SIM 2899 Sheet 2

Total Page:16

File Type:pdf, Size:1020Kb

SIM 2899 Sheet 2 Scientific Investigations Map 2899 U.S. Department of the Interior Sheet 2 of 3 U.S. Geological Survey Pamphlet and CD-ROM accompany map GLACIAL, SEDIMENTARY AND HYDROTHERMAL DEPOSITS VOLCANIC CENTERS OF SOUTHERNMOST CASCADES 1917 C.E. p17 Phreatic deposit, May–June w2 Viscous debris-flow deposits, May 22 p2 Pumice-fall deposit, May 22 pw2 Pyroclastic-flow and associated fluid debris-flow deposits, May 22 Deposits of 1914–1917 eruption of Lassen Peak 1915 C.E. d9 Dacite flow, May 19–20 f9 Flood deposits, May 19–20 sw9 Avalanche and debris-flow deposits, May 19–20 p9 Pyroclastic deposit, May 19 CORRELATION OF MAP UNITS HEADNOTE d4 Dacite dome, May 14–19 [See Description of Map Units (pamphlet) for detailed unit descriptions and interpretation of unit ages; ages shown may be averages of several ages. See table 2 and references in unit descriptions for age analysis information. Fantastic mf2 Flow 2 Units of volcanic centers and the Caribou Volcanic Field are shown on colored backgrounds for emphasis. Sequences are groups of volcanoes related by lithology and age. Chains are sequences displaying conspicuous linear Lava Beds mf1 Flow 1 geometry. Indentations in left margin of Lassen Volcanic Center area indicate intercalations with glacial and surficial units. Age boundaries based on Gradstein and others (2005) and Walker and others, 2009. Paleomagnetic Basaltic andesites of Cinder Cone 1666 C.E. mp2 Flow 2 polarity (+, normal; -, reversed) boundaries based on Berggren and others (1995). C.E., Common Era. Unit age is left of unit box; unit name is right of unit box. Some unit boxes represent groups of units, such as the unit box Qsh Landslide h Hydro- ht Travertine Painted mp1 Flow 1 labeled bb, which is not a unit on the map. A note in parentheses to the right of the unit name shows that the box represents units bb1–bb6 and bb8–bb12. Colored arrows pointing up and down from unit boxes indicate the deposits in thermally Dunes mo Old Bench flow possible range in age of unit. See table 3 for alphabetical listing of map unit labels, as well as unit name, page number of unit description in pamphlet, unit age, location by heading in Correlation of Map Units, and quadrangle hydrothermally altered rocks 278±28 yr B.P. Qsj Avalanche deposits of Chaos Jumbles location in database] altered core of in active HOLOCENE Brokeoff thermal areas rcf Volcano Talus, emplaced pce Lithic pyroclastic-flow deposit from REGIONAL VOLCANIC ROCKS hot from rce partial collapse of dome E domes B–F pcd Lithic pyroclastic-flow deposit from Qf Alluvium Qc Colluvium cc Domes partial collapse of dome D and talus A–F rcd Rhyodacite of Chaos Crags rcc NORTH AND WEST OF LASSEN VOLCANIC CENTER SOUTH AND EAST OF LASSEN VOLCANIC CENTER REGIONAL VOLCANIC ROCKS OF THE CARIBOU AREA Qd Diatomite rcb rca 1,103±13 yr B.P. pc Pumiceous pyroclastic-flow Late Pleistocene volcanic rocks 3,310±55 yr B.P. and fall deposits ~8,000 yr B.P. Qwh Debris-flow deposits from the northeast side of Lassen Peak Qth Till or protalus-rampart debris ? 11.7 Qtal Late till of ka* Anklin Meadows a74 Andesite of hill 7416 atd Andesite of Devils Rock Garden Qta Till of Anklin Meadows Qoa Outwash gravel of Anklin Meadows Twin Lakes sequence, younger Twin Qcl Talus on Lassen Peak Qtrl Post-maximum till of Raker Peak consisting of Lassen Peak avalanche debris Eagle Peak sequence mtt Qty Till, younger Qoy Outwash Qou Outwash Qsl Avalanche debris from Lassen Peak spread across glacial ice Basaltic andesite of Turnaround Lake glaciations gravel, gravel, 24±6 ka bhc Hat Creek Basalt mrc Basaltic andesite of Red Cinder Cone Lithic pyroclastic-flow deposit younger undivided 27±1 ka pfl (tholeiitic) glaciations from partial collapse of dome Dacite of Lassen Peak dl Tumble brc Dome adb Andesite of Bidwell Spring Basalt