DOCSLIB.ORG

Owner's Manual,1996 Pontiac Bonneville

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Owner's Manual,1996 Pontiac Bonneville I LLt -The 1996 Pontiac Bonneville Owner’s Manual Seats and Restraint Systems ............................................................. 1-1 This section tells you how to use your seats and safety belts properly. It also explains“SRS” the system. Features and Controls ..................... ;............................................ 2-1 This section explainshow to start and operate your Pontiac. Comfort Controls and Audio Systems ...................................................... 3-1 This section tells you how to adjust the ventilation and comfort controls andhow to operate your audio system. Your Driving and the Road .............................................................. 4-1 Here you’ll find helpful information and tips about the roadhow and to drive under different conditions. ProblemsontheRoad .................................................................. 5-1 This section tells you whatto do if you have a problem whiledriving, such as a flat tire or overheated engine, etc. Service and Appearance Care.. .......................................................... 6-1 Here the manual tellsyou how to keep your Pontiacrunning properly and looking good. Maintenanceschedule......... .......................................................... 7-1 This section tellp you when to perform vehicle maintenance and what fluidsand lubricants to use. Customer Assistance Information ... .#.................................................... 8-1 \ This section tells youhow to contact Pontiac for assistance and how to get service and owner publications. It also gives you information on “Reporting Safety Defects”on page 8-9. Index .................................................................................. 9-1 Here’s an alphabetical listing ofalmost every subject in this manual.You can use it to quickly find something you. want to read. We support voluntary technician certification. CERTIFIED GENERAL MOTORS, GM and the GM Emblem, IL WE SUPPORT PONTIAC, the PONTIAC Emblem and the name VOLUNTARY TECHNICIAN BONNEVILLE are registered trademarks of General CERTIFICATION THROUGH Motors Corporation. National Institute for AUTOMOTIVE SERVICE This manual includes the latest information at the it time EXCELILENCE was printed. We reserve theright to make changesin the product afterthat time without further notice. For vehicles firstsold in Canada, substitute the name "General Motors of Canada Limited"for Pontiac For Canadian Owners Who Prefer a Division whenever it appearsin this manual. French Language Manual: Please keep this manualin your Pontiac, so it will be Aux propribtaires canadiens:Vous pouvez vous there if you ever need it when you're on' the road.If you procurer un exemplaire dece guide en franGais chez sell the vehicle, please leave this manualit soin the new votre concessionaireou au: owner canuse it. DGN Marketing Services Ltd. 1500 Bonhill Rd. Mississauga, Ontario L5T1C7 Litho in U.S.A. 'Copyright General Motors Corporation 1995 Part No. 10273 198 .B First Edition All Rights Reserved ii 1 How to Use This Manual Many people read their owner’s manualfrom beginning /1\ CAUTIGN: to end when theyfirst receive theirnew vehicle. If you do this, it will help you learn about the features and These mean thereis something that could hurt controls for your vehicle. In this manual, you’ll find that you or other people. pictures and words work together to explain things quickly. In the caution area, we tell you what the hazardis. Then Index we tell you what todo to help avoid or reduce the A good place to lookfor what you needis the Indexin hazard. Please read these cautions.If you don’t, you or others could be hurt. the backof the manual. It’san alphabetical listof all that’s in the manual, and the page number where you’ll find it. You will also finda circle with a slash throughit in Safety Warnings and Symbols this book. This safety symbol means“Don’t,’’ You will find a numberof safety cautions in this book. “Don’t do this,”or “Don’t We use a box and the word CAUTION to tell you about let this happen.” things that couldhurt you if you were toignore the warning. iii Vehicle DamageWarnings In the notice =ea, we tell you aboutsomething that can damage your vehicle. Mafly times, this damage would Also, in this book you will find thesenotices: not be coveredby your warranty, and it could be costly But the notice will tellyou what to do to help avoid the NOTICE: damage. "When you read other manuals, you might see CAUTION These mean there is something that could and NOTICE warnings in different colors or in differat words. 