GEOLOGY of the UPPER CRETACEOUS HORNBROOK FORMATION, OREGON and CALIFORNIA Editor

Total Page:16

File Type:pdf, Size:1020Kb

GEOLOGY of the UPPER CRETACEOUS HORNBROOK FORMATION, OREGON and CALIFORNIA Editor GEOLOGY OF THE UPPER CRETACEOUS HORNBROOK FORMATION, OREGON AND CALIFORNIA Editor TOR H. NILSEN U.S. Geological Survey Menlo Park, California September 28-30, 1984 Published by The Pacific Section Society of Economic Paleontologists and Mineralogists Los Angeles, California U.S.A. Geology of the Upper Cretaceous Hornbrook Formation, Oregon and California, 1984 Copyright © 2012 Pacific Section, SEPM (Society for Sedimentary Geology) For copies of this volume, write to: Treasurer, Pacific Section S.E.P.M. P.O. Box 10359 Bakersfield, CA 93389 Copyright© 1984 by the Pacific Section, Society of Economic Paleontologists and Mineralogists COPYRIGHT The papers in this volume were prepared for presentation at the 1984 fieldtrip of the Pacific Section of the Society of Economic Paleontologists and Mineralogists, held in Ashland, Oregon, September 28-30, 1984. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, without the prior writtten permission of the copyright owner. Printed by Comet Reproduction Service Santa Fe Springs, CA 90670 Pacific Section Society of Economic Paleontologists and Mineralogists Field Trip Leaders TOR H. NILSEN U.S. Geological Survey Menlo Park, California MONTY A. ELLIOTT Southern Oregon State College Ashland, Oregon Pacific Section SEPM Officers - 1984 PRESIDENT ROBERT E. GARRISON University of California, Santa Cruz, California VICE PRESIDENT JEFFREY MOUNT University of California, Davis, California SECRETARY CHRISTINE CARLSON U.S. Geological Survey, Menlo Park, California TREASURER PAUL F. BERTUCCI Chevron, U.S.A., Concord, California PAST PRESIDENT KENNETH A. PISCIOTTO SOHIO Petroleum, San Francisco, California PRESIDENT ELECT J. ALAN BARTOW U.S. Geological Survey, Menlo Park, California MANAGING EDITOR REINHARD SUCHSLAND DEPCO, Inc., Bakersfield, California PREFACE AND ACKNOWLEDGEMENTS This field trip guidebook to the Upper Cretaceous Hornbrook Formation of north-central California and southwestern Oregon has been prepared for the Annual Fall Field Trip of the Pacific Section of the Society of Economic Paleontologists and Mineralogists (SEPM), to be held in Ashland, Oregon, September 28-30, 1984. This field trip is the northernmost annual field trip held by the Pacific Section—almost all previous trips have been in the areas of either central or southern California. I am thankful to the executive council of the Pacific Section SEPM for their support, encouragement, and willingness to extend the geographic limits of their annual field trips and, in particular, for their attempts to include the geologic community of the Pacific Northwest in the planning of the trip. I am especially indebted to Kenneth Pisciotto, Steven Graham, Robert Garrison, Virgil Frizzell, Alan Bartow, Paul Bertucci, Jeffrey Mount, Reinhard Suchsland, and Christine Carlson of the Pacific Section for their help and support in organizing the field trip and preparing the guidebook. The field trip co-leader, Monty Elliott of Southern Oregon State College (SOSC), also undertook the responsibility of initially organizing lodging, meals, transportation, tickets to the Shakespeare Festival, and lecture halls, and is due many thanks. Ralph Golia and Greg Barats helped during various stages of the field trip organization, and Jan Zigler has carefully edited most of the papers and provided invaluable assistance in all stages of the guidebook preparation. The Ashland area is certainly a beautiful one that provides many exciting opportunities for both cultural, educational, and outdoor activities. I hope that, within the framework of the field trip, the exciting geology of