Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, 1972
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Bedrock Geologic Map of the Northern Part of the Empire Ranch 7 ½' Quadrangle, Pima County, Arizona: Arizona Geological 0 0
Arizona Geological Survey OFR-09-05 (Empire Ranch Bedrock), v.1.0 110°45' 110°42'30" 110°40' 110°37'30" 524000 525000 526000 527000 528000 529000 530000 531000 532000 533000 534000 535000 BEDROCK GEOLOGIC MAP OF THE NORTHERN PART OF THE EMPIRE " 0 " 3 0 ' 3 2 ' RANCH 7 ½' QUADRANGLE, PIMA 5 2 ° 5 1 ° 3 1 3 COUNTY, ARIZONA by Ferguson, C.A. 0 0 0 0 0 0 6 6 2 2 August 2009 5 5 3 3 Arizona Geological Survey Open-File Report 09-05 (OFR-09-05), version 1.0 Citation for this map: Ferguson, C.A., 2009, Bedrock geologic map of the Northern Part of the Empire Ranch 7 ½' Quadrangle, Pima County, Arizona: Arizona Geological 0 0 0 0 Survey Open-File Report OFR-09-05, scale 1:24,000. 0 0 5 5 2 2 5 5 3 3 Research supported by the U.S. Geological Survey, National Cooperative Geologic Mapping Program, under assistance award number 08HQAG0093. The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government. 0 0 0 0 0 0 4 4 2 2 5 5 3 3 Map Symbol Descriptions Location Map 63 Mapped area shown in blue Horizontal bedding Eutaxitic foliation 15 Inclined bedding 31 Flow foliation 24 Inclined apparent bedding 19 Generic foliation 0 0 0 0 0 0 34 48 3 3 Upright bedding, facing indicators Cleavage 2 2 5 5 3 3 present at this location 39 Flow lineation 56 Overturned bedding 81 12 ÷ Paleocurrent direction determined Intersection lineation from imbricate clasts 5 Slickenline lineation 21 Joint 17 69 ' 0 0 0 ' Minor -
Lexicon of Geologic Names of Southern Arizona Larry Mayer, 1978, Pp
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/29 Lexicon of geologic names of southern Arizona Larry Mayer, 1978, pp. 143-156 in: Land of Cochise (Southeastern Arizona), Callender, J. F.; Wilt, J.; Clemons, R. E.; James, H. L.; [eds.], New Mexico Geological Society 29th Annual Fall Field Conference Guidebook, 348 p. This is one of many related papers that were included in the 1978 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Mid-Tertiary Geology and Geochronology of the Clifton-Morenci Area, Greenlee and Graham Counties, Arizona, and Adjacent New Mexico
Mid-Tertiary geology and geochronology of the Clifton-Morenci area, Greenlee and Graham Counties, Arizona, and adjacent New Mexico by Charles A. Ferguson1, M. Stephen Enders2, Lisa Peters3, and William C. McIntosh3 Arizona Geological Survey Open-file Report 00-07 August, 2000 Arizona Geological Survey 416 W. Congress, Suite 100, Tucson, AZ 85701 Also available in Adobe® PDF format with DI-18 and DGM-01 1 Arizona Geological Survey, 416 W. Congress, #100, Tucson, AZ 85701 email:[email protected] 2 Phelps Dodge Morenci, Inc., 4521 Highway 191, Morenci, AZ 85540 3 New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM 87801 Mid-Tertiary geology and geochronology of the Clifton- Morenci area, Greenlee and Graham Counties, Arizona, and adjacent New Mexico INTRODUCTION The geology of the Clifton-Morenci area has been investigated for nearly 100 years beginning with the pioneering work of W. Lindgren at the start of the 20th century. For most of the century, geological investigation focused on mineralization and the complex suite of Eocene porphyritic intrusive stocks and dikes in the area. Very little attention was directed at the regional structural and stratigraphic relationships in the overlying, and largely unmineralized Tertiary volcanic rocks. From the beginning, geologists have understood that supergene enrichment played a critical role in making the Morenci district a world class porphyry copper deposit (Lindgren, 1905a). For much of the past 90 years, enrichment was thought to have occurred during two phases of exposure and erosion: pre-volcanic and post-volcanic (Lindgren, 1905a; Moolick and Durek, 1966; Langton, 1973; North and Preece, 1993). -