1 damage your vehicle. You'll also see warning labelson your vehicle.They use the same words, CAUTION or NOTICE. iv Vehicle Symbols These are some of the symbols you may find on your vehicle. For example, These symbols These symbols These symbols These symbols Here are some these symbols are important have to do with are on someof are used on other symbols are used onan for you and your lights: your controls: warning and you may see: original battery: your passengers indicator lights: whenever your vehicle is CAUTION driven: POSSIBLE A WIPER Q ENGINE FUSE INJURY COOLANT - e- f-l TEMP - DOOR LOCK TURN PROTECT SIGNALS EYES BY UNLOCK e BATTERY LIGHTER m SHIELDING CHARGING I-1 SYSTEM PARKING p$ CAUSTIC LAMPS WINDSHIELD HORN FASTEN DEFROSTER )tr SEAT BRAKE (0) BELTS BURNS COOLANT SPEAKER AVOID a b SPARKS OR FLAMES ENGINE OIL PRESSURE e,FUEL SPARK OR ,\I/, p3 RAM€ VENTILATING COULD e? ANTI~LOCK EXPLODE AIR BAG p\ FOG LAMPS FAN ) (@) $0 BRAKES BATTERY - v NOTES vi Section, 1 Seats and -Restraint Systems ~~~~ Here you’llfind information about the seats in your ManualFront Seat Pontiac and how to use your safety belts properly.You ~~ ._ can also learn about somethkgs you should not do with air bags and safety belts. A CAUTION: Seats and Seat Controls You can lose control of the vehicle if youto try t ,.:’ This section,tellsyou aboutthe seats -- how to adjust adjust a manual driver’s seat while the vehicleis them -- and also about reclining seatbacks and head restraints. moving. The sudden movement could startle and confuse you, or make you push a pedal when you don’t want to. Adjust the driver’s seat only when the vehicle is not moving. Pull up on the control bar under thefront of the seat to unlock it. Slide the seat to where you want it. Then release the bar andtry to move the seat withyour body, to make sure the seat is locked into place. I 1-1 Power Seat (Option) Center Control (B): Move the seat forward by pressing the control forward, or backwardby pressing the control To adjust the power seatson backward. some mkls: , Move the seat higherby holding the controlup. Lower the ,seatby holding the control down. Rear Control (C): Raise the rearof the seatby holding the switchup. Lower therew of the seatby holding the switch down. Power Lumbar Controls (Option) d! Reshapes the lower back area of the seat. Front Control (A): Raise the front of the seat by & Reshapes the middleback kea of the seat. holding the switchup. Lower the front of the seat by holding the switchdown. mk Reshapes the upper back areaof the seat. Adjustable Support Seat (Option) Reclining Front Seatbacks On some models, you'll find the controlson the center console. Slide the selector switch toL or R to choose the front seatyou want to adjust. -d#. Adjusts the seat forward or back. d Adjusts the seat up or down. Adjusts the seatback to an upright or reclined To adjust the seatback,lift the lever onthe outer side of position. the seat and movethe seatback to whereyou want it. Release the lever to lock the seatback. Pullon up the lever and the seat will go to an upright position. d-b Adjusts the positionof the seatback side bolsters. 'a Tilts therear of the seat up or down. A& A& Tilts the front of the seatup or down. 1-3 I Sitting in a reclined position when your vehicle is in motion can be dangerous. Even if you buckle up, your safety belts can’t do their job when you’re reclined like this. The shoulderbelt can’t do its jobbecause it won’t be against your body. Instead, it will be in front of you. In a crash you could go into it, receiving neck or other injuries. The lap belt can’t do its jobeither. ‘Ina crash the belt could go up over your abdomen. The belt forces would be there, not at your pelvic bones. This could cause serious internal injuries. But don’t have a seatback reclinedif your vehicleis For proper protection when the vehicle isin moving. motion, have the seatback upright. Then sit well back in the seat and wear your safety belt properly. Head Restraints Slide the head restraintup or down so that thetop of the restraint is closest to the top of your ears. This position reduces the chanceof a neck injury in a crash. On some models, the head restraintstilt forward and rearward also. 1-4 Safety Belts: They’re for Everyone Your vehicle has a light that comes onas a reminder to This part of the manual tells youhow to use safety belts buckle up. (See “Safety Belt properly. It also tells you some things you should not do Reminder Light” in the with safety, belts. Index.) And it explains the Supplemental Restraint System (SRS),or air bag system I- I- Don’t let anyone ride wherehe or she can’t wear In most.states and Canadian provinces, the law says to a safety belt properly. If you are in a crash and wear safety belts. Here’s why:They work. you’re not wearing a safety belt, your injuries You never know if you’ll be in a crash.If you do have a can be much worse. You can hit thingsinside the crash, .you don’t knowif it will be a bad one. vehicle or be ejected fromit. You can be seriously A few crashes are rnild, and some crashes canbe so injured orkilled.
