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The Lower Gila Region, Arizona
DEPARTMENT OF THE INTERIOR HUBERT WORK, Secretary UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, Director Water-Supply Paper 498 THE LOWER GILA REGION, ARIZONA A GEOGBAPHIC, GEOLOGIC, AND HTDBOLOGIC BECONNAISSANCE WITH A GUIDE TO DESEET WATEEING PIACES BY CLYDE P. ROSS WASHINGTON GOVERNMENT PRINTING OFFICE 1923 ADDITIONAL COPIES OF THIS PUBLICATION MAT BE PROCURED FROM THE SUPERINTENDENT OF DOCUMENTS GOVERNMENT PRINTING OFFICE WASHINGTON, D. C. AT 50 CENTS PEE COPY PURCHASER AGREES NOT TO RESELL OR DISTRIBUTE THIS COPT FOR PROFIT. PUB. RES. 57, APPROVED MAT 11, 1822 CONTENTS. I Page. Preface, by O. E. Melnzer_____________ __ xr Introduction_ _ ___ __ _ 1 Location and extent of the region_____._________ _ J. Scope of the report- 1 Plan _________________________________ 1 General chapters _ __ ___ _ '. , 1 ' Route'descriptions and logs ___ __ _ 2 Chapter on watering places _ , 3 Maps_____________,_______,_______._____ 3 Acknowledgments ______________'- __________,______ 4 General features of the region___ _ ______ _ ., _ _ 4 Climate__,_______________________________ 4 History _____'_____________________________,_ 7 Industrial development___ ____ _ _ _ __ _ 12 Mining __________________________________ 12 Agriculture__-_______'.____________________ 13 Stock raising __ 15 Flora _____________________________________ 15 Fauna _________________________ ,_________ 16 Topography . _ ___ _, 17 Geology_____________ _ _ '. ___ 19 Bock formations. _ _ '. __ '_ ----,----- 20 Basal complex___________, _____ 1 L __. 20 Tertiary lavas ___________________ _____ 21 Tertiary sedimentary formations___T_____1___,r 23 Quaternary sedimentary formations _'__ _ r- 24 > Quaternary basalt ______________._________ 27 Structure _______________________ ______ 27 Geologic history _____ _____________ _ _____ 28 Early pre-Cambrian time______________________ . -
Grand Enchantment Trail Guide
published on the Grand Enchantment Trail website www.simblissity.net | © Brett Tucker G.E.T. Guidebook Segment 10: Pinaleño Mountains 25.9 miles Segment Length Segment Status Season 25.9 mi. finalized & accessible spring, summer, fall Resources OVERVIEW MAP ELEVATION PROFILE Additional maps: Coronado N.F. Safford & Santa Catalina Ranger Districts (USFS) Land management agency: Coronado National Forest Safford Ranger District G.E.T. Topo Maps 30-32 Water Chart Image Gallery: Album 3 Beginning access point Ending access point FR 286 at FR 675. From Safford, take US 70 west to FR 307 at Ash Creek Trailhead. From Safford, follow Pima and turn left at sign for Tripp Canyon Road / FR US 70 west to Pima, then take Main St south to its end. 286. Reach an intersection with Patterson Mesa Rd Turn right on Cottonwood Rd, then left on dirt 2WD Cluff within a half mile and turn left. FR 286 resumes at Ranch Rd. Reach Cluff Ranch wildlife management area right within a quarter mile, marked by metal signs in 4 mi, where 2WD vehicles should park (~5 mi before (brief easement through private land). A large the actual Ending Access Point for Seg 10). Suitable swinging gate soon encountered should be left as it high-clearance vehicles such as Jeeps may continue on was found. Proceed southwest on dirt 2WD FR 286. Cluff Ranch Rd. Keep left at the fork by main entrance to In ~15 miles from Pima reach a junction with 4WD FR Cluff Ranch, then turn left at a 3-way junction onto 351. -
Southwest NM Publication List
Southwest New Mexico Publication Inventory Draft Source of Document/Search Purchase Topic Category Keywords County Title Author Date Publication/Journal/Publisher Type of Document Method Price Geology 1 Geology geology, seismic Southwestern NM Six regionally extensive upper-crustal Ackermann, H.D., L.W. 1994 U.S. Geological Survey, Open-File Report 94- Electronic file USGS publication search refraction profiles, seismic refraction profiles in Southwest New Pankratz, D.P. Klein 695 (DJVU) http://pubs.er.usgs.gov/usgspubs/ southwestern New Mexico ofr/ofr94695 Mexico, 2 Geology Geology, Southwestern NM Magmatism and metamorphism at 1.46 Ga in Amato, J.M., A.O. 2008 In New Mexico Geological Society Fall Field Paper in Book http://nmgs.nmt.edu/publications/g $45.00 magmatism, the Burro Mountains, southwestern New Boullion, and A.E. Conference Guidebook - 59, Geology of the Gila uidebooks/59/ metamorphism, Mexico Sanders Wilderness-Silver City area, 107-116. Burro Mountains, southwestern New Mexico 3 Geology Geology, mineral Catron County Geology and mineral resources of York Anderson, O.J. 1986 New Mexico Bureau of Mines and Mineral Electronic file (PDF) NMBGMR search $10.00 for resources, York Ranch SE quadrangle, Cibola and Catron Resources Open File Report 220A, 22 pages. <http://geoinfo.nmt.edu/publicatio CD Ranch, Fence Counties, New Mexico ns/openfile/details.cfml?Volume=2 Lake, Catron, 20A> Cibola 4 Geology Geology, Zuni Salt Catron County Geology of the Zuni Salt Lake 7 1/2 Minute Anderson, O.J. 1994 New Mexico Bureau of Mines and -
