramatic landscape. Image ©Google Maps, 2016. The Rocks are located in what is known as the Soledad Basin, which sits cradled to the south of the smaller Sierra Pelona Mountains, and to the west and north of the more well-known, larger San Gabriel Mountains. Soledad Canyon runs to the south of the park, Mint Canyon runs to the north, and Agua Dulce Canyon runs north to south right through the Vasquez Rocks area. The distinctive formations in the Vasquez Rocks area were actually formed through a relatively simple process, and the clues to its creation are still visible all around. Over the course of the past 25 million years (the most commonly agreed-upon age by geologists), vast amounts of sediment (sand, soil, rocks, and organic materials) were brought downward into the Soledad Basin by events such as rains, flooding, landslides, wind, and earthquakes from the surrounding San Gabriel and Sierra Pelona Mountains. As these materials were deposited on the basin’s floor, they would settle flat on the ground surface, and as years passed, new deposits covered the older ones, eventually placing them under tremendous amounts of pressure. With this pressure, the deeper layers became solidified, turning into what we know as sandstone. -
Geologic Units of California
UNITED STATES DEPARTMENT OF THE INTERIOR Ray Lyman Wilbur, Secretary GEOLOGICAL SURVEY George Oils Smith, Director Bulletin 826 NAMES AND DEFINITIONS OF THE GEOLOGIC UNITS OF CALIFORNIA COMPILED BY M.GRACE WILMARTH UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON: 1931 For snle by the Superintendent of Documents, Washington, D. C. ----- Price 20 cents PREFACE By T. W. STANTON In Bulletin 769, " The geologic time classification of the United States Geological Survey," by M. Grace Wilmarth, secretary of the committee on geologic names, it was announced that Miss. Wilmarth had in preparation a more extended compilation which will form a stratigraphic lexicon of the United States, containing definitions of all the geologic formations that have been named and described in this country. Work on this compilation is making good progress and has now reached a stage where it is possible to give geologists a sample of the lexicon, which will be locally useful and at the same time give them an opportunity to make helpful criticisms both of the character of the material to be included in the larger work and of the form in which it is presented. It happens that California is almost completely isolated from the other States in its stratigraphic development and that the great local variations in sedimentation within its borders, epecially in Tertiary time, have caused the naming of an unusual number of formations. Less than half a dozen of the formations named in California extend into Oregon and Washington, and the number that come into eastern California from Nevada is not much larger. It is therefore thought desirable to issue the " Names and definitions of the geologic units of California " as a separate publication.