Navajo National Monument Geologic Resource Evaluation Report
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Curriculum Vita - Stephen J
Curriculum Vita - Stephen J. Reynolds School of Earth and Space Exploration, Arizona State University, Tempe, Arizona 85287-1404 (480) 965-9049 (work) Website: http://reynolds.asu.edu email: [email protected] Degrees/Registration University of Texas, El Paso: B.S., Geology, 1974 University of Arizona: M.S., Geosciences, 1977, Ph.D., Geosciences,1982 Arizona Registered Geologist #26773 (1993-present) Recent Professional Experience Arizona State University, Dept. of Geology: Professor (6/97 to present), Associate Professor (8/91 to 6/97). Teaching responsibilities include Advanced Geologic Field Mapping, Advanced Structural Geology, Applied Arizona Geology, Cordilleran Regional Geology, Geology of Arizona, Geotectonics, Introductory Geology, Orogenic Systems, Summer Field Geology, Methods of Geoscience Teaching ASU Center for Research on Education in Science, Mathematics, Engineering, and Technology, Associate Director (6/99 to present); chairman of founding committee. Arizona Geological Survey and Arizona Bureau of Geology and Mineral Technology: Research Geologist (6/88 to 7/91), Associate Research Geologist (6/87 to 6/88); Assistant Research Geologist (2/81 to 6/87). University of Arizona, Dept. of Geosciences: Visiting Associate Professor, (1991 to ~1997); Adjunct Associate Research Scientist (1987 to 1991); Research Associate and Assistant (1/75 to 12/80); Teaching Assistant (8/74 to 7/75) Geologist and Consulting Geologist: Clients include Animas Resources (2007 to present), Pediment Exploration, Ltd. (2007 to present), Clear Creek -
PRELUDE to SEVEN SLOTS: FILLING and SUBSEQUENT MODIFICATION of SEVEN BROAD CANYONS in the NAVAJO SANDSTONE, SOUTH-CENTRAL UTAH by David B
PRELUDE TO SEVEN SLOTS: FILLING AND SUBSEQUENT MODIFICATION OF SEVEN BROAD CANYONS IN THE NAVAJO SANDSTONE, SOUTH-CENTRAL UTAH by David B. Loope1, Ronald J. Goble1, and Joel P. L. Johnson2 ABSTRACT Within a four square kilometer portion of Grand Staircase-Escalante National Monument, seven distinct slot canyons cut the Jurassic Navajo Sandstone. Four of the slots developed along separate reaches of a trunk stream (Dry Fork of Coyote Gulch), and three (including canyons locally known as “Peekaboo” and “Spooky”) are at the distal ends of south-flowing tributary drainages. All these slot canyons are examples of epigenetic gorges—bedrock channel reaches shifted laterally from previous reach locations. The previous channels became filled with alluvium, allowing active channels to shift laterally in places and to subsequently re-incise through bedrock elsewhere. New evidence, based on optically stimulated luminescence (OSL) ages, indicates that this thick alluvium started to fill broad, pre-existing, bedrock canyons before 55,000 years ago, and that filling continued until at least 48,000 years ago. Streams start to fill their channels when sediment supply increases relative to stream power. The following conditions favored alluviation in the study area: (1) a cooler, wetter climate increased the rate of mass wasting along the Straight Cliffs (the headwaters of Dry Fork) and the rate of weathering of the broad outcrops of Navajo and Entrada Sandstone; (2) windier conditions increased the amount of eolian sand transport, perhaps destabilizing dunes and moving their stored sediment into stream channels; and (3) southward migration of the jet stream dimin- ished the frequency and severity of convective storms. -
Ron Blakey, Publications (Does Not Include Abstracts)
Ron Blakey, Publications (does not include abstracts) The publications listed below were mainly produced during my tenure as a member of the Geology Department at Northern Arizona University. Those after 2009 represent ongoing research as Professor Emeritus. (PDF) – A PDF is available for this paper. Send me an email and I'll attach to return email Blakey, R.C., 1973, Stratigraphy and origin of the Moenkopi Formation of southeastern Utah: Mountain Geologist, vol. 10, no. 1, p. 1 17. Blakey, R.C., 1974, Stratigraphic and depositional analysis of the Moenkopi Formation, Southeastern Utah: Utah Geological Survey Bulletin 104, 81 p. Blakey, R.C., 1977, Petroliferous lithosomes in the Moenkopi Formation, Southern Utah: Utah Geology, vol. 4, no. 2, p. 67 84. Blakey, R.C., 