Cenozoic Thermal, Mechanical and Tectonic Evolution of the Rio Grande Rift
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 91, NO. B6, PAGES 6263-6276, MAY 10, 1986 Cenozoic Thermal, Mechanical and Tectonic Evolution of the Rio Grande Rift PAUL MORGAN1 Departmentof Geosciences,Purdue University,West Lafayette, Indiana WILLIAM R. SEAGER Departmentof Earth Sciences,New Mexico State University,Las Cruces MATTHEW P. GOLOMBEK Jet PropulsionLaboratory, CaliforniaInstitute of Technology,Pasadena Careful documentationof the Cenozoicgeologic history of the Rio Grande rift in New Mexico reveals a complexsequence of events.At least two phasesof extensionhave been identified.An early phase of extensionbegan in the mid-Oligocene(about 30 Ma) and may have continuedto the early Miocene (about 18 Ma). This phaseof extensionwas characterizedby local high-strainextension events (locally, 50-100%,regionally, 30-50%), low-anglefaulting, and the developmentof broad, relativelyshallow basins, all indicatingan approximatelyNE-SW •-25ø extensiondirection, consistent with the regionalstress field at that time.Extension events were not synchronousduring early phase extension and were often temporally and spatiallyassociated with major magmatism.A late phaseof extensionoccurred primarily in the late Miocene(10-5 Ma) with minor extensioncontinuing to the present.It was characterizedby apparently synchronous,high-angle faulting givinglarge verticalstrains with relativelyminor lateral strain (5-20%) whichproduced the moderuRio Granderift morphology.Extension direction was approximatelyE-W, consistentwith the contemporaryregional stress field. Late phasegraben or half-grabenbasins cut and often obscureearly phasebroad basins.Early phase extensionalstyle and basin formation indicate a ductilelithosphere, and this extensionoccurred during the climax of Paleogenemagmatic activity in this zone.Late phaseextensional style indicates a more brittle lithosphere,and this extensionfollowed a middle Miocenelull in volcanism.Regional uplift of about1 km appearsto haveaccompanied late phase extension, andrelatively minor volcanism has continued to thepresent. -
Geologic Resources Inventory Map Document for Gila Cliff Dwellings National Monument
U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Directorate Geologic Resources Division Gila Cliff Dwellings National Monument GRI Ancillary Map Information Document Produced to accompany the Geologic Resources Inventory (GRI) Digital Geologic Data for Gila Cliff Dwellings National Monument gicl_geology.pdf Version: 8/11/2014 I Gila Cliff Dwellings National Monument Geologic Resources Inventory Map Document for Gila Cliff Dwellings National Monument Table of Contents Geolog.i.c. .R...e..s.o..u..r.c..e..s.. .I.n..v.e..n..t.o..r..y. .M...a..p.. .D..o..c..u..m...e..n..t....................................................................... 1 About th..e.. .N...P..S.. .G...e..o..l.o..g..i.c. .R...e..s.o..u..r.c..e..s.. .I.n..v.e..n..t.o..r..y. .P...r.o..g..r.a..m........................................................... 2 GRI Dig.i.t.a..l. .M...a..p.. .a..n..d.. .S..o..u..r.c..e.. .M...a..p.. .C..i.t.a..t.i.o..n..s............................................................................. 4 GRI Dig.i.t.a..l. .G...e..o..l.o..g..i.c. .M...a..p.. .o..f. .G...i.l.a.. .C..l.i.f.f. .D..w...e..l.l.i.n..g..s. .N...a..t.i.o..n..a..l. .M..o..n..u..m...e..n..t.................................... 5 Map Un..it. .L..i.s..t................................................................................................................................................................. 5 Map Un..it. .D...e..s..c..r.i.p..t.io..n..s.................................................................................................................................................... 5 Qa - A..l.l.u..v..iu..m.. -
U.S. Department of the Interior U.S. Geological Survey