Load more

Recommended publications
  • Geologic Map of the Twin Falls 30 X 60 Minute Quadrangle, Idaho
    Geologic Map of the Twin Falls 30 x 60 Minute Quadrangle, Idaho Compiled and Mapped by Kurt L. Othberg, John D. Kauffman, Virginia S. Gillerman, and Dean L. Garwood 2012 Idaho Geological Survey Third Floor, Morrill Hall University of Idaho Geologic Map 49 Moscow, Idaho 83843-3014 2012 Geologic Map of the Twin Falls 30 x 60 Minute Quadrangle, Idaho Compiled and Mapped by Kurt L. Othberg, John D. Kauffman, Virginia S. Gillerman, and Dean L. Garwood INTRODUCTION 43˚ 115˚ The geology in the 1:100,000-scale Twin Falls 30 x 23 13 18 7 8 25 60 minute quadrangle is based on field work conduct- ed by the authors from 2002 through 2005, previous 24 17 14 16 19 20 26 1:24,000-scale maps published by the Idaho Geological Survey, mapping by other researchers, and compilation 11 10 from previous work. Mapping sources are identified 9 15 12 6 in Figures 1 and 2. The geologic mapping was funded in part by the STATEMAP and EDMAP components 5 1 2 22 21 of the U.S. Geological Survey’s National Cooperative 4 3 42˚ 30' Geologic Mapping Program (Figure 1). We recognize 114˚ that small map units in the Snake River Canyon are dif- 1. Bonnichsen and Godchaux, 1995a 15. Kauffman and Othberg, 2005a ficult to identify at this map scale and we direct readers 2. Bonnichsen and Godchaux, 16. Kauffman and Othberg, 2005b to the 1:24,000-scale geologic maps shown in Figure 1. 1995b; Othberg and others, 2005 17. Kauffman and others, 2005a 3.
    [Show full text]
  • Carbon Monoxide As a Metabolic Energy Source for Extremely Halophilic Microbes: Implications for Microbial Activity in Mars Regolith
    Carbon monoxide as a metabolic energy source for extremely halophilic microbes: Implications for microbial activity in Mars regolith Gary M. King1 Department of Biological Sciences, Louisiana State University, Baton Rouge, LA 70803 Edited by David M. Karl, University of Hawaii, Honolulu, HI, and approved March 5, 2015 (received for review December 31, 2014) Carbon monoxide occurs at relatively high concentrations (≥800 that low organic matter levels might indeed occur in some deposits parts per million) in Mars’ atmosphere, where it represents a poten- (e.g., 12). Even so, it is uncertain whether this material exists in a tially significant energy source that could fuel metabolism by a local- form or concentrations suitable for microbial use. ized putative surface or near-surface microbiota. However, the The Martian atmosphere has largely been ignored as a potential plausibility of CO oxidation under conditions relevant for Mars in energy source, because it is dominated by CO2 (24, 25). Ironically, its past or at present has not been evaluated. Results from diverse UV photolysis of CO2 forms carbon monoxide (CO), a potential terrestrial brines and saline soils provide the first documentation, to bacterial substrate that occurs at relatively high concentrations: our knowledge, of active CO uptake at water potentials (−41 MPa to about 800 ppm on average, with significantly higher levels for −117 MPa) that might occur in putative brines at recurrent slope some sites and times (26, 27). In addition, molecular oxygen lineae (RSL) on Mars. Results from two extremely halophilic iso- (O2), which can serve as a biological CO oxidant, occurs at lates complement the field observations.