the area will add to your enjoyment of it. "I have thrust myself into this maze, Haply to wive and thrive, as best I may." The Taming of the Shrew, Wm. Shakespeare Tor H. Nilsen Contents Page INTRODUCTION TO FIELD TRIP Tor H. Nilsen 1 DESCRIPTION OF FIELD TRIP STOPS AND ROADLOG, UPPER CRETACEOUS HORNBROOK FORMATION, SOUTHERN OREGON AND NORTHERN CALIFORNIA Tor H. Nilsen 9 GEOLOGIC AND GEOGRAPHIC SETTING OF THE HORNBROOK FORMATION, OREGON AND CALIFORNIA Monty Elliott 43 STRATIGRAPHY, SEDIMENTOLOGY, AND TECTONIC FRAMEWORK OF THE UPPER CRETACEOUS HORNBROOK FORMATION, OREGON AND CALIFORNIA .... Tor H. Nilsen 51 AGE AND CORRELATION OF THE CRETACEOUS HORNBROOK FORMATION, CALIFORNIA AND OREGON W.V. Sliter, D.L. Jones, and C.K. Throckmorton 89 SANDSTONE PETROGRAPHY OF THE UPPER CRETACEOUS HORNBROOK FORMATION, OREGON AND CALIFORNIA Ralph T. Golia and TorH. Nilsen 99 CONGLOMERATE CLAST COMPOSITION OF THE UPPER CRETACEOUS HORNBROOK FORMATION, OREGON AND CALIFORNIA Greg M. Barats, TorH. Nilsen and Ralph T. Golia 111 GEOCHEMISTRY OF COAL FROM THE DITCH CREEK SILTSTONE MEMBER OF THE HORNBROOK FORMATION, NORTHERN CALIFORNIA Jan L. Zigler and TorH. Nilsen 123 POROSITY, PERMEABILITY, AND DIAGENESIS OF SURFACE SAMPLES OF SANDSTONE FROM THE HORNBROOK FORMATION C.W. Kreighin andB.E. Law 129 THE PETROLEUM SOURCE-ROCK POTENTIAL OF THE UPPER CRETACEOUS HORNBROOK FORMATION, NORTH-CENTRAL CALIFORNIA AND SOUTHWESTERN OREGON B.E. Law, D.E. Anders and T.H. Nilsen 133 STRATIGRAPHY AND SEDIMENTOLOGY OF THE OSBURGER GULCH SANDSTONE MEMBER OF THE UPPER CRETACEOUS HORNBROOK FORMATION, NORTHERN CALIFORNIA AND SOUTHERN OREGON M.T. Gaona 141 LATE CRETACEOUS TRANSGRESSIVE SEDIMENTATION: A COMPARISON OF THE BASAL HORNBROOK FORMATION AND THE CAPE SEBASTIAN SANDSTONE, NORTHERN CALIFORNIA AND SOUTHWESTERN OREGON Joanne Bourgeois 149 TECTONOSTRATIGRAPHIC TERRANES IN SOUTHWESTERN OREGON M.C. Blake, Jr. 159 GEOLOGY OF THE KLAMATH MOUNTAINS NEAR YREKA, CALIFORNIA N. Mortimer 167 A NEOGENE STRUCTURAL DOME IN THE KLAMATH MOUNTAINS, CALIFORNIA AND OREGON N. Mortimer and R.G. Coleman 179 STRATIGRAPHY AND SEDIMENTOLOGY OF THE PAYNE CLIFFS FORMATION, SOUTHWESTERN OREGON Brian K. McKnight 187 THE LOWER WESTERN CASCADE VOLCANIC GROUP IN NORTHERN CALIFORNIA Joseph A. Vance 195 CATASTROPHIC DEBRIS AVALANCHE FROM AN ANCESTRAL MOUNT SHASTA VOLCANO, CALIFORNIA .. D.R. Crandell, C.D. Miller, R.L. Christiansen, H.X. Glicken and C.G. Newhall 197 A GEOLOGIC CROSS SECTION OF NORTHEASTERN CALIFORNIA FROM SEISMIC REFRACTION RESULTS G.S. Fuis and J.J. Zucca 203 A POTENTIAL-FIELD INTERPRETATION OF THE STRUCTURAL EDGE OF THE CRETACEOUS HORNBROOK BASIN IN NORTHERN CALIFORNIA M.C. Erskine, Jr., J. A. Wolleben and D.L. Lawler 211 IMPLICATIONS OF PALEOMAGNETISM FOR THE TECTONIC HISTORY OF THE EASTERN KLAMATH AND RELATED TERRANES IN CALIFORNIA AND OREGON Edward A. Mankinen, William P. Irwin and C. Sherman Gromme 221 PALEOMAGNETIC CONSTRAINTS ON THE INTERPRETATION OF EARLY CENOZOIC PACIFIC NORTHWEST PALEOGEOGRAPHY RayE. Wells 231 A PALEOGEOGRAPHIC REINTERPRETATION OF SOME MIDDLE CRETACEOUS UNITS, NORTH-CENTRAL OREGON: EVIDENCE FOR A SUBMARINE TURBIDITE SYSTEM Lewis C. Kleinhans, Elizabeth A. Balcells-Baldwin and Richard E. Jones 239 INTRODUCTION TO FIELD TRIP Tor H. Nilsen U.S. Geological Survey 345 Middlefield Road Menlo Park, California 94025 GENERAL SETTING The Hornbrook Formation has attracted the attention of the petroleum industry for many years, The Upper Cretaceous Hornbrook Formation crops partly because natural gas has been found in out to the northwest of Mount Shasta in north- numerous water wells in the area. The potential for central California and southwestern Oregon (Fig. finding both petroleum source and reservoir rocks in 1). It forms a northwest-striking and northeast- the Hornbrook Formation to the east of the