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Prepared in cooperation with New Mexico Bureau of Mines and Mineral Resources 1997 MINERAL AND ENERGY RESOURCES OF THE MIMBRES RESOURCE AREA IN SOUTHWESTERN NEW MEXICO This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Cover: View looking south to the east side of the northeastern Organ Mountains near Augustin Pass, White Sands Missile Range, New Mexico. Town of White Sands in distance. (Photo by Susan Bartsch-Winkler, 1995.) MINERAL AND ENERGY RESOURCES OF THE MIMBRES RESOURCE AREA IN SOUTHWESTERN NEW MEXICO By SUSAN BARTSCH-WINKLER, Editor ____________________________________________________ U. S GEOLOGICAL SURVEY OPEN-FILE REPORT 97-521 U.S. Geological Survey Prepared in cooperation with New Mexico Bureau of Mines and Mineral Resources, Socorro U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Mark Shaefer, Interim Director For sale by U.S. Geological Survey, Information Service Center Box 25286, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government MINERAL AND ENERGY RESOURCES OF THE MIMBRES RESOURCE AREA IN SOUTHWESTERN NEW MEXICO Susan Bartsch-Winkler, Editor Summary Mimbres Resource Area is within the Basin and Range physiographic province of southwestern New Mexico that includes generally north- to northwest-trending mountain ranges composed of uplifted, faulted, and intruded strata ranging in age from Precambrian to Recent. -
The Mogollon-Datil Volcanic Field, Southwestern New Mexico Wolfgang E
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/59 When batholiths exploded: The Mogollon-Datil volcanic field, southwestern New Mexico Wolfgang E. (Wolf) Elston, 2008, pp. 117-128 in: Geology of the Gila Wilderness-Silver City area, Mack, Greg, Witcher, James, Lueth, Virgil W.; [eds.], New Mexico Geological Society 59th Annual Fall Field Conference Guidebook, 210 p. This is one of many related papers that were included in the 2008 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. -
Jaguar Critical Habitat Comments in Response to 71 FR 50214-50242 (Aug
October 19, 2012 Submitted on-line via www.regulations.gov, Docket No. FWS-R2-ES-2012-0042. Re: Jaguar critical habitat comments in response to 71 FR 50214-50242 (Aug. 20, 2012). To Whom it May Concern, The Center for Biological Diversity supports the designation of the entirety of the areas that the Fish and Wildlife Service proposes as critical habitat. However, these areas are not sufficient to conserve the jaguar in the United States. Nor does the Service’s itemization of threats to critical habitat areas cover the array of actions that would in fact destroy or adversely modify them. As we explain in detail in the comments below and through evidence presented in our appended letter of 10/1/2012 on the Recovery Outline for the Jaguar, we request seven principal changes in the final critical habitat designation rule, as follows: 1. The following additional mountain ranges within the current boundary of the Northwestern Recovery Unit (as described in the April 2012 Recovery Outline for the Jaguar) should be designated as critical habitat: in Arizona, the Chiricahua, Dos Cabezas, Dragoon and Mule mountains, and in New Mexico the Animas and adjoining Pyramid mountains. 2. The following additional “sky island” mountain ranges outside of the current boundaries of the Northwestern Recovery Unit should be designated as critical habitat: In New Mexico, the Alama Hueco, Big Hatchet, Little Hatchet, Florida, West and East Potrillo, Cedar and Big Burro mountains; in Arizona, the Galiuro, Santa Teresa, Pinaleno, Whitlock, Santa Catalina and Rincon mountains. Straddling both states, the Peloncillo Mountains north of the current boundaries of the Northwestern Recovery Unit should also be designated 3. -
Oldsmokeys Newsletter Newsletter of the Pacific Northwest Forest Service Retirees—Winter 2017
OldSmokeys Newsletter Newsletter of the Pacific Northwest Forest Service Retirees—Winter 2017 President’s Message—Ron Boehm As I write this message it is approaching Thanksgiving Day and I am reflecting on the many things for which we have to be thankful. Among them we did not have to help any OldSmokeys, their families, or current Forest Service folks with our Elmer Moyer Emer- gency Relief Fund this year! That fund remains healthy at slightly more than $12,000 for if and when it is needed. In our approved 2017 budget, we were able to allocate $10,000 for our Project/Grant Fund. Our Nominating Committee was able to convince Kent Connaughton to agree to serve as President-Elect. Please see the article and send in the ballot on page 3. Thank you Bob Devlin, Linda Goodman, and Mike Ash for your good work! Speaking of good work, our Board of Directors has continued their good work through this year. See who they are and what they do on page 16. Also, a big THANK YOU to Les Joslin for this newsletter and the other 43 issues he has produced over the past 10-plus years. Here is a request from Les in his own words: “This will be the 44th issue of this newsletter I will have produced since assuming this job from Wendall Jones with the Spring 2006 issue. While I may have a few more issues left in me, I think you will agree it is time for a change and time for the PNWFSA to recruit a new editor. -