1979, Oil impregnated carbonate rocks of the Timpoweap Member Moenkopi Formation, Hurricane Cliffs area, Utah and Arizona: Utah Geology, vol. 6, no. 1, p. 45 54. Blakey, R.C., 1979, Stratigraphy of the Supai Group (Pennsylvanian Permian), Mogollon Rim, Arizona: in Carboniferous Stratigraphy of the Grand Canyon Country, northern Arizona and southern Nevada, Field Trip No. 13, Ninth International Congress of Carboniferous Stratigraphy and Geology, p. 89 109. Blakey, R.C., 1979, Lower Permian stratigraphy of the southern Colorado Plateau: in Four Corners Geological Society, Guidebook to the Permian of the Colorado Plateau, p. 115 129. (PDF) Blakey, R.C., 1980, Pennsylvanian and Early Permian paleogeography, southern Colorado Plateau and vicinity: in Paleozoic Paleogeography of west central United States, Rocky Mountain Section, Society of Economic Paleontologists and Mineralogists, p. 239 258. Blakey, R.C., Peterson, F., Caputo, M.V., Geesaman, R., and Voorhees, B., 1983, Paleogeography of Middle Jurassic continental, shoreline, and shallow marine sedimentation, southern Utah: Mesozoic PaleogeogÂraphy of west central United States, Rocky Mountain Section of Society of Economic Paleontologists and Mineralogists (Symposium), p. -
Monument Valley Meander
RV Traveler's Roadmap to Monument Valley Meander However you experience it, the valley is a wonder to behold, a harsh yet hauntingly beautiful landscape. View it in early morning, when shadows lift from rocky marvels. Admire it in springtime,when tiny pink and blue wildflowers sprinkle the land with jewel-like specks of color. Try to see it through the eyes of the Navajos, who still herd their sheep and weave their rugs here. 1 Highlights & Facts For The Ideal Experience Agathla Peak Trip Length: Roughly 260 miles, plus side trips Best Time To Go: Spring - autumn What To Watch Out For: When on Indian reservations abide by local customs. Ask permission before taking photos, never disturb any of the artifacts. Must See Nearby Attractions: Grand Canyon National Park (near Flagstaff, AZ) Petrified Forest National Park (near Holbrook, AZ) Zion National Park (Springdale, UT) 2 Traveler's Notes Monument Valley Navajo Tribal Park The stretch of Rte. 163 called the Trail of the Ancients in honor of the vanished Anasazis cuts across Monument Valley at the Utah border on its way to the little town of Mexican Hat. Named for a rock formation there that resembles an upside-down sombrero a whimsical footnote to the magnificence of Monument Valley—Mexican Hat is the nearest settlement to Goosenecks State Park, just ahead and to the west via Rtes. 261 and 316. The monuments in the park have descriptive names. They are based on ones imagination. These names were created by the early settlers of Monument Valley. Others names portray a certain meaning to the Navajo people. -
Geological Processes and Evolution
GEOLOGICAL PROCESSES AND EVOLUTION J.W. HEAD1, R. GREELEY2, M.P. GOLOMBEK3, W.K. HARTMANN4, E. HAUBER5, R. JAUMANN5, P. MASSON6, G. NEUKUM5, L.E. NYQUIST7 and M.H. CARR8 1Department of Geological Sciences, Brown University, Providence, RI 02912 USA 2Department of Geology, Arizona State University, Tempe, AZ 85287 USA 3Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, CA 91109 USA 4Planetary Science Institute, Tucson, AZ 85705 USA 5DLR Institute of Space Sensor Technology and Planetary Exploration, Rutherfordstrasse 2, 12484 Berlin-Aldershof, Germany 6University of Paris-Sud, 91405, Orsay Cedex France 7Johnson Space Center, Houston TX 77058 USA 8US Geological Survey, Branch of Astrogeological Studies, 345 Middlefield Road, Menlo Park, CA 94025 USA Received:14 February 2001; accepted:12 March 2001 Abstract. Geological mapping and establishment of stratigraphic relationships provides an overview of geological processes operating on Mars and how they have varied in time and space. Impact craters and basins shaped the crust in earliest history and as their importance declined, evidence of extensive regional volcanism emerged during the Late Noachian. Regional volcanism characterized the Early Hesperian and subsequent to that time, volcanism was largely centered at Tharsis and Elysium, con- tinuing until the recent geological past. The Tharsis region appears to have been largely constructed by the Late Noachian, and represents a series of tectonic and volcanic centers. Globally distributed structural features representing contraction characterize the middle Hesperian. Water-related pro- cesses involve the formation of valley networks in the Late Noachian and into the Hesperian, an ice sheet at the south pole in the middle Hesperian, and outflow channels and possible standing bodies of water in the northern lowlands in the Late Hesperian and into the Amazonian. -