BEDROCK GEOLOGIC MAP of the NORTHERN PART of the EMPIRE RANCH 7 1F2' QUADRANGLE, PIMA COUNTY, ARIZONA by Ferguson, C.A
BEDROCK GEOLOGIC MAP OF THE NORTHERN PART OF THE EMPIRE RANCH 7 1f2' QUADRANGLE, PIMA COUNTY, ARIZONA by Ferguson, C.A. August 2009 Arizona Geological Survey Open-File Report 09-05 (OFR-09-05), version 1.0 Disturbed areas (Holocene) - Areas distrubed by human activity; embackments, dams, dumps. Talus and colluvium (Quaternary) - Talus and colluvium Active Alluvium (Holocene) - Active alluvium Older alluvium (Quaternary) - Alluvium in terraces incised more than 3m. Gila Conglomerate (Miocene) -Boulder-cobble-pebble, clast-supported conglomerate and pebbly sandstone. Conglomerate occurs in fairly massive to very thick-bedded units with stratification defined by grain-size variations. Clasts are sub-angular to sub rounded , but also range to well-rounded. Assemblages range from monomict to oligomict with a wide variety of possible clasts, all derived from local sources. Clasts, in general order of abundance are: phenocryst-rich ash-flow tuff, arkosic sandstone, argillite, quartz sandstone and quartzite, limestone, andesitic volcanics, and two kinds of granitoid (Proterozoic, and late Cretaceous). Each of these are locally very abundant. Unit of North Canyon (Miocene Gila Group) - Oligomict to polymict conglomerate. Clasts of arkose and ash-flow tuff dominate in most areas, but this conglomerate also contains clasts of white porphyry (ranging from phenocryst-rich quartz-phyric to feldspar-phenocryst-poor), limestone, quartzite, and granodiorite. Unit of Adobe Tank (Miocene Gila Group) - Monomict to oligomict conglomerate dominated by clasts of arkose (Bisbee Group), and ash-flow tuff (rhyolite of Mt Fagan) in the west. To the east this conglomerate also contains, locally, light-colored granitoid clasts that match the Empire Mts Granite (Upper Cretaceous). -
GEOLOGIC MAP of the DUNCAN and CANADOR PEAK QUADRANGLES ARIZONA and NEW MEXICO by Roger B
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEOLOGIC MAP OF THE DUNCAN AND CANADOR PEAK QUADRANGLES ARIZONA AND NEW MEXICO By Roger B. Morrison' MISCELLANEOUS GEOLOGIC INVESTIGATIONS MAP 1-442 PUBLISHED BY THE U. S. GEOLOGICAL SURVEY WASHINGTON. D. C. 1965 DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-442 UNITED STATES GEOlOGICAl SURVEY GEOLOGIC MAP OF. T'HE DUNCAN AND CANADOR PEAK QUADRANGLES ARIZONA AND NE\V MEXICO By Roger B. Morrison PRECA.\1 BRIAN ROCKS Colorado, but the apparent maximum exposed thickness is at least 500 feet and possibly as much as 700 feet. GRANITE The lower part, about 230 feet thick, is gray to black The granite is red, pink, and pinkish gray, generally coarse generally calcareous shale, interlayered with a few to many grained and equigranular, but locally porphyritic. It is com black concretionary limestone beds. The middle part, about posed of red to pink feldspar-mostly microcline with 200 feet thick, consists of zones of olive-gray and gray to variable quantities of oligoclase and locally perthite locally black shale alternating with approximately equally quartz, and commonly small quantities of biotite. Pegmatite, thick zones of pale-gray to white locally pink and tan sand aplite, and diorite dikes and quartz veins occur locally. The stone that are well bedded to thick bedded and locally cross south and southwest boundaries of the granite area are bedded on a small ~cale. The upper part, about 100 feet faults having more than 4,000 feet <;fisplacement. thick, is mainly light-olive to black calcareous shale inter A profound erosion surface, probably of low relief, sep bedded with sandstone. -
Evolution of Deformation in the Buck Mountain Fault Damage Zone, Cambrian Flathead Sandstone, Teton Range, Wyoming Stephanie R