Gila National Forest - Forest Plan Revision
Forest Plan Revision Overview The Forest Plan is the comprehensive document guiding management for all resources on the National Forest for the next 15 years or more An opportunity for your knowledge and suggestions to be heard and shape the Forest’s future management Policy requires that forest plans be revised periodically. The Forest and surrounding areas have experienced significant changes since 1986 when the existing plan was approved. THREE PHASES 1.Assessment (1.5 years) 2.Plan Revision (~3 years) 3.Implementation and Monitoring (15+ years) How can you help? Be an active stakeholder in developing a future vision for the forest Your input will help develop plan direction that will provide for a healthy, diverse, and productive Forest in addition to the many benefits and uses desired by local communities and visitors of today and future generations. For more information, please visit our website http://go.usa.gov/h88k Gila National Forest - Forest Plan Revision Road Map Dates are anticipated and subject to change Assessment Initial Stakeholder Forest Plan Revision Steps Engagement Needs for Initial Change Plan Communication and Identified outreach and Develop Draft Plan Public Review of Selection of Preferred Implementation Notice of Collaboration Plan engagement and Monitoring Draft Plan/DEIS Alternative and Monitoring Intent (NOI) Program to Initiate Science Synthesis Assessment Response to BA/BE and Consultation with US Assessment Report Publicly Develop Comments and Fish and Wildlife Existing Conditions Available Alternatives -
Estimated Probability of Postwildfire Debris Flows in the 2012 Whitewater–Baldy Fire Burn Area, Southwestern New Mexico
Prepared in cooperation with U.S. Department of Agriculture Forest Service, Gila National Forest Estimated Probability of Postwildfire Debris Flows in the 2012 Whitewater–Baldy Fire Burn Area, Southwestern New Mexico Open-File Report 2012–1188 U.S. Department of the Interior U.S. Geological Survey Cover: Left, The Sandy Point staging area for aerial mulching, Gila National Forest, N. Mex. (photograph by U.S. Forest Service). Right, Crews clearing log jam in Copper Creek, Gila National Forest, N. Mex. (photograph by U.S. Forest Service). Background, View of the Whitewater–Baldy Complex oriented east from U.S. Route 180, May 23, 2012, Gila National Forest, N. Mex. (photograph by U.S. Forest Service). Estimated Probability of Postwildfire Debris Flows in the 2012 Whitewater– Baldy Fire Burn Area, Southwestern New Mexico By Anne C. Tillery, Anne Marie Matherne, and Kristine L. Verdin Prepared in cooperation with U.S. Department of Agriculture Forest Service, Gila National Forest Open-File Report 2012–1188 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 This and other USGS information products are available at http://store.usgs.gov/ U.S. Geological Survey Box 25286, Denver Federal Center Denver, CO 80225 To learn about the USGS and its information products visit http://www.usgs.gov/ 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. -
Whitewater Baldy Complex Burned Area Emergency Response (BAER) Team Executive Summary
6/18/2012 Whitewater Baldy Complex Burned Area Emergency Response (BAER) Team Executive Summary Glenwood, Reserve, Black Range, and Wilderness Ranger Districts Gila National Forest Silver City, New Mexico June 18, 2012 1 6/18/2012 Executive Summary Introduction In May and June of 2012, the Whitewater Baldy Complex burned approximately 290,000 acres (117,359 hectares) of the Glenwood, Reserve, Wilderness, and Black Range Ranger Districts of the Gila National Forest. The Fire started as two separate lightning strike fires near Mogollon Baldy and in the headwaters of Whitewater Creek in the Gila Wilderness east of Glenwood NM. The two fires joined in extreme fire behavior on 5/23/2012 to form the Whitewater Baldy Complex. The fire severely burned a large tract of land across the Gila National Forest and the Gila Wilderness, including the headwaters of Whitewater Creek, Mineral Creek, and Gilita Creek that drain directly into the communities of Glenwood, Alma, and Willow Creek respectively. All of these population centers are situated in the floodplains of drainages affected by the fire. Much of the vegetation, duff and soil that once served to slow and hold water were eliminated as a result of the fire. Steep slopes further aggravate the situation. In fact, the Whitewater Baldy Complex Fire BAER team has modeled and predicted post-fire peak flows for a 25 year 6 hour precipitation event at 140 times the pre-fire flow in Willow Creek. Post-fire flows from a 25 year precipitation event are expected to increase 2-4 times in most of the affected drainages.