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GSA Foundation Update 18 Details Contents GSA TODAY publishes news and information for more than 17,000 GSA members and subscribing libraries. GSA Today lead science articles should present the results of exciting new research or summarize and synthesize important problems or issues, and they must be understandable to all Vol. 12, No. 8 August 2002 in the earth science community. Submit manuscripts to science editor Karl Karlstrom, [email protected]. GSA TODAY (ISSN 1052-5173) is published monthly by The Geological The Great Sand Dunes Colorado Photo by Martin Miller Society of America, Inc., with offices at 3300 Penrose Place, Boulder, Colorado. Mailing address: P.O. Box 9140, Boulder, CO 80301-9140, U.S.A. Periodicals postage paid at Boulder, Colorado, and at additional mailing offices. Postmaster: Send address changes to GSA Today, Member Services, Colorado Plateau uplift and erosion evaluated using GIS P.O. Box 9140, Boulder, CO 80301-9140. Joel L. Pederson, Rob D. Mackley, and James L. Eddleman 4 Copyright © 2002, The Geological Society of America, Inc. (GSA). All rights reserved. Copyright not claimed on content prepared wholly by U.S. Dialogue Overcoming Obstacles to Incorporating Experiential government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, Learning into the Geology Curriculum 11 to use a single figure, a single table, and/or a brief paragraph of text in other subsequent works and to make unlimited photocopies of items in this journal for noncommercial use in classrooms to further education DEADLINE! Last Chance to Vote 11 and science. For any other use, contact Copyright Permissions, GSA, P.O. Box 9140, Boulder, CO 80301-9140, USA, fax 303-357-1070, GSA Establishes Limnogeology Division 12 [email protected]; reference GSA Today, ISSN 1052-5173. Per- mission is granted to authors to post the abstracts only of their articles on their own or their organization’s Web site providing the posting Call for Geological Papers: 2003 GSA Section Meetings 13 includes this reference: “The full paper was published in the Geological Society of America’s journal GSA Today, [include year, month, and page numbers if known, where the article will appear].” GSA provides this and Birdsall-Dreiss Distinguished Lecturer for other forums for the presentation of diverse opinions and positions by 2003 Announced 14 scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. E&EG Science Co-editor Named 15 SUBSCRIPTIONS for 2002 calendar year: Society Members: GSA Call for Applications: 2003–2004 Congressional Today is provided as part of membership dues. Contact Member Services at 1-888-443-4472, (303) 447-2020, or [email protected] for Science Fellowship 15 membership information. Nonmembers & Institutions: Free with paid subscription to both GSA Bulletin and Geology, otherwise $65 for U.S., Canada, and Mexico; $75 elsewhere. Contact Subscription Services at Rock Stars—George Mercer Dawson: (800) 627-0629 or [email protected]. Also available on an annual Pioneer Explorer of Western Canada 16 CD-ROM (together with GSA Bulletin, Geology, GSA Data Repository, and an Electronic Retrospective Index to journal articles from 1972); $94 to GSA Members, others call GSA Subscription Services for prices and GSA Foundation Update 18 details. Claims: For nonreceipt or for damaged copies, members contact Member Services; all others contact Subscription Services. Claims are honored for one year; please allow sufficient delivery time for overseas Announcements 20 copies, up to six months. RIDGE 2000: The Next Decade of Innovative Studies STAFF Executive Director: John W. Hess and Discoveries at the Mid-Ocean Ridge 21 Science Editor: Karl E. Karlstrom, Department of Earth and Planetary Science, University of New Mexico, Albuquerque, NM 87131-1116, Denver 2002 Field Trips: Where Discovery Begins 22 [email protected] Director of Publications: Jon Olsen Managing Editor: Jeanette Hammann, [email protected] Journal Highlights 24 Editorial Assistant: Christina Alba Production Manager: Diane C. Lorenz Production Coordinator: Margo Y. Good Reminder: Penrose Conference Scheduled 26 Graphics Production: Margo Y. Good GeoVentures: 2002 Grand Canyon Memories 27 ADVERTISING Classifieds and display: Contact Ann Crawford, 1-800-472-1988, ext. 1053, (303) 357-1053, fax 303-357-1073; Classified Advertising 28 [email protected]. GSA ONLINE: www.geosociety.org Printed in U.S.A. using pure soy inks. On the cover: Obique three-dimensional view looking northeast onto the Colorado Plateau showing estimated erosional exhumation since ca. 30 Ma. Note the high erosion following Grand Canyon at bottom left of image. The canyon appears inverted because of high erosion along its axis and low values in the surrounding rim country. Negative values shown in blue are places of net deposition since ca. 30 Ma, such as the Quaternary San Francisco volcanic field near Flagstaff, Arizona, at the bottom center of image. Erosional unloading of the Colorado Plateau over the middle-late Cenozoic should cause significant rock uplift through isostatic rebound. 