Pan-American Current Research on Fluid Inclusions Rice University, Houston, Texas, U.S.A., June 12-14, 2018, Abstract Volume Evolution of deformation in the Buck Mountain Fault damage zone, Cambrian Flathead Sandstone, Teton Range, Wyoming Stephanie R. FORSTNER, Stephen E. LAUBACH, András FALL Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas, U.S.A. E-mail: [email protected] The Teton Range is a normal fault block that contains older reverse faults (Love et al., 1992). Although generally considered to be Late Cretaceous to early Tertiary structures, the timing, kinematic style, and history of these faults is conjectural. Faults include the Forellen Peak Fault to the north, the Buck Mountain Reverse Fault (BMRF) to the west and south, and the Teton normal fault to the east (Love et al., 1992). The BMRF is rooted in Precambrian crystalline rocks and dips steeply to the east about 60°. The fractured Cambrian Flathead sandstone, an orthoquartzite (90%+ quartz), rests nonconformably on the Precambrian. Its stratigraphic position and relative isotropic mineralogy make the Flathead an ideal horizon for studying brittle deformation. Oriented Flathead hand samples were collected from the footwall of the BMRF along a partially overturned syncline (Figure 1). Continuous SEM-Cathodoluminescence (SEM-CL) scanlines of these samples allow for a systematic kinematic analysis of the cemented opening-mode fractures. We quantify attributes such as; geometry, spacing, orientation, and cross-cutting relationships. In isotropic rock, mode-I fractures primarily propagate along the plane perpendicular to Shmin; therefore, microfractures can be used to indicate paleostress trajectories, strain, and relative fracture timing (Anders et al., 2014; Hooker et al. -
Guidebook Contains Preliminary Findings of a Number of Concurrent Projects Being Worked on by the Trip Leaders
TH FRIENDS OF THE PLEISTOCENE, ROCKY MOUNTAIN-CELL, 45 FIELD CONFERENCE PLIO-PLEISTOCENE STRATIGRAPHY AND GEOMORPHOLOGY OF THE CENTRAL PART OF THE ALBUQUERQUE BASIN OCTOBER 12-14, 2001 SEAN D. CONNELL New Mexico Bureau of Geology and Mineral Resources-Albuquerque Office, New Mexico Institute of Mining and Technology, 2808 Central Ave. SE, Albuquerque, New Mexico 87106 DAVID W. LOVE New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM 87801 JOHN D. SORRELL Tribal Hydrologist, Pueblo of Isleta, P.O. Box 1270, Isleta, NM 87022 J. BRUCE J. HARRISON Dept. of Earth and Environmental Sciences, New Mexico Institute of Mining and Technology 801 Leroy Place, Socorro, NM 87801 Open-File Report 454C and D Initial Release: October 11, 2001 New Mexico Bureau of Geology and Mineral Resources New Mexico Institute of Mining and Technology 801 Leroy Place, Socorro, NM 87801 NMBGMR OFR454 C & D INTRODUCTION This field-guide accompanies the 45th annual Rocky Mountain Cell of the Friends of the Pleistocene (FOP), held at Isleta Lakes, New Mexico. The Friends of the Pleistocene is an informal gathering of Quaternary geologists, geomorphologists, and pedologists who meet annually in the field. The field guide has been separated into two parts. Part C (open-file report 454C) contains the three-days of road logs and stop descriptions. Part D (open-file report 454D) contains a collection of mini-papers relevant to field-trip stops. This field guide is a companion to open-file report 454A and 454B, which accompanied a field trip for the annual meeting of the Rocky Mountain/South Central Section of the Geological Society of America, held in Albuquerque in late April. -
(Ca. 1.45 Ga), WESTERN NORTH AMERICA: PSEUDOFOSSILS, FACIES, TIDES and SYNDEPOSITIONAL TECTONIC ACTIVITY in a MESOPROTEROZOIC INTRACRATONIC BASIN