of Red Cinder Cone Buttes Qtr Till of Raker Peak Qor Outwash gravel of Raker Peak chain 35.1±3.1 ka atb Andesite of Bear Wallow Butte mrr Basaltic andesite of Red Cinder mdp Basaltic andesite of Pole Spring Road rk Flows mt67 Basaltic andesite of hill 6770 Rhyodacite of Kings Creek 35±1 ka pk Pumiceous pyroclastic-flow deposits mt54 Basaltic andesite of hill 5410 Bidwell br80 Basalt of hill 8030 mtu Basaltic andesite md36 Basaltic andesite of section 36 rsf Domes of Tumble Buttes Spring Rhyodacite of Sunflower Flat chain brm Basalt of Cameron Meadow 41±1 ka psf Pumiceous pyroclastic-flow deposits mtb Basaltic andesite of Bear Wallow Butte Red Tuya 43±2 ka rkr Rhyodacite of Krummholz ah Andesite of Hat Mountain mt61 Basaltic andesite of hill 6138 bra Basalt of Ash Butte 46±7 ka ass Andesite of Sugarloaf Peak 46.3±3.4 ka bdt Basalt of Twin Buttes Cinder chains mt5 Basaltic andesite of section 5 chain ? ? mdb Basaltic andesites of Black Butte (Units 1–2) br22 Basalt of hill 2283 att Andesite of Tumble Buttes r27 Rhyodacite of section 27 mte Basaltic andesites mtm Basaltic andesite of Mud Lake ae Andesite of Eagle Peak br25 Basalt of section 25 ? of Evelyn Lake bk Tholeiitic basalts of 65±45 ka bbz Tholeiitic basalts of Big Lake (units 1–2) Sugarloaf 66±4 ka re 67±4 ka msl Basaltic andesite of Buzzard Springs Dome and flow chain 69±20 ka arr Andesite of Red Cinder Rhyodacite of Eagle Peak Lassen domefield Little Potato Butte bic Tholeiitic basalt of pe Pumiceous pyroclastic-flow deposits Ice Cave Mountain bre Basalt east of Ash Butte PLEISTOCENE LATE 77±11 ka asp mrd Basaltic andesite and andesite Andesite of Potato Butte meh Basaltic andesite brw Basalt of Widow Lake 82±14 ka mfp Basaltic andesite of Fairfield Peak of Red Lake Mountain ms47 Basaltic andesite of hill 4709 of Eskimo Hill mrg Basaltic andesites of Long Lake (Units 1–3) 93±13 ka ac Qtb Andesite of Crater Butte aso Andesites of Old Station 97.6±9.8 ka bc Basalts of Cone Lake Road (Units 1–2) Till of Badger Mountain mrm Basaltic andesite of Red Mountain mrb Basaltic andesite of Caribou Wilderness bcc Basalts of Cold 102.1±11.4 ka bg Basalts of old railroad grade (Units 1–4) brt Basalts of Triangle Lake (Units 1–2) Creek Butte 105.0±6.0 ka bp Basalts of Poison Butte (Units 1–6) ? mte Basaltic andesites 107.5±3.8 ka Basalts and basaltic andesites bb of Evelyn Lake 100.1±8.5 ka of Bogard Buttes (Units 1–6; 8–12) Poison 106.2±3.6 ka bpc Basalts of Pine Creek (Units 1–3) Lake Qto Till, older Qoo Qou Outwash gravel, 101.0±1.9 ka Outwash chain bt Basalts of Pittville Road (Units 1–4) glaciations gravel, undivided bmc Tholeiitic basalts of 108±14 ka older Mill Creek Plateau m20 Basaltic andesite west of hill 2078 glaciations Middle Pleistocene and older volcanic rocks 108.6±2.1 ka bs Basalts of Stephens Campground (Units 1–5) 110.8±3.8 ka 101.5±8.7 ka br Basalts of Robbers Spring (Units 1–5) 125 ka* 143±6 ka mbg Basaltic andesite of Little Bunchgrass Meadow ? ? ? mbx Basaltic andesite of Box Canyon 167±4 ka Basalts and basaltic bsm msm 172±23 ka andesites of Sifford Basaltic andesite of Small Butte Brunhes (+) Mountain 193±11 ka rd Rhyodacite of Dersch Meadows 199±22 ka bec Tholeiitic basalt of 190±18 ka b44 Tholeiitic basalt of b18 Tholeiitic basalt 188±32 ka Eagle Canyon Calif. Hwy 44 of hill 1879 amh Andesite and basalt of Mount Harkness 210±120 ka 212±5 ka dr Dacite of Reading Peak 232±8 ka db Dacite of Bumpass Mountain bn Tholeiitic basalt of Nobles Trail 236±1 ka dc Dacite of Crescent Crater mm Basaltic andesites of 202.0±2.2 ka bl35 Basalt of section 35 Qs82 Avalanche deposit 244±10 ka ds Dacite of Ski Heil Peak Magee Volcano from dacite of 247±56 ka ap Andesite and basaltic andesite bl2 Basalt of section 2 bl20 Basalt of hill 2088 249±12 ka dh Dacite of Mount Helen hill 8283 of Prospect Peak Cone bl30 Basalt of section 30 duh Dacite under Mount