    [Show full text]
  • FIELD STUDIES of CRATER GRADATION in GUSEV CRATER and MERIDIANI PLANUM USING the MARS EXPLORATION ROVERS. J. A. Grant1, M. P. Golombek2, A
    Role of Volatiles and Atmospheres on Martian Impact Craters 2005 3004.pdf FIELD STUDIES OF CRATER GRADATION IN GUSEV CRATER AND MERIDIANI PLANUM USING THE MARS EXPLORATION ROVERS. J. A. Grant1, M. P. Golombek2, A. F. C. Haldemann2, L. Crumpler3, R. Li4, W. A. Watters5, and the Athena Science Team 1Center for Earth and Planetary Studies, National Air and Space Museum, Smithsonian Institution, Washington, DC 20560, 2Jet Propulsion Laboratory, California Institute of Tech- nology, Pasadena, CA 91109, 3New Mexico Museum of Natural History and Science, Albuquerque, NM 87104, 4Department of Civil Engineering and Remote Sensing, The Ohio State University, Columbus, OH 43210, 5Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139. Introduction: The Mars Exploration Rovers Spirit Impact Structures in Meridiani Planum: Craters and Opportunity investigated numerous craters since explored at Meridiani are fewer and farther between landing in Gusev crater (14.569oS, 175.473oE) and than at Gusev and all are formed into sulfate bedrock Meridiani Planum (1.946oS, 354.473oE) over the first [3]. With the exception of the most degraded examples, 400 sols of their missions [1-4]. Craters at both sites Meridiani craters have depth-to-diameter ratios >0.10 are simple structures and vary in size and preservation and preserve walls sloped generally >10 degrees. En- state. Comparing observed and expected pristine mor- durance crater is 150 m-in-diameter, 22 m deep, and phology and using process-specific gradational signa- possesses walls sloped between 15-30 degrees, but tures around terrestrial craters as a template [5-7] al- locally exceeding the repose angle (Table 1).
    [Show full text]
  • 1994 Pontiac Bonneville
    PONTIAC i IS94 EONNEVILLE OWNER'S MANUAL 1994 Owner’s Manual pPontiac Bonneville Table of Contents Introduction HOWto Use This Manual ............ Part I Seats & Restraint Systems ........... 7L Part 2 Features & Controls ............... 41 c Part 3 Comfort Controls & Audio Systems . I I I I Part 4 Your Driving and the Road ......... 137 E Part 5 Problems on the Road ............. 165 Part 6 Service & Appearance Care ........ 193 I Part 7 MaintenanceSchedule ............ 247 E Part 8 Customer Assistance Information . 265 Includes “Reporting Safety Defects” on page 269. Part9 Index ........................... 279 I Service Station Information .. Last Page Printed in USA 10260958 A Second Edition ... Important Notes About thisManual Please keep this manual in your Pontiac, so it will be there if you ever need it when you’re on the road. If YOU sell the vehicle, please leave this manual in it so the new owner can use it. This manual includes the latest information at the time it was printed. We reserve the right to make changes in the product after that time without further notice. Note to Canadian Owners For vehicles first sold in Canada, substitute the name “General Motors of Canada Limited” for Pontiac Division wheneverit appears in this manual. For Canadian Owners Who Prefer a French Language Manual: Aux proprietaires canadiens: Vous pouvez vous procurer un exemplaire de ce guide en franGais chez votre concessionaire ou au DGN Marketing Services Ltd., 1500 Bonhill Rd., Mississauga, Ontario L5T 1C7. Published by Pontiac Division GM and the GM Embiem, Pontiac, the Pontiac Emblem General Motors Corporation and the name Bonneville are registered trademarks of General Motors Corporation.