outcrop dipping homoclinal sequence that underlies a series belt, beneath the western Cascade Range, has of narrow, discontinuous, northwest-trending valleys resulted in the leasing of large areas, especially between highlands of the Klamath Mountains and the in the Modoc Plateau region (Alldredge and Meigs, Cascade Range (Fig. 2). The Hornbrook Formation 1984). An exploration well drilled by Klamath rests unconformably on highly deformed Paleozoic, Exploration in 1983-84 about 21 km northeast of Triassic, and Jurassic metamorphic rocks and on Yreka, on the south flank of Bogus Mountain (Fig. Triassic and Jurassic plutons of the Klamath 2), penetrated about 640 m of Cretaceous sedimentary Mountains. The Hornbrook is overlain unconformably rocks, with a show of wet oil or gas (Alldredge and to the northeast by lower Tertiary nonmarine Meigs, 1984). sedimentary and volcanic rocks of the western Cascade Range. The location of all relevant U.S. The Cretaceous Ochoco basin in the Mitchell Geological Survey quadrangles in southern Oregon and area of central Oregon (Fig. 1) has been an area of northern California is shown in Figure 3. active petroleum exploration because it contains more than 4,300 m of Cretaceous marine sedimentary The Hornbrook Formation is one of a large rocks. If the Hornbrook Formation, Ochoco basin, number of widely scattered Cretaceous sedimentary and Great Valley sequence originally formed part of units that crop out in various parts of Oregon and the same large depositional basin, and are possibly northern California (Fig. 1). These discontinuous interconnected today beneath the cover of volcanic remnants of Cretaceous strata crop out in the rocks, then a large petroleum province could Mitchell area and other parts of the Blue Mountains, potentially exist in southern Oregon and in the Grave Creek and O'Brien areas of the Klamath northeastern California, - and possibly farther north Mountains, on the northern and western flanks of the as well. Klamath Mountains in the Days
Recommended publications
  • Read Our Publications Online 24/7/365 at ALWAYS HONORING OUR TRUE HEROES WE BACK OUR BLUE
    JEFFERSON BACKROADS Read our publications online 24/7/365 at www.JeffersonBackroads.com ALWAYS HONORING OUR TRUE HEROES WE BACK OUR BLUE A New State of Mind Wholesale & Retail Accessories for Jeffersonians JeffersonOutfitters.com Hildy Langewis 800-337-7389 - [email protected] Welcome Aboard! TABLE OF CONTENTS: THANK YOU! This happy little local 3 ADVERTISING RATES & INFO publication is made possible ONLY thanks to 9 BREWERIES AND DISTILLERIES - LOCAL our Honored Advertisers who graciously place their ADs with us. Our beloved writers, readers 15 DUNSMUIR RAILROAD DEPOT NEWS & EVENTS & subscribers complete the 10 EVENTS - JUST A FEW LOCAL HAPPENINGS circle... 13 GRANNY HAMMOND’S 100TH BIRTHDAY Keeping your 29 & 31 MAPS Business & Events on our 32-33 QUILTING STORIES, EVENTS, PHOTOS & INFO Community’s Radar is our 25 SENIOR CITIZENS INFO Best Pride & 8 STORY: BACKROADS ADVENTURES Joy! 26 STORY: INSPIRATIONS FROM THE FOREST We Positively LOVE what we 22 STORY: NORTHERN KLAMATH CO. HISTORY & EVENTS do. Sharing YOUR business 18 STORY: STITCHING IN THE DITCH - QUILTING is OUR 30 STORY: TAWANDA FARMS - LAMB & SHEEP WOOL Business. 12 & 25 VETERANS EVENTS - INFO & SERVICES Cover Image - Campsite at Butt Lake near Chester, California Photo by M. Fain Jefferson Backroads is proudly published for Law Abiding Citizens, our fellow Independent, Hard Working, Old School, Patriotic American Rebels who live in or travel through our Rugged & Beautiful State of Jefferson Region. The same true INDEPENDENT NATURE and OLD SCHOOL ESSENCE of “The State of Jefferson” can be found in Small Towns all across Rural America. We are proudly keeping our Patriotic American Spirit Alive.