Helen dsc Dacite of acl Andesite and basaltic Summit Creek andesite of Cluster Lake 220±14 ka bl22 Basalt of hill 2232 dpl Dacite of Lassen Peak parking lot dv Dacite of Bumpass Lakes chain bl21 Basalt of hill 2109 261±5 ka d82 Dacite of hill 8283 Vulcans Castle sequence ? mlc Basaltic andesites of Cone Lake ml18 Basaltic andesite of hill 1868 270±18 ka arp Andesite of Raker Peak pdh Lithic tephra from dmz Dacite of upper Manzanita Creek Triangle Deep Hole mtr Lake 277±22 ka Basaltic andesite of Triangle Lake sequence mt20 Basaltic andesites of section 20 297±1 ka rmz beb Basalts of Bond Valley (Units 1–3) Rhyodacite of Manzanita Chute mhl Basaltic andesite of Echo Twin Lakes sequence, older Twin 302±7 ka bsl Basalt of Lost Spring Lake 302±36 ka mee 298±9 ka rmc Rhyodacite of Mount Conard Huckleberry Lake Basaltic andesites of Echo Lake (Units 1–2) bsd Basalt of Duck Lake sequence mes rlm Rhyodacite of Loomis Peak Basaltic andesite of Star Butte 313±8 ka av Andesite of Viola bct Basalt of bo Basalt of Onion Springs Island bii Basalt of mce Basaltic andesite mcj Basaltic andesite mcr Basaltic andesite Cherry Caribou Thicket awp Andesites of West Lake Island Lake of Eleanor Lake of Jewel Lake of Rim Lake Prospect Peak Sunrise chain mcn Basaltic andesites of North Caribou (Units 1–8) bbf Basalt of Badger Flat sequence 331±45 ka bie Basalt of QUATERNARY Peak East Lake bcs Basalt of South Caribou sequence 362±33 ka mcm Basaltic andesite of middle Caribou Caribou bcw mch Basaltic andesite of Hay Meadow Basalt of sequence Caribou mc71 Basaltic andesite of hill 7114 Wilderness bs72 Basalt of hill 7243 bci Basalt of Indian Meadow 393±4 ka bss Basalts of Sunrise Peak (Units 1–2) 400±14 ka mc Basaltic andesites of 387±10 ka amd Andesite of Mount Diller bsb Basalt of Bathtub Lake bcp Basalt of Silver Lake (Units 1–11) Caribou Peak Qwb Debris-flow deposit bcb from Brokeoff Volcano Basalt of Cowboy Lake
Recommended publications
  • Abandonment of the Name Hartford Hill Rhyolitetuff and Adoption of New Formation Names for Middle Tertiary Ash-Flow Tuffs in the Carson City- Silver City Area, Nevada
    Abandonment of the Name Hartford Hill RhyoliteTuff and Adoption of New Formation Names for Middle Tertiary Ash-Flow Tuffs in the Carson City- Silver City Area, Nevada GEOLOGICAL SURVEY BULLETIN 1457-D Abandonment of the Name Hartford Hill Rhyolite Tuff and Adoption of New Formation Names for Middle Tertiary Ash-Flow Tuffs in the Carson City- Silver City Area, Nevada By EDWARD C. BINGLER CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1457-D UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1978 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Dingier, Edward C. Abandonment of the name Hartford Hill rhyolite tuff and adoption of new formation names for middle Tertiary ash-flow tuffs in the Carson City - Silver City area, Nevada (Contributions to stratigraphy) Geological Survey Bulletin 1457-D Supt. of Docs. No.: I 19.3: 1457-D Bibliography: p. D19 I. Geology, Stratigraphic-Tertiary. 2. Volcanic ash, tuff, etc.-Nevada- Carson City region. 3. Geology-Nevada-Carson City region. I. Title. II. Series. HI. Series: United States. Geological Survey. Bulletin 1457-D. QE75.B9 no. 1457-D [QE691] 557.3'08s [551.7'8] 78-606063 For sale by the Superintendent of Documents, U. S. Government Printing Office Washington, D. C. 20402 Stock Number 024-001-03124-8 CONTENTS Page Abstract___________________________________ Dl Introduction ______________________________________ 1 Acknowledgments ________________________________ 5 Ash-flow stratigraphy in the Carson City-Silver City area ___________ 7 Mickey Pass Tuff ________________________________ 7 Lenihan Canyon Tuff _____________________________ 8 Nine Hill Tuff _______________________________ 11 Eureka Canyon Tuff ______________________________ 14 Dacitetuff __________________________________ 16 Rhyolite tuff and augite rhyodacite tuff ___________________ 16 Santiago Canyon Tuff _____________________________ 17 References cited _____________________________^_____ 19 ILLUSTRATIONS Page FIGURE 1.