    [Show full text]
  • Ricane Magazines
    ■' ■■ A;, PAGE TWENTl >»> WEDNESDAY.'SEPTEMBER 7, 1969 iffiattrlTPBffr I fm lb A vence Didiy Nat Preaa Ron Hie Weather for tlw WMfe Bated ronMoot a t D.E8. WaattMa BoMM «iDM4tii.isar . rU r mad wvm taalgU. l.aw dt 13,125 X t« as. Fridor OMMttlt wony, w ant Hemlwr o< ttaa Aadlt «6yh a fn r Mattered ehowera Uk»- Bonon of Obwnlattoa Ijr. Hifk la Ste. M aneheaUr^A City of Village Charm VOL. LXXIX. NO. 289 iCTWENTY PAGES) MANCHESTER, CONN., THURSDAY, SEPTEMBER 8, 1960 (OlaMlOed AdvertlBlnc on Page 18) PRICJ^ FIVB CENTS Blasts VN, Belgium Second Group from the pages of the Plans Look at nation^s leading fashion Security Check ricane magazines... and our very .Washington, Sept. 8 (4^--- A second congressional com­ mittee is Goins to look into own second floor sportswear tJie defection of two U.S. code clerks; , Leopoldville. The C ongo.f^ion* “ "“ rntag the U.N. will A special 5-man subcon^nittee departrnent!... be Ukeh shortly.. of the House Armed Services Com­ Sept. 8 <i<P)-7-Preinier Patrice 11 16 announcement was issued mittee was formed, yesterday to X Lumumba went before an in the wake of the national assem­ check on how the Pentagon and angry Senate today to defend bly’s action yesterday voiding at­ Central Intelilgence Agency SWEATERS FOR '60 tempts by the conservative presi­ <CIA) ’’rsofult, screen, re-screen Trainmen Ask his, government and two dent and the left-leaning premier Full Force hours later they were cheek­ and clear their personnel.” to fire each other from their Jobs.
    [Show full text]
  • Ebook < Impact Craters on Mars # Download
    7QJ1F2HIVR # Impact craters on Mars « Doc Impact craters on Mars By - Reference Series Books LLC Mrz 2012, 2012. Taschenbuch. Book Condition: Neu. 254x192x10 mm. This item is printed on demand - Print on Demand Neuware - Source: Wikipedia. Pages: 50. Chapters: List of craters on Mars: A-L, List of craters on Mars: M-Z, Ross Crater, Hellas Planitia, Victoria, Endurance, Eberswalde, Eagle, Endeavour, Gusev, Mariner, Hale, Tooting, Zunil, Yuty, Miyamoto, Holden, Oudemans, Lyot, Becquerel, Aram Chaos, Nicholson, Columbus, Henry, Erebus, Schiaparelli, Jezero, Bonneville, Gale, Rampart crater, Ptolemaeus, Nereus, Zumba, Huygens, Moreux, Galle, Antoniadi, Vostok, Wislicenus, Penticton, Russell, Tikhonravov, Newton, Dinorwic, Airy-0, Mojave, Virrat, Vernal, Koga, Secchi, Pedestal crater, Beagle, List of catenae on Mars, Santa Maria, Denning, Caxias, Sripur, Llanesco, Tugaske, Heimdal, Nhill, Beer, Brashear Crater, Cassini, Mädler, Terby, Vishniac, Asimov, Emma Dean, Iazu, Lomonosov, Fram, Lowell, Ritchey, Dawes, Atlantis basin, Bouguer Crater, Hutton, Reuyl, Porter, Molesworth, Cerulli, Heinlein, Lockyer, Kepler, Kunowsky, Milankovic, Korolev, Canso, Herschel, Escalante, Proctor, Davies, Boeddicker, Flaugergues, Persbo, Crivitz, Saheki, Crommlin, Sibu, Bernard, Gold, Kinkora, Trouvelot, Orson Welles, Dromore, Philips, Tractus Catena, Lod, Bok, Stokes, Pickering, Eddie, Curie, Bonestell, Hartwig, Schaeberle, Bond, Pettit, Fesenkov, Púnsk, Dejnev, Maunder, Mohawk, Green, Tycho Brahe, Arandas, Pangboche, Arago, Semeykin, Pasteur, Rabe, Sagan, Thira, Gilbert, Arkhangelsky, Burroughs, Kaiser, Spallanzani, Galdakao, Baltisk, Bacolor, Timbuktu,... READ ONLINE [ 7.66 MB ] Reviews If you need to adding benefit, a must buy book. Better then never, though i am quite late in start reading this one. I discovered this publication from my i and dad advised this pdf to find out. -- Mrs. Glenda Rodriguez A brand new e-book with a new viewpoint.