Bulletin of the Geological Society of America Vol. 71. Pp. 1729-1754, 7 Figs. December 1960 Bermuda: a Partially Drowned, Late M
BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA VOL. 71. PP. 1729-1754, 7 FIGS. DECEMBER 1960 BERMUDA: A PARTIALLY DROWNED, LATE MATURE, PLEISTOCENE KARST BY J HARLEN BRETZ ABSTRACT During Pleistocene time, the Bermuda Islands repeatedly underwent partial inundation and re-emergence. The land areas were continuously attacked and reduced by rain and ground water but repeatedly renewed, during times of submergence, by deposition of marine limestone and by contemporaneous additions of shore-born and wind-transported carbonate sand, now eolianite. Soils formed under subaerial conditions are now buried be- neath later deposits and constitute important stratigraphic markers. The igneous founda- tion rock appears to have been exposed during some low marine stands, and the former shore lines seem to be recorded by submerged terraces. The major karst features are largely below sea level, and they must date from times of continental glaciations. Previous writers have assigned eolian accumulation to times of Pleistocene low sea level and soil-making to times of interglacial high sea. Both conclusions are held to be er- roneous. CONTENTS TEXT Figure Page Page Navy and Air Force modifications of the Introduction 1729 shore line 1730 Acknowledgments 1732 2. Bermuda Islands with the adjacent Dunes and eolianites 1732 banks 1733 Paleosols 1736 3. Diagram of section at Whalebone Bay, Ber- Caves 1741 muda Islands 1735 Origin of the interior basins 1744 4. Diagram to show contrast in soil record on Correlation of soil-making and dune-building uplands and lowlands, Bermuda with Pleistocene eustatism 1746 Islands 1736 Conclusion 1752 5. Diagram of Shore Hills type section, References cited 1754 Bermuda Islands 1737 6. -
The Moenave Formation: Sedimentologic and Stratigraphic Context of the Triassic–Jurassic Boundary in the Four Corners Area, Southwestern U.S.A
Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 111–125 www.elsevier.com/locate/palaeo The Moenave Formation: Sedimentologic and stratigraphic context of the Triassic–Jurassic boundary in the Four Corners area, southwestern U.S.A. ⁎ Lawrence H. Tanner a, , Spencer G. Lucas b a Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY 13214, USA b New Mexico Museum of Natural History, 1801 Mountain Road, N.W., Albuquerque, NM 87104, USA Received 20 February 2005; accepted 20 June 2006 Abstract The Moenave Formation was deposited during latest Triassic to earliest Jurassic time in a mosaic of fluvial, lacustrine, and eolian subenvironments. Ephemeral streams that flowed north-northwest (relative to modern geographic position) deposited single- and multi-storeyed trough cross-bedded sands on an open floodplain. Sheet flow deposited mainly silt across broad interchannel flats. Perennial lakes, in which mud, silt and carbonate were deposited, formed on the terminal floodplain; these deposits experienced episodic desiccation. Winds that blew dominantly east to south-southeast formed migrating dunes and sand sheets that were covered by low-amplitude ripples. The facies distribution varies greatly across the outcrop belt. The lacustrine facies of the terminal floodplain are limited to the northern part of the study area. In a southward direction along the outcrop belt (along the Echo Cliffs and Ward Terrace in Arizona), dominantly fluvial–lacustrine and subordinate eolian facies grade mainly to eolian dune and interdune facies. This transition records the encroachment of the Wingate erg. Moenave outcrops expose a north–south lithofacies gradient from distal, (erg margin) to proximal (erg interior). The presence of ephemeral stream and lake deposits, abundant burrowing and vegetative activity, and the general lack of strongly developed aridisols or evaporites suggest a climate that was seasonally arid both before and during deposition of the Moenave and the laterally equivalent Wingate Sandstone. -