    [Show full text]
  • The Boring Volcanic Field of the Portland-Vancouver Area, Oregon and Washington: Tectonically Anomalous Forearc Volcanism in an Urban Setting
    Downloaded from fieldguides.gsapubs.org on April 29, 2010 The Geological Society of America Field Guide 15 2009 The Boring Volcanic Field of the Portland-Vancouver area, Oregon and Washington: Tectonically anomalous forearc volcanism in an urban setting Russell C. Evarts U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025, USA Richard M. Conrey GeoAnalytical Laboratory, School of Earth and Environmental Sciences, Washington State University, Pullman, Washington 99164, USA Robert J. Fleck Jonathan T. Hagstrum U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025, USA ABSTRACT More than 80 small volcanoes are scattered throughout the Portland-Vancouver metropolitan area of northwestern Oregon and southwestern Washington. These vol- canoes constitute the Boring Volcanic Field, which is centered in the Neogene Port- land Basin and merges to the east with coeval volcanic centers of the High Cascade volcanic arc. Although the character of volcanic activity is typical of many mono- genetic volcanic fi elds, its tectonic setting is not, being located in the forearc of the Cascadia subduction system well trenchward of the volcanic-arc axis. The history and petrology of this anomalous volcanic fi eld have been elucidated by a comprehensive program of geologic mapping, geochemistry, 40Ar/39Ar geochronology, and paleomag- netic studies. Volcanism began at 2.6 Ma with eruption of low-K tholeiite and related lavas in the southern part of the Portland Basin. At 1.6 Ma, following a hiatus of ~0.8 m.y., similar lavas erupted a few kilometers to the north, after which volcanism became widely dispersed, compositionally variable, and more or less continuous, with an average recurrence interval of 15,000 yr.
    [Show full text]
  • Geology of the Los Adobes Rancho Area, Sonora, Mexico, and Santa Cruz County, Arizona
    GEOLOGY OF THE LOS ADOBES RANCHO AREA, SONORA, MEXICO, AND SANTA CRUZ COUNTY, ARIZONA by WYATT G. GILBERT AND DAVID J. LAJACK November, 2000 Arizona Geological Survey Contributed Map CM OO-C In cooperation with Minefinders Corporation, Ltd. Arizona Geological Survey 416 W. Congress, Suite 100, Tucson, AZ 85701 Includes 5 page text, 1:24,000 scale geologic map and cross-sections (1 sheet) INTRODUCTION During the period April IS-October 18, 1996, the authors mapped the geology of about 110 square kilometers west of Nogales, Sonora, Mexico along the international border near Los Adobes Rancho for Minefinders Corporation, Ltd .. Approximately 46 days were spent in the field. SUMMARY OF GEOLOGY Reconnaissance geologic mapping focused primarily on the Mesozoic and Tertiary igneous and sedimentary rocks that lie both north and south of the main road into the area. No fossil or radiometric age data were obtained from the area, and age assignments, made on stratigraphic and intrusive relationships, are provisional at best. The oldest rocks in the map area include generally coarse terrigenous clastic units (KJsc, KJsI, KJs, KJc) that generally dip moderately northeast. Similar units mapped as the La Jareta Formation in the Planchas de Plata area just south of the map area (Segerstrom, 1987) and immediately north of the international border as the Salero Formation (Drewes, 1981) or as the Summit Conglomerate (informal) and/or Bisbee Formation (Riggs, 1987) are thought to be Jurassic or Cretaceous in age. These sedimentary units are overlain by felsic pyroclastic beds (KJft, KJftb) that are in turn overlain by dacite (KJd, KJdv, KJda).