    [Show full text]
  • Pilot Rock - Soda Mountain 6089 Ft Elev
    Pilot Rock Cascade-Siskiyou BLM BLM archives Rising 570 ft to an elevation of 5910 ft., Pilot Rock is perhaps the most striking feature of Cascade- Siskyou National Monument. Visible from much of the Shasta Valley in northern California and parts of Oregon’s Rogue Valley, the Rock serves as a friendly beacon to some five million vehicles and their passengers that travel the I-5 corridor annually. Competing Theories Pilot Rock is part of the Cascade Range, a mountain Put simply, a “plug” is an intrusive body formed by mag- range notable for its string of volcanic peaks stretching ma which cooled underground and was later exposed by from British Columbia to northern California’s Lassen erosion. Peak. The Monument’s proclamation refers to Pilot Rock as “a volcanic plug,” describing it as “a remnant of a Recent Research feeder vent left after a volcano eroded away, leaving an Recent research regarding Pilot Rock suggests that 25 outstanding example of the inside of a volcano.” Pilot million years ago, magma oozed through a weak spot Rock is composed mostly of volcanic andesite and has in the earth’s crust, but did not reach the surface. As a sheer, vertical faces with classic columnar jointing created result, some geologists refer to Pilot Rock as technically by the cooling of its andesite composition. a “volcanic plug,” but NOT as defined in the Monument’s proclamation. (The proclamation evidently uses “plug” Plug or a Neck or both? and “neck” interchangeably.) However “plugs”and Many geologists use the terms “neck” and “plug” in- “necks” are defined, what they both have in common is terchangeably, while others believe the terms apply to erosion.
    [Show full text]
  • Ashland Ranger District Rogue River National Forest APPENDICES
    'L-JCUMENU A 13.66/2: B 42x/APP./c.4 I V 0) C) oa)4e EN D\ Ashland Ranger District Rogue River National Forest APPENDICES APPENDIX A: KEY ISSUES & KEY QUESTIONS APPENDIX B: FIRE Identification of Specific Vegetation Zones for the Bear Watershed Analysis Area Fire Behavior Fuel Model Key Fuel Model Assignments Chronology of Events APPENDIX C: GEOLOGY, GEOMORPHOLOGY & SOILS Geology and Geomorphology of the Bear Watershed Analysis Area Characteristics of Soil Productivity APPENDIX D: HYDROLOGY What Sort of Debris is Transported Stream Classification Bibliography of Water Quality Studies Map: Drainageways Crossed Map: Dominant Precipitation Patterns APPENDIX E: FISHERIES Historic and Current Miles of Fish Habitat River Mile Index APPENDIX F: AQUATIC AND RIPARIAN HABITAT Habitat Comparison Chart Relative Comparison of Stream Gradients With Coarse Woody Debris Historic and Current Conditions for Aquatic Processes and Functions Maps: Reach Breaks of Neil Creek, West Fork & East Forks of Ashland Creek Table: Processes & Human Influences on Aquatic and Riparian Ecosystems Map: U.S. Fish & Wildlife Surveyed Wetlands Map: Supplemental Water Distribution System Broad Level Delineation of Major Stream Types (Rosgen) Delineative Criteria for Major Stream Types (Rosgen) APPENDIX G: HERITAGE RESOURCES Cultural Uses in the Bear Watershed Analysis Area Chronology of Important Dates APPENDIX A I KEY ISSUES & KEY QUESTIONS Key Questions IMPORTANT TO REMEMBER: These questions drive the analysis for Chapter II: Historic and Current Conditions and Future Trends. CLIMATE Identification of the atmospheric/climate regimes under which the ecosystem of the Bear Watershed Analysis Area have developed is important to this analysis. Attributes to be discussed in this analysis include periods of flood and drought, storm patterns in the winter and summer, occurrence of severe lightning and wind storms, rain on snow events, etc.
