Geologic Map of the Lassen Peak, Chaos Crags, And
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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. -
Loomis Visitor Center Loomis Museum Manzanita Lake Visitor
Form 10-306 STATE: UNITED STATES DEPARTMENT OF THE INTERIOR (Oct. 1972) NATIONAL PARK SERVICE California COUNTY: NATIONAL REGISTER OF HISTORIC PLACES Shasta INVENTORY - NOMINATION FORM FOR NFS USE ONLY FOR FEDERAL PROPERTIES ENTRY DATE (Type all entries - complete applicable sections) COMMON: Loomis Visitor Center Manzanita Lake Visitor Center Loomis Museum Manzanita Lake Museum AND/OR HISTORIC: Mae Loomis Memorial Museum STREET AND NUMBER: Building 43 CITY OR TOWN: Manzanita Lake, CONGRESSIONAL DISTRICT: Lassen Volcanic National Park STATE: COUNTY: California 06 Shasta 089 CATEGORY ACCESSIBLE OWNERSHIP STATUS CChec/c One) TO THE PUBLIC District Building |5T| Public Public Acquisition: fX] Occupied Yes: z Site Structure | | Private ||In Process | | Unoccupied |~~] Restricted o d] Object Q] Both |~~| Being Considered | | Preservation work [~] Unrestricted in progress SN.O H u PRESENT USE (Check One or More as Appropriate) | | Agricultural (jg Government C] Park | | Transportation | | Comments | | Commercial [""I Industrial Q Private Residence Q Other (Specify.) ^CJ3 Educational Q Military | | Religious | | Entertainment useum [ | Scientific Ul 111 Lassen Volcanic National Park, U.S. National Park Service REGIONAL HEADQUARTERS: (If applicable) STREET AND NUMBER: Western Region_____________ 450 Golden Gate Avenue Cl TY OR TOWN: STATE: H San Francisco California 06 > COURTHOUSE, REGISTRY OF DEEDS, ETC: Shasta County Courthouse co 2 STREET AND NUMBER: CITY OR TOWN: Redding California 06 TITLE OF SURVEY: DATE OF SURVEY: Federal State Catfnty •-,/ ••—— DEPOSITORY FOR SURVEY RECORDS: er-, €£» STREET AND NUMBER: W Cl TY OR TOWN: (Check One) llent Good |~| Deteriorated [~1 Ruins [~~| Unexposed CONDITION (Check One) (Check One,) Altered [jg Unaltered Moved jg[] Original Site Exterior The Loomis Museum is a building of rustic appearance constructed of a gray, native volcanic rock with cut face random ashlar masonry. -
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. -
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 -
Sampling of Great Year Round Attractions Found in Redding and Shasta Cascade
SAMPLING OF GREAT YEAR ROUND ATTRACTIONS FOUND IN REDDING AND SHASTA CASCADE Any Adventure, Any Day awaits those who visit Redding and Shasta Cascade. Whether your idea of a great vacation means extreme outdoor adventure, family-friendly activities, or cultural excursions, Redding and Shasta Cascade are filled with year-round unexpected pleasures. Land lovers can explore Redding through its expansive and nationally-recognized trails system, where visitors walk, hike, bike, or horseback ride their way to adventure. If you prefer playing in the water or floating on top, Redding’s access to several rivers and lakes allows for boating, paddle-boarding, rafting, swimming, and fishing on the Sacramento River, or at nearby Whiskeytown and Shasta Lakes. There are so many great things to do and see all year long in this breathtaking region, you’ll soon understand why visitors come back again and again. SUNDIAL BRIDGE This one-of-a-kind, glass decked pedestrian bridge serves as an incredible entrance to Redding’s Sacramento River National Recreation Trail. World-renowned Spanish architect, Santiago Calatrava, conceived the unique design of the bridge. It is the first bridge of its kind in the United States, and is the tallest working sundial in the world! The massive 217 foot pylon leans due north and functions as the gnomon of a sundial, casting its giant shadow on a garden- bordered dial plate at the bridge’s north end. The suspension, cable-stayed design of the bridge does not have any footings in the river, out of respect for the nearby salmon-spawning habitat. Receptions under the bridge are available. -
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. -
LAVO Summer Guide 2020
National Park Service U.S. Department of the Interior Lassen Volcanic Guide Lassen Volcanic National Park Summer/Fall 2020 Be Prepared for Modifications to Services and Facilities Learn more about how Lassen Volcanic National Park is responding to COVID-19 and how you can recreate responsibly on page 13. Explore Your Park in... Four Hours One Day Two or More Days Half a day is just enough to enjoy A full day gives you time to enjoy More time provides the opportunity to several Highway Highlights multiple Highway Highlights enjoy longer hikes and a full day in one (pg 3) along the 30-mile road (pg 3) and at least one hike in the of the more remote areas of the park. that connects the northwest and Southwest or Manzanita Lake areas. southwest entrances. Plan one Hike Cinder Cone (pg 8) and marvel hour drive time without stops. Take a hike (pg 8-9). The most at the Painted Dunes and lava rock- popular trails in the park offer a lined Butte Lake. Take in the sights, sounds, variety of sights and experiences: and smells of Sulphur Works Lassen Peak (5 mi), Bumpass Hell Climb to the active fire lookout Hydrothermal area (pg 3). (3 mi), Kings Creek Falls (3 mi), atop Mt. Harkness (pg 9) and take a and Manzanita Lake Loop (1.8 mi). refreshing dip in Juniper Lake. Hike the Devastated Area Parking is limited: arrive early; go Interpretive Trail (pg 8) and uncover the dramatic story of the mid-week; or choose an equally Explore a remote hydrothermal area 1914-1915 Lassen Peak eruptions.