    [Show full text]
  • Cerro Pizarro Volcano, Mexico by G. Carrasco-Nú
    1 Polygenetic nature of a rhyolitic dome and implications for hazard assessment: 2 Cerro Pizarro volcano, Mexico 3 by G. Carrasco-Núñez and N. Riggs 4 5 ABSTRACT 6 Rhyolitic domes are commonly regarded as monogenetic volcanoes associated with single, brief 7 eruptions. They are characterized by short-lived successions of pyroclastic and effusive activity 8 associated with a series of discrete eruptive events that apparently last on the order of years to 9 decades. Cerro Pizarro, a ~ 1.1 km3 rhyolitic dome in the eastern Mexican Volcanic Belt, shows 10 aspects of polygenetic volcanism including long-term repose periods (~ 50-80 ky) between 11 eruptions, chemical variations with time, and a complex evolution of alternating explosive and 12 effusive eruptions, a cryptodome phase, and sector collapse. This eruptive behavior provides 13 new insights into how rhyolite domes may evolve. A protracted, complex evolution bears 14 important implications for hazard assessment if reactivation of an apparently extinct rhyolitic 15 dome must be seriously considered. 16 17 Keywords: monogenetic volcanism, polygenetic volcanism, rhyolites, dome growth, volcanic 18 hazards, Mexican Volcanic Belt 19 20 INTRODUCTION 21 Monogenetic volcanoes comprise a wide spectrum of relatively small volcanic structures 22 (generally less than a few km3 erupted material) that show a commonly simple evolution (one 23 eruption, or a few clearly related eruptions), short life span (commonly years to decades for 24 mafic volcanoes, but possibly as much as a few centuries for rhyolitic domes), and minor 25 chemical composition changes. Monogenetic volcanoes are, in general, either basalt or rhyolite, 26 while polygenetic volcanoes, which erupt repeatedly and have a large and persistent magma 27 storage chamber, are commonly andesitic or dacitic in composition.
    [Show full text]
  • USGS Scientific Investigations Map 2832, Pamphlet
    Geologic Map of Mount Mazama and Crater Lake Caldera, Oregon By Charles R. Bacon Pamphlet to accompany Scientific Investigations Map 2832 View from the south-southwest rim of Crater Lake caldera showing the caldera wall from Hillman Peak on the west to Cleetwood Cove on the north. Crater Lake fills half of the 8- by 10-km-diameter caldera formed during the climactic eruption of Mount Mazama volcano approximately 7,700 years ago. Volcanic rocks exposed in the caldera walls and on the flanks record over 400,000 years of eruptive history. The exposed cinder cone and andesite lava flows on Wizard Island represent only 2 percent of the total volume of postcaldera volcanic rock that is largely covered by Crater Lake. Beyond Wizard Island, the great cliff of Llao Rock, rhyodacite lava emplaced 100–200 years before the caldera-forming eruption, dominates the northwest caldera wall where andesite lava flows at the lakeshore are approximately 150,000 years old. 2008 U.S. Department of the Interior U.S. Geological Survey This page intentionally left blank. CONTENTS Introduction . 1 Physiography and access . 1 Methods . 1 Geologic setting . 4 Eruptive history . 5 Regional volcanism . 6 Pre-Mazama silicic rocks . 6 Mount Mazama . 7 Preclimactic rhyodacites . 9 The climactic eruption . 10 Postcaldera volcanism . .11 Submerged caldera walls and floor . .11 Glaciation . .11 Geothermal phenomena . 12 Hazards . 13 Volcanic hazards . 13 Earthquake hazards . 14 Acknowledgments . 14 Description of map units . 14 Sedimentary deposits . 15 Volcanic rocks . 15 Regional volcanism, northwest . 15 Regional volcanism, southwest . 17 Mount Mazama . 20 Regional volcanism, east . 38 References cited .