    [Show full text]
  • 3D Ichnofabrics in Shale Gas Reservoirs
    3D ICHNOFABRICS IN SHALE GAS RESERVOIRS By @ Małgorzata Bednarz A thesis submitted to the School of Graduate Studies in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Earth Sciences Memorial University of Newfoundland October 2014 St. John’s Newfoundland Abstract This PhD research project uses three-dimensional ichnology to address issues of shale- hydrocarbon reservoir quality and provides new tools for ichnofabric analysis and ichnotaxonomic considerations. The study presents deterministic (devoid of conceptual simplifications and interpretations) visualizations of the true spatial geometry of the aff. Chondrites, aff. Phycosiphon and Nereites trace fossils and models the three-dimensional arrangements of the burrow components. The volumetric reconstructions of the real geometry of the trace fossils allowed for their comparison with the previously established visualizations and for reconsideration of pre-existing palaeobiological models. To date three-dimensional understanding of the majority of trace fossils is presented as conceptual drawings available only on two-dimensional media. Such reconstructions are extrapolated mainly from observations of cross sections of burrows from core and outcrop and do not allow for realistic volumetric quantification and full elucidation of complex trace fossil geometries in the context of the host-sediment. The new methodology based on precise serial grinding and volume-visualization presented herein addresses this gap in ichnological knowledge, and is especially useful for examination of the ichnofabric contained in mudstones and muddy siltstones where the application or non-destructive methods of 3D reconstructions as CT scanning or MRI is impossible owing to the rock petrological characteristics (e.g., low burrow-matrix density difference).
    [Show full text]
  • 12. Bioturbation and Trace Fossils in Deep Sea Sediments of the Walvis Ridge, Southeastern Atlantic, Leg 741
    12. BIOTURBATION AND TRACE FOSSILS IN DEEP SEA SEDIMENTS OF THE WALVIS RIDGE, SOUTHEASTERN ATLANTIC, LEG 741 Dieter K. Fütterer, Geologisch-Palàontologisches Institut der Universitàt Kiel, D-2300 Kiel, Federal Republic of Germany ABSTRACT Trace fossil distribution present in pelagic carbonates cored on the Walvis Ridge during Deep Sea Drilling Project Leg 74 are described. A characteristic deep-sea trace fossil assemblage comprising the cosmopolitan ichnogenera Planolites, Chondrites, Zoophycos, and Teichichnus was found at paleo-water-depths ranging from a few hundred to about 4500 m. Paleodepth distribution indicates that Zoophycos has changed its environmental preference from relatively shallow water in the Cretaceous into deeper water in the late Paleocene. Thus Zoophycos can be used as a paleodepth indicator in the bathyal environment if its stratigraphic age is known. INTRODUCTION Cretaceous age. Normal subsidence of the Walvis Ridge produced paleodepth core profiles passing from rela- Bioturbation is the churning, stirring, and reworking tively shallow initial paleo-water-depths continuously to of a sediment by bottom-dwelling benthic organisms. In their present-day positions, which are in some cases most cases it obliterates primary sedimentary structures 2000 m deeper. and thus any information on the environmental con- Continuous coring by the hydraulic piston corer ditions during sedimentation. Increasing bioturbation (HPC) produced very good recovery and only minor eventually results in a nearly complete homogenization drilling disturbance in the unconsolidated sediments. of the sediment. These prerequisites offered an ideal opportunity to col- However, distinctly shaped sedimentary features pro- lect continuous data on the distribution of trace fossils duced by the activity of bottom-dwelling organisms through time and to relate those data to systematic (known as trace fossils, ichnofossils, or lebensspuren) changes in water depths in the open ocean.