Tetrapod Biostratigraphy and Biochronology of the Triassic–Jurassic Transition on the Southern Colorado Plateau, USA
Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 242–256 www.elsevier.com/locate/palaeo Tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau, USA Spencer G. Lucas a,⁎, Lawrence H. Tanner b a New Mexico Museum of Natural History, 1801 Mountain Rd. N.W., Albuquerque, NM 87104-1375, USA b Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY 13214, USA Received 15 March 2006; accepted 20 June 2006 Abstract Nonmarine fluvial, eolian and lacustrine strata of the Chinle and Glen Canyon groups on the southern Colorado Plateau preserve tetrapod body fossils and footprints that are one of the world's most extensive tetrapod fossil records across the Triassic– Jurassic boundary. We organize these tetrapod fossils into five, time-successive biostratigraphic assemblages (in ascending order, Owl Rock, Rock Point, Dinosaur Canyon, Whitmore Point and Kayenta) that we assign to the (ascending order) Revueltian, Apachean, Wassonian and Dawan land-vertebrate faunachrons (LVF). In doing so, we redefine the Wassonian and the Dawan LVFs. The Apachean–Wassonian boundary approximates the Triassic–Jurassic boundary. This tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau confirms that crurotarsan extinction closely corresponds to the end of the Triassic, and that a dramatic increase in dinosaur diversity, abundance and body size preceded the end of the Triassic. © 2006 Elsevier B.V. All rights reserved. Keywords: Triassic–Jurassic boundary; Colorado Plateau; Chinle Group; Glen Canyon Group; Tetrapod 1. Introduction 190 Ma. On the southern Colorado Plateau, the Triassic– Jurassic transition was a time of significant changes in the The Four Corners (common boundary of Utah, composition of the terrestrial vertebrate (tetrapod) fauna. -
Subsurface Facies Analysis of the Devonian Berea Sandstone in Southeastern Ohio
SUBSURFACE FACIES ANALYSIS OF THE DEVONIAN BEREA SANDSTONE IN SOUTHEASTERN OHIO William T. Garnes A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE December 2014 Committee: James Evans, Advisor Jeffrey Snyder Charles Onasch ii ABSTRACT James Evans, Advisor The Devonian Berea Sandstone is an internally complex, heterogeneous unit that appears prominently both in outcrop and subsurface in Ohio. While the unit is clearly deltaic in outcrops in northeastern Ohio, its depositional setting is more problematic in southeastern Ohio where it is only found in the subsurface. The goal of this project was to search for evidence of a barrier island/inlet channel depositional environment for the Berea Sandstone to assess whether the Berea Sandstone was deposited under conditions in southeastern Ohio unique from northeastern Ohio. This project involved looking at cores from 5 wells: 3426 (Athens Co.), 3425 (Meigs Co.), 3253 (Athens Co.), 3252 (Athens Co.), and 3251 (Athens Co.) In cores, the Berea Sandstone ranges from 2 to 10 m (8-32 ft) thick, with an average thickness of 6.3 m (20.7 ft). Core descriptions involved hand specimens, thin section descriptions, and core photography. In addition to these 5 wells, the gamma ray logs from 13 wells were used to interpret the architecture and lithologies of the Berea Sandstone in Athens Co. and Meigs Co. as well as surrounding Vinton, Washington, and Morgan counties. Analysis from this study shows evidence of deltaic lobe progradation, abandonment, and re-working. Evidence of interdistributary bays with shallow sub-tidal environments, as well as large sand bodies, is also present. -
The Geology and Mineralization of the Grayback Mountains, Yavapai County, Arizona"
MJWii UflUJU he US I H x g University of Nevada Reno Mackay School of Mines J "The Geology and Mineralization of the Grayback Mountains, Yavapai County, Arizona" A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Geology By Michael Robert Kotraba April 1992 Signature Page Mackay School of Mines April 1992 ii Acknowledgements Many things go into the completion of a Masters Degree. Once you are given the opportunity to pursue the degree you need to find a thesis project and the support to complete the project. Without a doubt the most important support needed in this sort of endeavor comes from home. I would like to thank my wife, Julie and daughter, Kellie for their patience and support from start to finish. Many