    [Show full text]
  • 04Chapter3 Kavalieris.Pdf
    THE GEOLOGY AND GEOCHEMISTRY OF THE GUNUNG PANI GOLD PROSPECT, NORTH SULAWESI, INDONESIA by Imants Kavalieris A thesis submitted as the requirement for admission to the Degree of Master of Science at the Australian National University October 1984 -29- III. GEOLOGY OF THE PANI VOLCANIC COMPLEX AND RELATED ROCKS 3.1 Introduction The Pani Volcanic Complex (Fig. 5) consists of non-welded pyroclastics, breccias and massive or flow banded lava-like rhyodacites, essentially confined to a partly circular structure of about 3.5km diameter, within older granodiorite basement. The adjacent basement is extensively intruded by rhyodacite dykes and porphyritic microgranites. These rocks comprise more than 50% of the area within a 20km radius of the Pani Volcanic Complex. On the SW margin of the volcanic structure a dense dyke swarm appears structurally controlled mainly in an ESE direction. It has been concluded from these broad relation- ships that the Pani Volcanic Complex represents a deeply eroded remnant of an acid volcanic centre. The Pani Complex has at least one other major counterpart in the area, which reinforces this conclusion (the Tabulo ring- dyke Complex) . Description of rocks from the Tabulo structure are referred to in the following sections. 3.2 Lithology Mineralogically the Pani Complex igneous rocks are remarkably similar, although they comprise a wide range of textural types, from massive porphyritic rhyodacites to lapilli tuffs, agglomerates and volcanic breccia. Geology of the Pani Volcanic Complex {'_ ( ID~~_;_ Tpli ? ·· \ Hot Sprlno ) _.-_.·: .: : :t.·· Gunung .f? J j X ·.•··••·· \""'" : ~ X , X . \ LEGEND ~ "·· X ___ ,... s ....__ I ; .. ···"····/.. ~ X ~-te(!l-oO~o~ \ \ Rhyodacite lapilli tuff (Tpi +1[) ~ij·.,rx-~~":-:-':V"' .
    [Show full text]
  • The Volcano-Tectonic Evolution of the Miocene Santa Lucía Volcano, Boaco District, Nicaragua
    Journal of Geosciences, 56 (2011), 27–41 DOI: 10.3190/jgeosci.085 Original paper The volcano-tectonic evolution of the Miocene Santa Lucía Volcano, Boaco district, Nicaragua David BURIÁNEK1*, Petr HRADECKÝ2 1 Czech Geological Survey, Leitnerova 22, 658 59 Brno, Czech Republic; [email protected] 2 Czech Geological Survey, Klárov 3, 118 21 Prague 1, Czech Republic; [email protected] * Corresponding author The present-day Santa Lucía caldera is an erosional relic of a Late Oligocene to Early Miocene stratoshield volcano located in the south-western part of the Chortis Block in Central Nicaragua. Six main lithological units were recogni- zed: (Unit I) dacitic ignimbrite of Boaco type, which represents the basement of the Santa Lucía caldera; (Unit II) da- citic ignimbrite of Fonseca type, locally intercalated with epiclastic and dacitic lavas; (Unit III) “lower” andesite lavas; (Unit IV) blocky, lithic-rich pyroclastic flow deposits, (Unit V) “upper” andesite and basalt lavas, and (Unit VI) epic- lastic rocks (lahar deposits). On the basis of field mapping, petrological and geochemical data, a new model for the evolution of the Santa Lucía Vol- cano is presented. The first stage consisted of a series of strong Sub-Plinian eruptions, which produced thick ignimbri- te units. These events destroyed the pre-existing volcanic edifice. The second stage was dominated by large explosive eruptions producing mainly non-welded dacitic–andesitic ignimbrites. The next resulted in the formation of andesitic lava flows and minor tephra fall-out deposits, covered by voluminous basaltic lavas. Lahars probably triggered by vol- canic and/or seismic events represent the final stage of volcanic activity.