50% Total Recovered Fiber Image by J.L. Pederson. See “Colorado Plateau uplift and erosion evaluated using 10% Postconsumer GIS,” by J.L. Pederson et al., p. 4–10. Colorado Plateau uplift and erosion evaluated using GIS fact, less uplift on the plateau than pro- Cenozoic epeirogeny (e.g., Hunt, 1956; Joel L. Pederson, Rob D. Mackley, posed sources can supply. This suggests Morgan and Swanberg, 1985; and James L. Eddleman, Department Laramide uplift of the plateau was signifi- Humphreys, 1995; Spencer, 1996; of Geology, Utah State University, cantly less than that of the Rocky McQuarrie and Chase, 2000). The earliest Logan, Utah 84322-4505, USA Mountains, consistent with its prevalent researchers visiting the Colorado Plateau sedimentary basins, and/or that there has saw the deep incision of its spectacular been little or no post-Laramide uplift be- canyons and concluded that erosion has ABSTRACT yond erosional isostasy. been driven by recent—and ongoing— Study of the interaction between uplift uplift (e.g., Powell, 1875; Dutton, 1882; and erosion is a major theme of our sci- INTRODUCTION Davis, 1901; Hunt, 1956). This conclusion ence, but our understanding of their in- Pioneering geologists such as John was in keeping with W.M. Davis’ influen- terplay is often limited by a lack of Wesley Powell, Clarence Dutton, G.K. tial model that large-scale cycles of uplift quantitative data. A classic example is Gilbert, and William Morris Davis pon- and erosion end with landscapes de- the Colorado Plateau, for which the dered the Colorado Plateau landscape nuded to a peneplain near sea level, and starting and ending points are well evolution, and questions still puzzle re- with the related assumption that incision known: The region was at sea level in searchers today. In particular, what is the must be driven by subsequent uplift the Late Cretaceous, and now, the explanation for the plateau’s mild struc- rather than other means of lowering base deeply eroded land surface is at ~2 km. tural deformation compared to surround- level for streams. The concept of a The path of the landscape between ing areas, its high average elevation, and plateau denuded to near sea level after these endpoints is less clear, and there its dramatically incised landscape (Fig. 1)? Laramide time, and then epeirogenically has been longstanding debate on the Hypotheses for uplift of the Colorado uplifted later in the Cenozoic to account mechanisms, amounts, and timing of Plateau include mechanisms such as flat- for canyon incision, has persisted, but uplift and erosion. We use a geographic slab subduction, crustal thickening, and most workers recognize that the eleva- information system to map, interpolate, anomalous mantle properties during two tional history and the timing of erosion of and calculate the Cenozoic rock uplift stages of activity: (1) early Cenozoic the Colorado Plateau are still unknown. and erosional exhumation of the (Laramide) uplift; and (2) middle-late Colorado Plateau and gain insight into its landscape development through time. Initial results indicate uplift and erosion are highly spatially variable with mean values of 2117 m for rock uplift and 406 m for net erosional exhumation since Late Cretaceous coastal sandstones were deposited. We estimate 843 m of erosion since ca. 30 Ma (a larger value because of net deposition on the plateau over the early Cenozoic), which can account for 639 m of post-Laramide rock uplift by isostatic processes. Aside from this iso- static source of rock uplift, paleobotanical and fission-track data from the larger re- gion suggest the early Cenozoic Laramide orogeny alone should have caused more than the remaining rock uplift, and geo- physical studies suggest mantle sources for additional Cenozoic uplift. There is, in Figure 1. Physiographic extent of the Colorado Plateau according to Hunt (1956), which is used here for all discussion and analyses. Mean elevation is taken from merged 90 m digital elevation models (NAD83). 4 AUGUST 2002, GSA TODAY Isostatic response to the erosional ex- humation of the plateau over the middle- late Cenozoic should itself result in sig- nificant rock uplift, but this has not been adequately considered in evaluating the above ideas. Several well-known studies have investigated this effect in other areas using approaches different from those used here (e.g., Molnar and England, 1990; Montgomery, 1994; Tucker and Slingerland, 1994; Small and Anderson, 1995, 1998; Whipple et al., 1999). Here Figure 2. Illustrations of terms as described in text: U = rock uplift, U = we use a straightforward approach of di- R S ε rectly measuring rock uplift and exhuma- surface uplift (surface lowering when negative), = exhumation. A: The case of “active” tectonic rock uplift. B: “Passive” rock uplift due to isostatic tion using information preserved in the response to exhumation.
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