Lassen Volcanic National Park
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Plate Tectonics, Volcanoes, and Earthquakes / Edited by John P
ISBN 978-1-61530-106-5 Published in 2011 by Britannica Educational Publishing (a trademark of Encyclopædia Britannica, Inc.) in association with Rosen Educational Services, LLC 29 East 21st Street, New York, NY 10010. Copyright © 2011 Encyclopædia Britannica, Inc. Britannica, Encyclopædia Britannica, and the Thistle logo are registered trademarks of Encyclopædia Britannica, Inc. All rights reserved. Rosen Educational Services materials copyright © 2011 Rosen Educational Services, LLC. All rights reserved. Distributed exclusively by Rosen Educational Services. For a listing of additional Britannica Educational Publishing titles, call toll free (800) 237-9932. First Edition Britannica Educational Publishing Michael I. Levy: Executive Editor J. E. Luebering: Senior Manager Marilyn L. Barton: Senior Coordinator, Production Control Steven Bosco: Director, Editorial Technologies Lisa S. Braucher: Senior Producer and Data Editor Yvette Charboneau: Senior Copy Editor Kathy Nakamura: Manager, Media Acquisition John P. Rafferty: Associate Editor, Earth Sciences Rosen Educational Services Alexandra Hanson-Harding: Editor Nelson Sá: Art Director Cindy Reiman: Photography Manager Nicole Russo: Designer Matthew Cauli: Cover Design Introduction by Therese Shea Library of Congress Cataloging-in-Publication Data Plate tectonics, volcanoes, and earthquakes / edited by John P. Rafferty. p. cm.—(Dynamic Earth) “In association with Britannica Educational Publishing, Rosen Educational Services.” Includes index. ISBN 978-1-61530-187-4 ( eBook) 1. Plate tectonics. -
NOMINATION FORM for NPS USE ONLY for FEDERAL PROPERTIES ENTRY DATE (Type All Entries - Complete Applicable Sections) Rti^T Fl 1SP6
STATE: .Form Igd?6 UNITED STATES DEPARTMENT OF THE INTERIOR (Uct. IV/^J NATIONAL PARK SERVICE California COUNTY: NATIONAL REGISTER OF HISTORIC PLACES Shasta and Lassen INVENTORY - NOMINATION FORM FOR NPS USE ONLY FOR FEDERAL PROPERTIES ENTRY DATE (Type all entries - complete applicable sections) rti^T fl 1SP6 COMMON: Nobles' Emigrant Trail HS-1 AND/OR HISTORIC: Nobles' Trail (Fort Kearney, South Pass and Honey Lake Wagon Road) STREET AND NUMBER: M --"'' ^ * -X'"' '' J-- - ;/* ( ,: - "; ^ ;." ; r ^-v, % /'• - O1- - >,- ,•<•-,- , =••'"' CITY OR TOWN: / '-' j- ,. " ,-, ,, , CONG RESSIONAL DISTRICT: Lassen Volcanic National Park S econd STATE: CODE COUN TY: CODE California 06 Shaj3ta and Lassen 089/035 :. : ; STATUS ACCESSIBLE (Check?ATE,G SOne)R \ OWNERSHIP SIAIU3 T0 THE p UBL|c gf] District Q Building [ig Public Public Acquisition: [ | Occupied Yes: : : -Z Q Site | | Structure | | Private Q In Process PT"1 Unoccupied | | Restricted 0 [~~| Object Qj Both f~| Being Consider)sd Q Preservation work [X] Unrestricted in progress [~~] No u PRESENT USE (Check One or More as Appropriate) | | Agricultural jj£] Government [X] Park | | Transportation | | Comments h- I | Commercial Q2 Industrial [~~| Private Residence | | Other (SpeciM »/> Q Educational Q Military [~1 Religious ;; /. z [^Entertainment Q Museum f"| Scientific UJ STATE: »/> National Park Service REGIONAL HEADQUARTERS: (If applicable) SIr REET AND NUMBER: Western Region l^50 Golden Gate Avenue Cl TY OR TOWN: SIPATE: CODE San Francisco California Ub V BliBsi^iiiiBHIiiMMIiBlilBl^isMiM^Ml Illlllillliil^^ COURTHOUSE, REGISTRY OF DEEDS, ETC: COUNTY: STREET AND NUMBER: CITY OR TOWN: SIPATE: CODE Lassen Volcanic National Park California Ob toM^ TITLE OF SURVEY: The National Survey of Historic '&&& s^n^lt^J^aglix "Overland Migrations West of the Mississippi" TI AsX -X^ ENT^Y*"NUMBER o DATE OF SURVEY: 1959 [X] Federal Q State / ^yl County | _ | LocoilP' ^k X3 Z DEPOSITORY FOR SURVEY RECORDS: t) •j? in C OAHP, WASO c/> rj V?\ m STREET AND NUMBER: 'l - i H~*~! ^|T"-, r £;. -
Area Adventure Hat Creek Ranger District Lassen National Forest