    [Show full text]
  • Oligocene and Miocene Arc Volcanism in Northeastern California: Evidence for Post-Eocene Segmentation of the Subducting Farallon Plate
    Origin and Evolution of the Sierra Nevada themed issue Oligocene and Miocene arc volcanism in northeastern California: Evidence for post­Eocene segmentation of the subducting Farallon plate Joseph P. Colgan1,*, Anne E. Egger2, David A. John1, Brian Cousens3, Robert J. Fleck1, and Christopher D. Henry4 1U.S. Geological Survey, 345 Middlefield Road, Mail Stop 973, Menlo Park, California 94025, USA 2Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Stanford, California 94305, USA 3Carleton University, 1125 Colonel By Drive, Ottawa, Ontario, Canada K1S5B6 4Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada 89557, USA ABSTRACT sitionally similar to Oligocene rocks in the Unlike the western Cascades, however, vol­ Warner Range. They are distinctly different canic rocks of the ancestral Cascades are a subset The Warner Range in northeastern Cali- from younger (Late Miocene to Pliocene) of a diverse and widespread suite of Cenozoic fornia exposes a section of Tertiary rocks over high-Al, low-K olivine tholeiites, which are volcanic rocks erupted across the Basin and 3 km thick, offering a unique opportunity to more mafic (46%–49% SiO2), did not build Range Province since the Eocene. The ancestral study the long-term history of Cascade arc large edifices, and are thought to be related Cascades samples plotted in Figure 1 are those volcanism in an area otherwise covered by to backarc extension. The Warner Range is considered by du Bray et al. (2009) to be plausi­ younger volcanic rocks. The oldest locally
    [Show full text]
  • Origin of Andesite and Dacite: Evidence of Mixing at Glass Mountain in California and at Other Circum-Pacific Volcanoes
    Origin of andesite and dacite: Evidence of mixing at Glass Mountain in California and at other circum-Pacific volcanoes JOHN C. EICHELBERGER* Department of Geology, Stanford University, Stanford, California 94305 ABSTRACT subtracting appropriate proportions of appropriate phases from a hypothetical parent liquid. Likewise, by choosing an appropriate The intimate association of basalt, andesite, dacite, and rhyolite hypothetical source rock and adjusting conditions, nearly any ob- within a volcanic center suggests that these rocks are genetically served composition could be produced by partial melting. The test related. Individual lava flows that show a gradation in composition of such models is whether they agree with the phase assemblages in may preserve maximum evidence of the magmatic processes pro- magmas. It is often impossible to make this evaluation for intrusive ducing this association. One such flow of rhyolite to dacite compo- rocks because it is difficult to look back through the crystallization sition, Glass Mountain in northern California, was formed by con- process to the magmatic stage. However, fresh volcanic rocks rep- tamination of rhyolite magma as it intruded the basaltic flows of resent quenched magma samples in which the liquid remains as a the Medicine Lake Highland shield volcano. Although dacite flows metastable glass or finely crystalline groundmass, and the crystal and domes commonly show less variation in composition than the phases remain as phenocrysts. Although it cannot be assumed that Glass Mountain flow, many show similar evidence of contamina- volcanic rocks are representative of all igneous rocks, they do allow tion by basalt by the presence of abundant basaltic inclusions and interpretation of magmatic processes with a minimum of assump- phenocrysts and phenocryst clots from those inclusions.
    [Show full text]
  • Analysis of Composition and Chronology of Dome Emplacement
    ANALYSIS OF COMPOSITION AND CHRONOLOGY OF DOME EMPLACEMENT AT BLACK PEAK VOLCANO, ALASKA UTILIZING ASTER REMOTE SENSING DATA AND FIELD-BASED STUDIES A THESIS Presented to the Faculty of the University of Alaska Fairbanks In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE By Jennifer Nicole Adleman, B.S. Fairbanks, Alaska May 2005 iii Abstract Black Peak volcano is a —3.5lcin-diameter caldera located on the Alaska Peninsula that formed —4,600 years ago in an eruption that excavated >101cm 3 of material. The caldera floor is occupied by at least a dozen overlapping dacitic to andesitic lava domes and flows. Examination of XRF results and observations of the domes in and around the caldera reveals a range of 57-65wt% Si0 2 and variations in amphibole content. Evidence for magma mixing includes vesicular enclaves and geochemical trends that indicate involvement of a more mafic magma into a dacitic reservoir. The purpose of this study is to investigate if, and how, these differences in composition and mineralogy are detectable in satellite emissivity and TIR data (ASTER) and compare the results to ground-based field observations to discern changes in the mineralogical and chemical properties of the domes. This study incorporates the use of decorrelation-stretch image processing techniques and the deconvolution of laboratory emissivity spectra to assess the viability of discriminating variations in the lithologies observed at Black Peak volcano. Compositional results from XRD and electron microprobe analyses are comparable to those obtained through deconvolution processing. Surfaces of <10% amphibole and Si02 of 60-65wt% and those that correspond to > 10% and <6 Iwt% Si02 are distinguishable in the ASTER data.