SEDIMENTARY, MICROBIAL AND DEFORMATION FEATURES IN THE LOWER BELT SUPERGROUP (ca. 1.45 Ga), WESTERN NORTH AMERICA: PSEUDOFOSSILS, FACIES, TIDES AND SYNDEPOSITIONAL TECTONIC ACTIVITY IN A MESOPROTEROZOIC INTRACRATONIC BASIN A Thesis Submitted to the College of Graduate and Postdoctoral Studies In Partial Fulfillment of the Requirements For the Degree of Doctor of Philosophy In the Department of Geological Sciences University of Saskatchewan Saskatoon By Roy Gregory Rule © Copyright Roy Gregory Rule, July, 2020. All rights reserved. PERMISSION TO USE In presenting this thesis in partial fulfilment of the requirements for a Postgraduate degree from the University of Saskatchewan, I agree that the Libraries of this University may make it freely available for inspection. I further agree that permission for copying of this thesis in any manner, in whole or in part, for scholarly purposes may be granted by the professor or professors who supervised my thesis work or, in their absence, by the Head of the Department or the Dean of the College in which my thesis work was done. It is understood that any copying or publication or use of this thesis or parts thereof for financial gain shall not be allowed without my written permission. It is also understood that due recognition shall be given to me and to the University of Saskatchewan in any scholarly use which may be made of any material in my thesis. Requests for permission to copy or to make other uses of materials in this thesis in whole or part should be addressed to: Head of the Geological Sciences Geology Building University of Saskatchewan Saskatoon, Saskatchewan S7N 5E2, Canada Or Dean College of Graduate and Postdoctoral Studies University of Saskatchewan 116 Thorvaldson Building, 110 Science Place Saskatoon, Saskatchewan S7N 5C9, Canada i ABSTRACT Sedimentary, microbial and deformation features in the lower Belt Supergroup (ca. -
And Eastern Pennsylvania
GEOLOGY OF THE RIDGE AND VALLEY PROVINCE, NORTHWESTERN NEW JERSEY AND EASTERN PENNSYLVANIA JACK B. EPSTEIN U. S. Geological Survey, Reston, Va. 22092 INTRODUCTION The rocks seen in this segment of the field trip range A general transgressive-shelf sequence followed in age from Middle Ordovician to Middle Devonian and characterized mainly by tidal sediments and barrier bars constitute a.deep basin-continental-shallow shelf succes (Poxono Island, Bossardville, Decker, Rondout)~ suc sion. Within this succession, three lithotectonic units, or ceeded by generally subtidal and bar deposits (Helder sequences of rock that were deformed semi burg and Oriskany Groups), and then by deeper sub independently of each other, have somewhat different tidal deposits (Esopus, . Schoharie. and Buttermilk structural characteristics. Both the Alleghenian and Falls), finally giving way to another deep~water to Taconic orogenies have left their imprint on the rocks. shoaling sequence (Marcellus Shale through the Catskill Wind and water gaps are structurally controlled, thus Formation). Rocks of the Marcellus through Catskill placing doubt upon the hypothesis of regional super will not be seen on this trip. position. Wisconsinan deposits and erosion effects are common. We will examine these geologic features as This vertical stratigraphic sequence is complicated a well as some of the economic deposits in the area. bit because most Upper Silurian and Lower Devonian units are much thinner or are absent toward a paleo Figure 1 is an index map of the field-trip area, show positive area a few tens of miles southwest of the field ing the trip route and quadrangle coverage. Figure 2 is a trip area. -
How the Gap Formed
Delaware Water Gap National Recreation Area How the Gap formed What is a water gap? Several words in the English language The Delaware Water Gap is justly famous for denote a “break” or “cleft” in the moun- its depth, width, and scenic beauty. The Gap tains. Chasm and notch are popular in New is a mile wide from New Jersey’s Mount England; pass and gorge in the South and Tammany (1,527 feet) to Pennsylvania’s West of the United States. Gap is especially Mount Minsi (1,463 feet.) The Gap is about common in this part of the country. 1,200 feet deep from the tops of these mountains to the surface of the river, which A gap or wind gap is a break or pass through at this point is 290 feet above sea level. The the mountains, in this case the Appalachian maximum depth of the river at the Gap is Mountains. A water gap is a pass that a river about 55 feet. runs through. How does a gap form? Geology is the study of the earth’s forma- Starting with Native American legend, there tion. Though the geologist’s time frame may have been many ideas about how the seem vast and remote, the results of Delaware Water Gap formed. One current geological processes are the mountains we theory explains the Gap through a series of hike on, the river we swim in, and the processes: continental shift (involving plate scenery we admire. tectonics), mountain building (orogeny), erosion, and the “capturing” of rivers and streams. -