    [Show full text]
  • Faculty Publications and Presentations 2010-11
    UNIVERSITY OF ARKANSAS FAYETTEVILLE, ARKANSAS PUBLICATIONS & PRESENTATIONS JULY 1, 2010 – JUNE 30, 2011 Table of Contents Bumpers College of Agricultural, Food and Life Sciences………………………………….. Page 3 School of Architecture…………………………………... Page 125 Fulbright College of Arts and Sciences…………………. Page 133 Walton College of Business……………………………... Page 253 College of Education and Health Professions…………… Page 270 College of Engineering…………………………………... Page 301 School of Law……………………………………………. Page 365 University Libraries……………………………………… Page 375 BUMPERS COLLEGE OF AGRICULTURE, FOOD AND LIFE SCIENCES Agricultural Economic and Agribusiness Alviola IV, P. A., and O. Capps, Jr. 2010 “Household Demand Analysis of Organic and Conventional Fluid Milk in the United States Based on the 2004 Nielsen Homescan Panel.” Agribusiness: an International Journal 26(3):369-388. Chang, Hung-Hao and Rodolfo M. Nayga Jr. 2010. “Childhood Obesity and Unhappiness: The Influence of Soft Drinks and Fast Food Consumption.” J Happiness Stud 11:261–275. DOI 10.1007/s10902-009-9139-4 Das, Biswa R., and Daniel V. Rainey. 2010. "Agritourism in the Arkansas Delta Byways: Assessing the Economic Impacts." International Journal of Tourism Research 12(3): 265-280. Dixon, Bruce L., Bruce L. Ahrendsen, Aiko O. Landerito, Sandra J. Hamm, and Diana M. Danforth. 2010. “Determinants of FSA Direct Loan Borrowers’ Financial Improvement and Loan Servicing Actions.” Journal of Agribusiness 28,2 (Fall):131-149. Drichoutis, Andreas C., Rodolfo M. Nayga Jr., Panagiotis Lazaridis. 2010. “Do Reference Values Matter? Some Notes and Extensions on ‘‘Income and Happiness Across Europe.” Journal of Economic Psychology 31:479–486. Flanders, Archie and Eric J. Wailes. 2010. “ECONOMICS AND MARKETING: Comparison of ACRE and DCP Programs with Simulation Analysis of Arkansas Delta Cotton and Rotation Crops.” The Journal of Cotton Science 14:26–33.
    [Show full text]
  • Meteorite Flux to Earth in the Early Cretaceous As Reconstructed from Sediment-Dispersed Extraterrestrial Spinels
    Meteorite flux to Earth in the Early Cretaceous as reconstructed from sediment-dispersed extraterrestrial spinels Birger Schmitz1,2*, Philipp R. Heck2, Walter Alvarez3,4, Noriko T. Kita5, Surya S. Rout2, Anders Cronholm1, Céline Defouilloy5, Ellinor Martin1, Jan Smit4,6, and Fredrik Terfelt1 1Astrogeobiology Laboratory, Department of Physics, Lund University, SE-22100 Lund, Sweden 2Robert A. Pritzker Center for Meteoritics and Polar Studies, The Field Museum of Natural History, Chicago, Illinois 60605, USA 3Department of Earth and Planetary Science, University of California, Berkeley, California 94720, USA 4Osservatorio Geologico di Coldigioco, Contrada Coldigioco 4, 62021 Apiro, Italy 5WiscSIMS, Department of Geoscience, University of Wisconsin–Madison, Madison, Wisconsin 53706, USA 6Department of Sedimentary Geology, Vrije Universiteit, 1081 HV Amsterdam, Netherlands ABSTRACT to 470 ± 6 Ma (Korochantseva et al., 2007), but the most precise relative We show that Earth’s sedimentary strata can provide a record of date is given by an abrupt two-orders-of magnitude increase worldwide the collisional evolution of the asteroid belt. From 1652 kg of pelagic in sand-sized L-chondritic chromite grains in mid-Ordovician sediments Maiolica limestone of Berriasian–Hauterivian age from Italy, we (Schmitz et al., 2003; Heck et al., 2016). recovered 108 extraterrestrial spinel grains (32–250 μm) represent- By dissolving 100-kg-sized samples of condensed sediments from ing relict minerals from coarse micrometeorites. Elemental and three different time periods in various acids, the highly refractory extraterres- oxygen isotope analyses were used to characterize the grains, provid- trial spinel minerals can be concentrated. The recovered grains typically ing a first-order estimate of the major types of asteroids delivering contain high concentrations of solar-wind noble gases, indicating that material at the time.