    [Show full text]
  • Soppinfeksjoner (Saprolegnia Spp.) På Laksefisk I Norge -Statusrapport
    NINA Norsk institutt for naturforskning Soppinfeksjoner (Saprolegnia spp.) på laksefisk i Norge -statusrapport B. O. Johnsen O. Ugedal NINA Oppdragsmelding 716 NINA Norsk institutt for naturforskning Soppinfeksjoner (Saprolegnia spp.) på laksefisk i Norge - statusrapport Bjørn Ove Johnsen Ola Ugedal nina oppdragsmelding 716 Johnsen, B.O. & Ugedal, O. 2001. Soppinfeksjoner NINA•NIKUs publikasjoner (Saprolegnia spp.) på laksefisk i Norge - statusrapport. – NINA Oppdragsmelding 716:1-34. NINA•NIKU utgir følgende faste publikasjoner: Trondheim, november 2001 NINA Fagrapport NIKU Fagrapport ISSN 0802-4103 Her publiseres resultater av NINA og NIKUs eget forsk- ISBN 82-426-1268-4 ningsarbeid, problemoversikter, kartlegging av kunnskaps- nivået innen et emne, og litteraturstudier. Rapporter utgis også som et alternativ eller et supplement til internasjonal Forvaltningsområde: publisering, der tidsaspekt, materialets art, målgruppe m.m. Naturinngrep gjør dette nødvendig. Impact assessment Opplag: Normalt 300-500 Rettighetshaver ©: NINA Oppdragsmelding NINA•NIKU NIKU Oppdragsmelding Dette er det minimum av rapportering som NINA og NIKU gir Stiftelsen for naturforskning og kulturminneforskning til oppdragsgiver etter fullført forsknings- eller utrednings- prosjekt. I tillegg til de emner som dekkes av fagrapportene, Publikasjonen kan siteres fritt med kildeangivelse vil oppdragsmeldingene også omfatte befaringsrapporter, seminar- og konferanseforedrag, års-rapporter fra over- våkningsprogrammer, o.a. Opplaget er begrenset. (Normalt 50-100) NINA•NIKU Project Report Serien presenterer resultater fra begge instituttenes prosjekter når resultatene må gjøres tilgjengelig på engelsk. Serien omfatter original egenforskning, litteraturstudier, analyser av spesielle problemer eller tema, etc. Opplaget varierer avhengig av behov og målgrupper Temahefter Disse behandler spesielle tema og utarbeides etter behov bl.a. for å informere om viktige problemstillinger i samfunnet. Redaksjon: Målgruppen er "allmennheten" eller særskilte grupper, f.eks.
    [Show full text]
  • Martian Rock Types Analysis of Surface Composition
    Martian rock types Analysis of surface composition • Most of the knowledge from the surface compostion of Mars comes from: • Orbital spacecraft’s spectroscopic data • Analysis by rovers on the surface • Analysis of meteroites Southern Highlands • Mainly Basalts – Consists primarily of Olivine, Feldspars and Pyroxenes Northern Lowlands • Mainly Andesite – More evolved forms of magma – Highly volatile – Constitutes the majority of the crust Intermediate Felsic Types • High Silica Rocks • Exposed on the surface near Syrtis Major • Uncommon but include: • Dacites and Granitoids • Suggest diverse crustal composition Sedimentary Rocks • Widespread on the surface • Makes up the majority of the Northern lowlands deposists – May have formed from sea/lake deposits – Some show cross‐bedding in their layers – Hold the best chance to find fossilized life Carbonate Rocks • Formed through hydrothermal precipitation Tracks from rover unveil different soil types • Most soil consists of finely ground basaltic rock fragments • Contains iron oxide which gives Mars its red color • Also contains large amounts of sulfur and chlorine Tracks from rover unveil different soil types • Light colored soil is silica rich • High concentrations suggest water must have been involved to help concentrate the silica Blueberries • Iron rich spherules Meteorites on Mars What is a Martian meteorite? • Martian meteorites are achondritic meteorites with strong linear correlations of gases in the Martian atmosphere. Therefore, the gas trapped in each meteorite matches those that the Viking Lander found in Mar’s atmosphere. The graph below explains this correlation. • Image: http://www.imca.cc/mars/martian‐meteorites.htm Types of Martian Meteorites • 34 meteorites have been found that are Martian and they can be separated into 4 major categories with sub‐categories.