Area Adventure Hat Creek Ranger District Lassen National Forest Welcome The following list of recreation activities are avail- able in the Hat Creek Recreation Area. For more detailed information please stop by the Old Station Visitor Information Center, open April - December, or our District Office located in Fall River Mills. Give Hat Creek Rim Overlook - Nearly 1 million years us a call year-around Mon.- Fri. at (530) 336-5521. ago, active faulting gradually dropped a block of Enjoy your visit to this very interesting country. the Earth’s crust (now Hat Creek Valley) 1,000 feet below the top of the Hat Creek Rim, leaving behind Subway Cave - See an underground cave formed this large fault scarp. This fault system is still “alive by flowing lava. Located just off Highway 89, 1/4 and cracking”. mile north of Old Station junction with Highway 44. The lava tube tour is self guided and the walk is A heritage of the Hat Creek area’s past, it offers mag- 1/3 mile long. Bring a lantern or strong flashlight nificent views of Hat Creek Valley, Lassen Peak, as the cave is not lighted. Sturdy Shoes and a light Burney Mountain, and, further away, Mt. Shasta. jacket are advisable. Subway Cave is closed during the winter months. Fault Hat Creek Rim Fault Scarp Vertical movement Hat Creek V Cross Section of a Lava Tube along this fault system alley dropped this block of earth into its present position Spattercone Trail - Walk a nature trail where volca- nic spattercones and other interesting geologic fea- tures may be seen. -
Sulphur Works Is Believed to Have Been the Main Vent for Mount Tehama, a Stratovolcano That Started Erupting About 600,000 Years Ago
Junior Park Explorer Lassen Volcanic National Park Mystery of Mount Tehama Imagine you are standing almost a mile deep inside a stratovolcano. Well, 400,000 years ago you would have been! The area around Sulphur Works is believed to have been the main vent for Mount Tehama, a stratovolcano that started erupting about 600,000 years ago. By 400,000 years ago, it had reached its full height of 11,500 feet. Look around you in a full circle. Can you spot the mountains pictured below? They are all remnants (left over bits) of Mount Tehama. Remnant 1 – Brokeoff Mountain Remnant 2 – Mount Diller Remnant 3 – Pilot Pinnacle Remnant – Mount Conard Activity 1 - See if you can find these remnants on your park map. Trace a circle from one mountain to the next to outline the footprint of Mount Tehama. Be sure to include Little Hot Springs Valley inside the footprint. Activity 2 - Use the diagram on the next page to reconstruct Mount Tehama. Connect point A to point B, A to C, A to D, A to E, & A to F, individually. Can you see Mount Tehama in your imagination? Color in the mountain if you wish. Activity 3 - Another way to reconstruct Mount Tehama is as a view from down in the Sacramento Valley. On the next page, check out how the skyline of Lassen Volcanic National Park looks today, looking east from near Redding. Can you draw what the skyline might have looked like when Mount Tehama was at its full height of 11,500 feet, 400,000 years ago? Use the graph on the next page. -
Apinos, Open-File Report 83-400 This Report Is Preliminary and Has Not
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY The Volcano Hazards Program: Objectives and Long-Range P 1ans R. A. Bailey, P. R, Beauchemln, F, P. ~apinos, and D. W. Klick. Open-File Report 83-400 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. - - Reston 1983 TABLE OF CONTENTS Page I. Introduction 1 General Assessment of the Potential for Future Eruptions A. Mount St. Helens B. Other Cascade Volcanoes C, Other Western Conterminous U.S. Volcanoes D. Hawaii an Volcanoes E. Alaskan Volcanoes 111. Program bals, Objectives, and Components A. Volcanic Hazards Assessment B. Volcano Monitoring C. Fundamental Research 0. Emergency-Response Planning and Public Education IV. A Long-Range Volcano Hazards Program A. Funding his tor.