    [Show full text]
  • Field Trip Guide to the Upper Cretaceous Hornbrook Formation and Cenozoic Rocks of Southern Oregon and Northern California Field
    Field Trip Guide to the Upper Cretaceous Hornbrook Formation and Cenozoic Rocks of southern Oregon and northern California Students in SOU’s field geology course examining sandstones of the Rocky Gulch Member of the Hornbrook Formation near Hilt, California. Field Trip Leader: Bill Elliott Department of Geology, Southern Oregon University Saturday, September 8, 2007 Introduction The Klamath Mountains are an elongated north-trending geological province that occupies approximately 19,000 km2 in southwestern Oregon and northern California. The Klamath Mountains are made-up of numerous terranes that accreted during the Antler (Devonian), Sonoman (Permian to Late Triassic), and Nevadan (Jurassic to Early Cretaceous) orogenies (Mortimer, 1984). These terranes have been grouped into four metamorphic belts, from oldest (east) to youngest (west): Eastern Klamath Belt; Central Metamorphic; Western Paleozoic and Triassic; and Western Jurassic (Irwin, 1966; Irwin, 1994). In the Late Jurassic to Early Cretaceous, numerous magma bodies intruded the Klamath Mountains, including the Jurassic Mt. Ashland pluton and Early Cretaceous Grants Pass pluton (Hotz 1971; Gribble et al., 1990). During the Late Jurassic to Early Cretaceous, a subduction zone complex and forearc basin developed along the western margin of North America while folding and thrusting of Paleozoic and lower Mesozoic rocks associated with the Sevier orogeny triggered the formation of the Cordilleran foreland basin in the interior of North America (Figs. 1 and 2). The Hornbrook Formation (Upper Cretaceous) consists of a sequence of dominantly marine clastic sedimentary rocks about 1,200 meters thick exposed along the northeastern margin of the Klamath Mountains in southwestern Oregon to northern California (Fig.
    [Show full text]
  • Northwest Regional Conference Brochure
    The Oregon Trail State Volkssporting Association and Rogue Oregon Trail State Volkssporting Valley Walkers proudly invite you to attend the 25-28 June 2020 Northwest Regional Conference in Medford, Oregon. This fun event Association and Rogue Valley Walkers will provide a daily featured walk in Ashland, Jacksonville, Medford, Proudly present the 25-28 June 2020 and Casey State Park. Also offered are 3 self-guided challenge hikes Northwest Regional Conference in the Rogue River Gorge, Grizzly Peak, and Mount Ashland Meadows, a peaceful bike along the Bear Creek Greenway and a in Medford, Oregon swim. To enhance your experience, the Rogue River Walkers will ➢ 4 Featured Walks/3 Challenge Hikes/Bike/Swim have all 12 of their year round event directions and stamps available • Forest Therapy with Shakespeare, Ashland at the Inn throughout the conference. All sporting events are open to • Gold Mining Trails and Town, Jacksonville the public for a small $3.00 participation fee. No dogs allowed in • Medford Regional Director’s Meander, Medford Ashland’s Lithia Park. Wear hats, sunscreen and take water with you. • Casey State Park Caper Registration: Pre-registration required by 31 May 2020. Pre- • 3 Challenge Hikes in Rogue River Gorge, Grizzly Peak, registered walkers will be able to check in after noon on Wed, 24 Jun and Mount Ashland Meadows 2020 in the lobby of the Inn at the Commons. All other registration will • Bike along Bear Creek Greenway/Swim at pool be 7:00-4:00 Thu-Sat, 7:00-noon Sun. ➢ 12 nearby Rogue River Valley year round events ➢ Meet and Greet Social (Thursday) Meet and Greet: Thu, 25 Jun 2020, 4:30-6:00, light appetizers, and ➢ 4 Training Sessions (Friday) no host bar in The Meadows, Inn at the Commons.
    [Show full text]
  • Protecting Objects of Scientific Interest in the Cascade-Siskiyou National Monument: Status, Threats and Management Recommendations
    Protecting Objects of Scientific Interest in the Cascade-Siskiyou National Monument: Status, Threats and Management Recommendations Compiled and Edited by Dennis C. Odion Odion Botanical Consulting and University of California, Santa Barbara and Evan J. Frost Wildwood Environmental Consulting Ashland, OR December 2002 1 Protecting Objects of Scientific Interest in the Cascade-Siskiyou National Monument: Status, Threats and Management Recommendations Compiled and Edited by Dennis C. Odion Odion Botanical Consulting, and University of California, Santa Barbara and Evan J. Frost Wildwood Environmental Consulting Ashland, OR Prepared for the World Wildlife Fund Klamath-Siskiyou Regional Program Ashland, OR This project was supported by funds generously provided to the World Wildlife Fund from the Wyss Foundation, Bullitt Foundation, and Wilburforce Foundation Protecting Objects of Scientific Interest in the Cascade-Siskiyou National Monument 2 TABLE OF CONTENTS Introduction . .3 Summary Table . 5 I. Plant Species and Communities Vegetation Patterns, Rare Plants and Plant Associations, by Richard Brock . 8 Mixed Conifer Forests, with an Emphasis on Late-Successional / Old-Growth Conditions, by Dominick A. DellaSala . 25 Chaparral and Other Shrub-Dominated Vegetation, by Dennis C. Odion . 38 II. Fish and Wildlife Species Birds of the Cascade-Siskiyou National Monument, by Pepper W. Trail . 42 Peregrine Falcons, by Joel E. Pagel . 53 Butterflies and Moths, by Erik Runquist . 57 Aquatic Environments and Associated Fauna, by Michael S. Parker . 69 III. Key Ecosystem Processes Fire as an Object of Scientific Interest and Implications for Forest Management, by Evan J. Frost and Dennis C. Odion . 76 Landscape and Habitat Connectivity as an Object of Scientific Interest, by Dominick A.