    [Show full text]
  • Petrology of the Keetley Volcanics in Summit and Wasatch Counties
    PETROLOGY OF THE KEETLEY VOLCANICS IN SUMMIT AND WASATCH COUNTIES, NORTH-CENTRAL UTAH A THESIS SUBMITTED TO THE FACULTY OF THE GRADUATE SCHOOL OF THE UNIVERSITY OF MINNESOTA BY ms SI EINARI LEVEINEN IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE MARCH, 1994 PETROLOGY OF THE KEETLEY VOLCANICS IN SUMMIT AND WASATCH COUNTIES, NORTH-CENTRAL UTAH A THESIS SUBMITTED TO THE FACULTY OF THE GRADUATE SCHOOL OF THE UNIVERSITY OF MINNESOTA BY JUSSI EINARI LEVEINEN IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE MARCH, 1994 Abstract The Keetley Volcanics rest subhorizontally in a structural saddle between the Uinta and Wasatch Mountains ca. 35 km east of Salt Lake City. The Keetley Volcanics consist essentially of Oligocene to Late Eocene volcanic breccias, sandstones, lava flows and porphyritic intrusives. Volcanic breccias are volumetrically the most important, being as thick as 500 m (total) in the vicinity of Keetley. Most of the breccias and intrusives are andesitic. Chemical compositions vary from trachyandesite to silica-poor rhyodacite. The relatively uniform compositions suggest a trachyandesitic source that differentiated by fractional crystallization in a relatively shallow chamber. Large porphyry intrusions are also present west of the Keetley Volcanics. Apparently, the Keetley Volcanics represent a part of magmatic events in the Uinta-Oquirrh mineral belt that started in Late Eocene and continued into earliest Miocene. The Keetley Volcanics may belong to a larger group of mid-Tertiary early to syn-extensional volcanic rocks that were formed before the gradual development of the San Andreas - Basin and Range transform-extensional system.
    [Show full text]
  • Hydrothe~Mal Alteration of Basaltic Andesite and Other Rocks in Drill Hole Gs-6, Steamboat Springs, Nevada
    GEOLOGICAL SURVEY RESEARCH 1967 HYDROTHE~MAL ALTERATION OF BASALTIC ANDESITE AND OTHER ROCKS IN DRILL HOLE GS-6, STEAMBOAT SPRINGS, NEVADA By ROBERT SCHOEN and DONALD E. WHITE, Menlo Park, Calif. Abstract.-Geothermal waters produced two recognizable pat­ tionships between the compositions of waters and the terns of hydrothermal alteraltion in the rocks in drill hole observed alteration patterns. GS-6. During an early period, the rocks were subjected to The generalized geology of the thermal area is potassium metasomatism that formed K-feldspar and celadon­ ite from unstable feldspars and ferromagnesian minerals, re­ shown in figure 1. The basement rocks consist of a spectively. A later period of hydrogen metasomatism pro­ granodiorite pluton of late Mesozoic age intruded into duced mixed-layer· illite-montmorillonite, montmorillonite, and metamorphosed sedimentary and volcanic rocks of kaolinite, probably as a series directly related to the intensity probable early Mesozoic age. Tertiary and Quater­ of alteration. The clays formed during hydrogen metasoma­ nary volcanic and sedimentary rocks were deposited tism are irregularly distributed with depth and probably are related to reactions involving C02 and H2S. This later period intermittently on the evoded surf'ace of this basement, of argillization still may be in progress. and andesite dikes intruded the granodiorite. Out­ crops of the Tertiary volcanic and sedimentary rocks are too small to distinguish in figure 1, but core This paper presents the results of a mineralogic samples of these rocks, from drill hole GS-6, are shown study of GS-6, one of eight holes drilled at Steamboat in figure 2. Springs, Nev., by the U.S.
    [Show full text]