^ B. General Objectives C. Specific Objectives D. Plans for Studies E. Resources F. International Cooperat ion V. The Federal Role 3 1. A. Public Need for Information about Impending 31 Volcanic Hazards B. Interstate Implications of Volcanic Disasters 32 C. Disruption of Regional and National Economies 32 0. Implication for Federal Lands 33 E. Mitigation of Subsequent Federal Disaster Assistance Costs 33 F. Need for an Integrated Research Program 33 Figure 1, Location of Potentially Hazardous Volcanoes in the U.S. 4 e Figure 2, History of Cascades Volcanism, 1800-1980 6 THE VOLCANO HAZARDS PROGRAM: OBJECTIVES AN0 LONG-RANGE PLANS I. INTRODUCTION Volcanoes and the products of volcanoes have a much greater impact on people and society than is generally perceived. Although commonly destructive, volcanic eruptions can be spectacularly beautiful and, more importantly, they have produced the very air we breathe, the water we drink, and our most fertile soils. -
Lassen Domefield Telephoto View from Parhams Point on Hat Creek Rim (Old Station Quadrangle)
May 19–20, 1915 flow upper Devastated Area Crescent Lassen dacite of Crater Peak Hill 8283 tuff cone of Raker Peak rhyodacite of Chaos Crags Krummholz Chaos Crags Mount Diller Chaos Crags dome E dome B dome F Domes of Sunflower Flat andesite of Raker Peak Hat Creek Hat Creek andesites of Badger Mountain Lassen domefield Telephoto view from Parhams Point on Hat Creek Rim (Old Station quadrangle). Remnants of the northeast lobe of the dacite flow of May 19–20, 1915 (unit d9) are exposed in the notch at the top of Lassen Peak, above the Devastated Area. The original blocky carapace of Lassen Peak (unit dl, 27±1 ka) has been removed by glaciation, whereas a blocky carapace is preserved on the unglaciated domes of Chaos Crags (units rcb, rce and rcf, 1,103±13 yr B.P.). Forested slopes in front of the domes of Chaos Crags are the rhyodacite domes of Sunflower Flat (unit rsf, 41±1 ka). Mount Diller is a remnant of the Brokeoff Volcano (590–390 ka). The slopes in front of Mount Diller, between Chaos Crags and Lassen Peak, are underlain primarily by the rhyodac- ite dome and flow of Krummholz (unit rkr, 43±2 ka, part of the Eagle Peak sequence) and the dacite of hill 8283 (unit d82, 261±5 ka, part of the Bumpass sequence) and are mantled by tephra of the Chaos Crags eruptions (unit pc, 1,103±13 yr B.P.). Crescent Crater (unit dc, 236±1 ka) is also part of the Bumpass sequence. Raker Peak is the vent for the andesite of Raker Peak (unit arp, 270±18 ka), part of the older Twin Lakes sequence. -
Earth Science Teaching Curriculum
Earth Science for Secondary Schools Earth Science Teaching Curriculum By Chelsea DeVries Brent G. Hallock Advisor California Polytechnic State University Earth and Soil Sciences Department San Luis Obispo 2010 Approval Page TITLE: Earth Science for Secondary Schools AUTHOR: Chelsea D. DeVries DATE SUBMITTED: December 8, 2010 Brent G. Hallock Senior Project Advisor Signature Dr. Lynn Moody Department Chair Signature i Acknowledgments • I want to thank Dr. Moody and Dr. Hallock for being so kind, supportive, helpful, and PATIENT with me through my journey at Cal Poly. I may never have made it without them!!!! • I also want to thank my loving parents, for knowing exactly what to say every time I wanted to give up. • I want to thank my lovely husband-to-be, for being the rock I needed to stand on when I felt like I was in sinking sand. • Lastly, but DEFINETLY not least, I want to thank Katherine O’Clair and Debra Leopard for helping me with all the “computer stuff.” • I am very grateful the Internet, books, and journals that were used to complete this project. Please refer to the resources page when any picture, photograph, or chart is listed. ii Table of Contents Table of Contents Page Tile Page Approval Page i Acknowledgements ii Table of Contents iii Abstract 1 Introduction 2 Material and Methods 3 Results 7 Resources 82 Appendix 85 ***Power Point Presentations included on CD iii Abstract Creating this senior project, based on secondary Earth Science curriculum, will be directed toward teachers and will assist in lessons and instruction and reaching students at a deeper level. -
Talus Fabric, Clast Morphology, and Botanical Indicators of Slope Processes on the Chaos Crags (California Cascades), U.S.A