things were sacrificed for the opportunity to return to school for a Masters degree and I am thankful for their willingness to make those sacrifices. Support from other family members was also appreciated. Thanks goes to my dad for being a faithful field assistant and camp cook, and to my sister and brother-in-law for providing a place to stay and a vehicle to drive while out in the field. The opportunity and funding to make my pursuit of a Masters degree possible was given by Dr. L.T. Larson. Not only did he make the whole process possible but he also made it enjoyable. I truly appreciated his guidance, expertise, encouragement, and sense of humor. Thanks L.T.! The idea for this thesis grew out of conversations with the staff geologist at Cyprus Bagdad, Dr. -
Locational Factors Determining the Distribution of Nesting Sites for A
Edith Cowan University Research Online Theses : Honours Theses 1998 Locational factors determining the distribution of nesting sites for a colony of wedge-tailed shearwaters, puffinus pacificus, onest W Wallabi Island, Houtman Abrolhos, Western Australia Julie Davis Edith Cowan University Follow this and additional works at: https://ro.ecu.edu.au/theses_hons Part of the Ecology and Evolutionary Biology Commons, and the Ornithology Commons Recommended Citation Davis, J. (1998). Locational factors determining the distribution of nesting sites for a colony of wedge- tailed shearwaters, puffinus pacificus, onest W Wallabi Island, Houtman Abrolhos, Western Australia. https://ro.ecu.edu.au/theses_hons/473 This Thesis is posted at Research Online. https://ro.ecu.edu.au/theses_hons/473 Edith Cowan University Copyright Warning You may print or download ONE copy of this document for the purpose of your own research or study. The University does not authorize you to copy, communicate or otherwise make available electronically to any other person any copyright material contained on this site. You are reminded of the following: Copyright owners are entitled to take legal action against persons who infringe their copyright. A reproduction of material that is protected by copyright may be a copyright infringement. Where the reproduction of such material is done without attribution of authorship, with false attribution of authorship or the authorship is treated in a derogatory manner, this may be a breach of the author’s moral rights contained in Part IX of the Copyright Act 1968 (Cth). Courts have the power to impose a wide range of civil and criminal sanctions for infringement of copyright, infringement of moral rights and other offences under the Copyright Act 1968 (Cth). -
Arizona, Road Trips Are As Much About the Journey As They Are the Destination
Travel options that enable social distancing are more popular than ever. We’ve designated 2021 as the Year of the Road Trip so those who are ready to travel can start planning. In Arizona, road trips are as much about the journey as they are the destination. No matter where you go, you’re sure to spy sprawling expanses of nature and stunning panoramic views. We’re looking forward to sharing great itineraries that cover the whole state. From small-town streets to the unique landscapes of our parks, these road trips are designed with Grand Canyon National Park socially-distanced fun in mind. For visitor guidance due to COVID19 such as mask-wearing, a list of tourism-related re- openings or closures, and a link to public health guidelines, click here: https://www.visitarizona. com/covid-19/. Some attractions are open year-round and some are open seasonally or move to seasonal hours. To ensure the places you want to see are open on your travel dates, please check their website for hours of operation. Prickly Pear Cactus ARIZONA RESOURCES We provide complete travel information about destinations in Arizona. We offer our official state traveler’s guide, maps, images, familiarization trip assistance, itinerary suggestions and planning assistance along with lists of tour guides plus connections to ARIZONA lodging properties and other information at traveltrade.visitarizona.com Horseshoe Bend ARIZONA OFFICE OF TOURISM 100 N. 7th Ave., Suite 400, Phoenix, AZ 85007 | www.visitarizona.com Jessica Mitchell, Senior Travel Industry Marketing Manager | T: 602-364-4157 | E: [email protected] TRANSPORTATION From east to west both Interstate 40 and Interstate 10 cross the state.