    [Show full text]
  • BONNEVILLE BASIN ANALOGUES for LARGE LAKE PROCESSES & CHRONOLOGIES of GEOMORPHIC DEVELOPMENT on MARS. K. Nicoll1, M.A. Chan
    40th Lunar and Planetary Science Conference (2009) 1962.pdf BONNEVILLE BASIN ANALOGUES FOR LARGE LAKE PROCESSES & CHRONOLOGIES OF GEOMORPHIC DEVELOPMENT ON MARS. K. Nicoll1, M.A. Chan2, T.J. Parker3, P.W. Jewell2, G. Koma- tsu4, and C.H. Okubo5, 1University of Utah, Department of Geography, 260 So. Central Campus Dr, Salt Lake City, UT 84112 USA, [email protected]; 2University of Utah Department of Geology and Geophysics, 135 S. 1460 E. Rm 383 Sutton Building., Salt Lake City, UT 84112 USA, [email protected], [email protected]; 3Jet Propulsion Laboratory, M/S 183-501, 4800 Oak Grove Drive, Pasadena, CA 91109 USA, [email protected]; 4International Research School of Planetary Sciences, Università d’Annuzio, Viale Pinadaro 42, 65127 Pescara, ITALY, [email protected]; 5MRO HiRISE Science & Operations, U.S. Geological Survey, 2255 N. Gemini Dr., Flagstaff, AZ 86001 USA, [email protected] Introduction: Pleistocene Lake Bonneville was a parameters, including paleowater depths, fetch, dura- large (~50,000 sq km) terrestrial closed lake system in tion of wave activity, etc [9-10]. Landforms associated Utah, USA that developed during the Last Glacial with Bonneville include erosional and aggradational Maximum (~20 ka BP), and persisted at highstand un- sedimentary features that developed over different til a catastrophic outburst flood event ~17.4 ka cal BP timescales, ranging from gradual (e.g., wave-cut shore- and warming climate significantly lowered its volume line terraces, lobate fan deltas developed over 1000s of [1]. Lake Bonneville and its modern relict Great Salt years) to the sudden or catastrophic (e.g., outburst Lake (fig.
    [Show full text]
  • Isostasy, Rheology, Cross Sections, Fault Mechanics
    2/16/12 GG612 Structural Geology Sec2on Steve Martel POST 805 [email protected] Lecture 4 Isostasy Rheology Strike-view Cross Sec2ons Fault Mechanics 2/16/12 GG612 1 Isostasy • Refers to gravitaonal equilibrium • Provides a physical raonale for the existence of mountains • Based on force balance and buoyancy concepts h P = ρ(h)g(h)dh ∫0 P = pressure (conven2on: compression is posi2ve) ρ = density g = gravitaonal acceleraon For constant ρ and constant g, P = ρgh hp://en.wikipedia.org/wiki/File:Iceberg.jpg 2/16/12 GG612 2 1 2/16/12 Isostasy • Assumes a “compensaon depth” at which pressures beneath two prisms are equal and the material beneath behaves like a stac fluid, where P1 = P2 • Flexural strength of crust not considered • Gravity measurements yield crustal thickness and density variaons • Complemented by seismic techniques hp://en.wikipedia.org/wiki/File:Iceberg.jpg 2/16/12 GG612 3 Isostasy History • Roots go back to da Vinci • Term coined by Clarence Edward DuWon (USGS) • Post-1800 interest triggered by surveying errors in India • Two main models: Pra, Airy 2/16/12 GG612 4 2 2/16/12 John Henry Pra (6/4/1809-12/28/1871) • Pra, J.H., 1855, On the arac2on of the Himalaya Mountains, and of the elevated regions beyond them, upon the Plumb- line in India. Philosophical Transac2ons of the Royal Society of London, v. 145, p. 53-100. • Bri2sh clergyman and mathemacian • Archdeacon of India hWp://sphotos.ak.fcdn.net/photos-ak-snc1/v2100/67/88/730660017/n730660017_5593665_6871.jpg 2/16/12 GG612 5 Sir George Biddell Airy (7/27/1801 - 1/2/1892 • Airy, G.B., 1855, On the computaon of the Effect of the AWrac2on of Mountain-masses, as disturbing the Apparent Astronomical Latude of Staons in Geode2c Surveys.