Document generated on 09/27/2021 5:20 a.m. Géographie physique et Quaternaire Talus fabric, clast morphology, and botanical Indicators of Slope Processes on the Chaos Crags (California Cascades), U.S.A. Relevés botaniques, granulométrie, forme et organisation des débris sur les talus d'éboulis en tant qu'indicateurs des processus dans les Chaos Crags (monts Cascades, Californie, U.S.A.). Morfología y orientación de derrubios clásticos, e indicadores botánicos de procesos de pendiente en Chaos Crags (Cascades, California) Francisco L. Pérez Volume 52, Number 1, 1998 Article abstract The Chaos Crags, a group of dacite domes in the Cascades Mtns (California), URI: https://id.erudit.org/iderudit/004861ar were affected by volcanic debris avalanches ca. 1675 A.D.; these left a sizable DOI: https://doi.org/10.7202/004861ar deposit and a scar on the north mountain flank, now covered by talus. This report examines the fabric and morphology of talus debris, their spatial See table of contents variation, and the geomorphic processes presently affecting the slope. The talus presents a bi-segmented profile with a steep upper rectilinear segment and a shorter concave, basal zone. Debris are sorted by size both along (larger Publisher(s) clasts downslope) and across the talus (larger particles below the cliffs). Shape sorting is weaker, but clast sphericity increases, and elongation decreases, Les Presses de l'Université de Montréal toward the footslope. Upper-talus fabrics (long axes parallel to talus plane and slope) show that clasts there move by sliding, while basal blocks are deposited ISSN by rockfall, which causes more iso- tropic fabrics. -
Lassen Volcanic National Park Created California
LASSEMHVOLCAN«C !B8& UNITED STATES Historic Events DEPARTMENT OF THE Lassen INTERIOR OPENING Harold L. Ickes, Secretary AND CLOSING Volcanic 1820 Arguello exploring party first to record DATES DEPEND and name Lassen Peak (St. Joseph's UPON NATIONAL PARK Mountain). 19 40 WEATHER CALIFORNIA CONDITIONS 1850-51 Last lava flow from Cinder Cone. LASSEN PEAK, WITH LAKE HELEN NATIONAL PARK SERVICE IN FOREGROUND Arno B. Cammerer, Director C OJ^TEU^TS 1864 Helen Brodt, first white woman to climb Lassen Peak, made ascent with Major Reading. Lake Helen named for Eruption of Lassen Peak her. 1 in 1915 Cover ASSEN VOLCANIC NA GEOLOGIC HISTORY TIONAL PARK, in northeast The Cascade Range, which is vol Geologic History .... 3 ern California, was created by canic in origin, is not ancient, measured 1906 May 6. Lassen Peak and Cinder Cone L Lassen Peak and Vicinity . 3 act of Congress approved August 9, in geologic time. Its beginning dates National Monuments established. 1916, to preserve Lassen Peak and the back to the Pliocene period, about a Chaos Crags and Chaos area containing spectacular volcanic ex million years before the great ice age Jumbles 6 hibits which surrounds it. This impres or glacial epoch. The present range sive peak, from which the park derives rests upon a great platform of lava Ancestral Mount Tehama . 6 1914 May 30. First known eruption of Las sen Peak since coming of white man. its name, stands near the southern end flows, which issued from many vents Cinder Cone Area ... 7 of the Cascade Mountains and is the and fissures. -
Mafic-Felsic Magma Interaction at Satsuma-Iwojima Volcano, Japan
Earth Planets Space, 54, 303–325, 2002 Mafic-felsic magma interaction at Satsuma-Iwojima volcano, Japan: Evidence from mafic inclusions in rhyolites Genji Saito1, James A. Stimac2, Yoshihisa Kawanabe1, and Fraser Goff3 1Geological Survey of Japan, AIST, Central 7, Higashi 1-1-1, Tsukuba, Ibaraki 305-8567, Japan 2Philippine Geothermal, Inc., 12th Fl. Citibank Tower, 8741 Paseo de Roxas, Makati, Philippines 3EES-6, MS-D462, Los Alamos National Laboratory, Los Alamos, NM 87545, U.S.A. (Received January 9, 2001; Revised January 25, 2002; Accepted February 4, 2002) Geochemical and petrographic studies of the rhyolites and mafic inclusions from Satsuma-Iwojima volcano were carried out in order to investigate evolution of a silicic, bimodal magma system during the post-caldera stage. Abundant mafic inclusions, which are fine-grained with vesicles in their cores, are present in the Showa- Iwojima rhyolitic