    [Show full text]
  • Ichnological Analysis of the Bidart and Sopelana Cretaceous/Paleogene (K/Pg) Boundary Sections (Basque Basin, W Pyrenees): Refining Eco-Sedimentary Environment
    Sedimentary Geology 234 (2011) 42–55 Contents lists available at ScienceDirect Sedimentary Geology journal homepage: www.elsevier.com/locate/sedgeo Ichnological analysis of the Bidart and Sopelana Cretaceous/Paleogene (K/Pg) boundary sections (Basque Basin, W Pyrenees): Refining eco-sedimentary environment F.J. Rodríguez-Tovar a,⁎, A. Uchman b, X. Orue-Etxebarria c, E. Apellaniz c, Juan I. Baceta c a Departamento de Estratigrafía y Paleontología, Facultad de Ciencias, Universidad de Granada, 18002 Granada, Spain b Jagiellonian University, Institute of Geological Sciences, Oleandry Str. 2a, PL-30-063 Kraków, Poland c Departamento de Estratigrafía y Paleontología, Facultad de Ciencia y Tecnología, Universidad del País Vasco, E-48080 Bilbao, Spain article info abstract Article history: Ichnological analysis of two Cretaceous–Paleogene boundary sections at Bidart (SE France) and Sopelana (N Received 12 August 2010 Spain) has been conducted in order to refining eco-sedimentary environment, and to a make comparison with Received in revised form 23 October 2010 previous interpretations based on microfossils. In both sections, trace fossil assemblage is low diverse, Accepted 22 November 2010 consisting of Chondrites, Planolites, Thalassinoides, Trichichnus, Zoophycos, and ?Phycosiphon, ascribed to the Available online 1 December 2010 Zoophycos ichnofacies, however, with distinct differences. In the Bidart section, early Danian dark-filled trace Editor: M.R. Bennett fossil assemblage is more abundant in large Thalassinoides, Zoophycos and larger Chondrites, and less abundant in Trichichnus and small Chondrites in comparison to the Sopelana section. Sopelana is thus interpreted as a Keywords: more offshore, deeper section than Bidart although both were located in the upper bathyal zone of the basin.
    [Show full text]
  • Siskiyou Summit Handbell Conference Class Offerings
    Siskiyou Summit Handbell Conference Class Offerings BE PREPARED! Score Preparation is the foundation for all you do as a ringer and a director! Ringers and directors of all skill levels will be guided through the steps of score preparation and study. Learn to see the score as more than just notes on the page. Be a total musician! Workshop Leader: Elizabeth Mays BRONZE COFERENCE CHOIR: Can’t get enough ringing and are comfortable ringing Level 4 music apply for the BCC. Rehearsals begin Friday afternoon at 4pm. Conductor: Ellie Hodder KEEP YOUR BATTERY CHARGED (B4C5‐AB5): Ringers in the Battery are the core of the handbell ensemble requiring that the they be aware of what is happening around them and the knowledge to respond musically to the melody line or rhythm section. Learn the ins and outs of ringing in the battery and the techniques you can apply to enhance your musicality. Workshop Leader: Diane Barnes THE MORE YOU KNOW THE MORE YOU CAN DO: Learn to adapt Weaving and 4‐in‐ Hand skills in all handbell ringing. Although these techniques often are referred to as “Solo or Small Ensemble Techniques,” the mastery of these techniques is useful in full‐ choir settings as it enables ringers to negotiate complex passages with ease, grace and musicality. This class assumes that the student has a basic knowledge of the Weaving and 4‐in‐Hand skills. Workshop Leader: Elizabeth Mays SPECIAL TECHNIQUES: DOTS, PLUSES, and ARROWS, OH MY: Come explore what all those extra symbols in your music mean and how to play them in a manner that is safe for your body, safe for your bells and ads to the musicality of the piece.
    [Show full text]