Glacier National Park Geologic Resource Evaluation Report
National Park Service U.S. Department of the Interior Geologic Resources Division Denver, Colorado Glacier National Park Geologic Resource Evaluation Report Glacier National Park Geologic Resource Evaluation Geologic Resources Division Denver, Colorado U.S. Department of the Interior Washington, DC Table of Contents List of Figures .............................................................................................................. iv Executive Summary ...................................................................................................... 1 Introduction ................................................................................................................... 3 Purpose of the Geologic Resource Evaluation Program ............................................................................................3 Geologic Setting .........................................................................................................................................................3 Glacial Setting ............................................................................................................................................................4 Geologic Issues............................................................................................................. 9 Economic Resources..................................................................................................................................................9 Mining Issues..............................................................................................................................................................9 -
White Grass Stories from the National Trust for Historic Preservation Web Site - Downloaded May 2014
White Grass Stories from the National Trust for Historic Preservation Web Site - Downloaded May 2014 “Share Your Story” The entries below are from a web site established by the National Trust for Historical Preservation as a supplement to its fund raising efforts to support the rehabilitation work at the historic White Grass Ranch, Grand Teton National Park, Moose, Wyoming. Called “Share Your Story,” former dudes, wranglers and special friends of the dude ranch era (1913-1985) were invited to enter a story/post a story on the Trust’s web site. The site was taken down in 2014 after the Trust closed its fundraising efforts having met its goal of over $970,000. Through an agreement with the National Trust, the White Grass Heritage Project is able to archive and republish those stories, and preserve an important part of White Grass Ranch history. NOTE: When the individual stories below were first posted on the National Trust’s web site, some posting dates were inaccurate due to a computer glitch. Information contained in “White Grass Ranch: A Compilation of Stories from the National Trust for Historic Preservation Website and More, 2014” created by Rachel Terhune was used to correct noted inaccuracies. Terhune’s booklet is archived in the Grand Teton National Park and the Jackson Hole Historical Society and Museum in Jackson, Wyoming Edited by Roger Butterbaugh, Seasonal Caretaker at White Grass Ranch/National Park Service Volunteer; Coordinator of the White Grass Heritage Project which aims to collect oral histories, historical photos, artifacts and more for archival purposes at the Grand Teton National Park and the Jackson Hole Historical Society and Museum -- March 25, 2016.