lava. Inclusions with similar textures are found in Iwodake volcanic bombs but are less common than in the Showa-Iwojima lava. The major and trace element compositions of the inclusions plot along mixing lines connecting the host rhyolites with spatially and temporally associated basaltic to basaltic andesite magmas. Plagioclase phenocrysts in the inclusions have a large variation in core compositions (An42 to An96), and exhibit various zoning profiles and reaction textures, indicating they coexisted with melts ranging from basaltic to rhyolitic composition. Pyroxenes also exhibit a wide range in composition and a variety of zoning patterns consistent with multiple sources. These results suggest that a stratified magma chamber exists beneath the volcano, consisting of a lower basaltic layer, an upper rhyolitic layer and an episodically-present, thin middle layer of andesite. -
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Index [Italic page numbers indicate major references] Abajo Mountains, 382, 388 Amargosa River, 285, 309, 311, 322, Arkansas River, 443, 456, 461, 515, Abort Lake, 283 337, 341, 342 516, 521, 540, 541, 550, 556, Abies, 21, 25 Amarillo, Texas, 482 559, 560, 561 Abra, 587 Amarillo-Wichita uplift, 504, 507, Arkansas River valley, 512, 531, 540 Absaroka Range, 409 508 Arlington volcanic field, 358 Acer, 21, 23, 24 Amasas Back, 387 Aromas dune field, 181 Acoma-Zuni scction, 374, 379, 391 Ambrose tenace, 522, 523 Aromas Red Sand, 180 stream evolution patterns, 391 Ambrosia, 21, 24 Arroyo Colorado, 395 Aden Crater, 368 American Falls Lava Beds, 275, 276 Arroyo Seco unit, 176 Afton Canyon, 334, 341 American Falls Reservoir, 275, 276 Artemisia, 21, 24 Afton interglacial age, 29 American River, 36, 165, 173 Ascension Parish, Louisana, 567 aggradation, 167, 176, 182, 226, 237, amino acid ash, 81, 118, 134, 244, 430 323, 336, 355, 357, 390, 413, geochronology, 65, 68 basaltic, 85 443, 451, 552, 613 ratios, 65 beds, 127,129 glaciofluvial, 423 aminostratigraphy, 66 clays, 451 Piedmont, 345 Amity area, 162 clouds, 95 aggregate, 181 Anadara, 587 flows, 75, 121 discharge, 277 Anastasia Formation, 602, 642, 647 layer, 10, 117 Agua Fria Peak area, 489 Anastasia Island, 602 rhyolitic, 170 Agua Fria River, 357 Anchor Silt, 188, 198, 199 volcanic, 54, 85, 98, 117, 129, Airport bench, 421, 423 Anderson coal, 448 243, 276, 295, 396, 409, 412, Alabama coastal plain, 594 Anderson Pond, 617, 618 509, 520 Alamosa Basin, 366 andesite, 75, 80, 489 Ash Flat, 364 Alamosa -
Geologic Map of Lassen Volcanic National Park and Vicinity, California by Michael A
Geologic Map of Lassen Volcanic National Park and Vicinity, California By Michael A. Clynne and L.J. Patrick Muffler Pamphlet to accompany Scientific Investigations Map 2899 Lassen Peak and the Devastated Area Aerial view of Lassen Peak and the proximal Devastated Area looking south. Area with sparse trees marks the paths of the avalanche and debris-flow deposits of May 19–20, 1915 (unitsw9 ) and the pyroclastic-flow and fluid debris-flow deposits of May 22, 1915 (unit pw2) (Clynne and others, 1999; Christiansen and others, 2002). Small dark crags just to right of the summit are remnants of the May 19–20, 1915, lava flow (unitd9 ). The composite dacite dome of Lassen Peak (unit dl, 27±1 ka) dominates the upper part of the view. Lithic pyroclastic-flow deposit (unitpfl ) from partial collapse of the dome of Lassen Peak is exposed in the canyon of the headwaters of Lost Creek in center of view. Ridges flanking central area are glacial moraines (unitQta ) thinly covered by deposits of the 1915 eruption of Lassen Peak (Christiansen and others, 2002). Small permanent snowfield is seen on the left lower slope of Lassen Peak. Area east of the snowfield is the rhyodacite lava flow of Kings Creek (unitrk , 35±1 ka, part of the Eagle Peak sequence). Dacite domes of Bumpass Mountain (unit db, 232±8 ka), Crescent Crater (unit dc, 236±1 ka), hill 8283 (unit d82, 261±5 ka), and Loomis Peak (unit rlm, ~300 ka) are part of the Bumpass sequence. Photograph by Michael A. Clynne. 2010 U.S. Department of the Interior U.S.