    [Show full text]
  • Planets Solar System Paper Contents
    Planets Solar system paper Contents 1 Jupiter 1 1.1 Structure ............................................... 1 1.1.1 Composition ......................................... 1 1.1.2 Mass and size ......................................... 2 1.1.3 Internal structure ....................................... 2 1.2 Atmosphere .............................................. 3 1.2.1 Cloud layers ......................................... 3 1.2.2 Great Red Spot and other vortices .............................. 4 1.3 Planetary rings ............................................ 4 1.4 Magnetosphere ............................................ 5 1.5 Orbit and rotation ........................................... 5 1.6 Observation .............................................. 6 1.7 Research and exploration ....................................... 6 1.7.1 Pre-telescopic research .................................... 6 1.7.2 Ground-based telescope research ............................... 7 1.7.3 Radiotelescope research ................................... 8 1.7.4 Exploration with space probes ................................ 8 1.8 Moons ................................................. 9 1.8.1 Galilean moons ........................................ 10 1.8.2 Classification of moons .................................... 10 1.9 Interaction with the Solar System ................................... 10 1.9.1 Impacts ............................................ 11 1.10 Possibility of life ........................................... 12 1.11 Mythology .............................................
    [Show full text]
  • Use of Geochemistry Data Collected by the Mars Exploration Rover Spirit in Gusev Crater to Teach Geomorphic Zonation Through Principal Components Analysis Christine M
    JOURNAL OF GEOSCIENCE EDUCATION 59, 184–193 (2011) Use of Geochemistry Data Collected by the Mars Exploration Rover Spirit in Gusev Crater to Teach Geomorphic Zonation through Principal Components Analysis Christine M. Rodrigue1,a) ABSTRACT This paper presents a laboratory exercise used to teach principal components analysis (PCA) as a means of surface zona- tion. The lab was built around abundance data for 16 oxides and elements collected by the Mars Exploration Rover Spirit in Gusev Crater between Sol 14 and Sol 470. Students used PCA to reduce 15 of these into 3 components, which, after quartimax rotation, very strikingly divided the surface traversed by Spirit’s into three distinct zones. Students then used such concepts as the Bowen reaction series, typical minerals in Earth’s basalts and andesitic arcs, the periodic table, and the Goldschmidt classification, together with Pancam images from Spirit and the Mars Orbiter Camera, to interpret the surfaces over which the rover moved. Students found this foray to Mars a challenging but enjoyable project, and it made PCA memorable to them long after the class had ended. Some variant on this lab could work for multivariate statistics courses in geology, geography, and environmental science, as well as advanced courses in the content of those disciplines, particularly those dealing with zonation. VC 2011 National Association of Geoscience Teachers. [DOI: 10.5408/1.3604826] INTRODUCTION example, a transect could be taken down a catena, across a This paper presents an exercise that uses Mars Explora- wetland–upland interface, or through a seasonal surface tion Rover geochemical data to teach principal components water and groundwater boundary (Fortin et al., 2000).
    [Show full text]