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CEMOZOIC DEPOSITS in the SOUTHERN FOOTHILLS of the SANTA CATALINA MOUNTAINS NEAR TUCSON, ARIZONA Ty Klaus Voelger a Thesis Submi
Cenozoic deposits in the southern foothills of the Santa Catalina Mountains near Tucson, Arizona Item Type text; Thesis-Reproduction (electronic) Authors Voelger, Klaus, 1926- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 25/09/2021 10:53:10 Link to Item http://hdl.handle.net/10150/551218 CEMOZOIC DEPOSITS IN THE SOUTHERN FOOTHILLS OF THE SANTA CATALINA MOUNTAINS NEAR TUCSON, ARIZONA ty Klaus Voelger A Thesis submitted to the faculty of the Department of Geology in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in the Graduate College, University of Arizona 1953 Approved; , / 9S~J Director of Thesis ^5ate Univ. of Arizona Library The research on which this thesis is based was com pleted by Mr. Klaus Voelger of Berlin, Germany, while he was studying at the University of Arizona under the program of the Institute of International Education. The final draft was written after Mr. Voelgerf s return to his home in the Russian-occupied zone of Berlin. Difficulties such as a shortage of typing paper of uniform grade and the impossibility of adequate supervision and advice on matters of terminology, punctuation, and English usage account for certain details in which this thesis may depart from stand ards of the Graduate College of the University of Arizona. These details are largely mechanical, and it is felt that they do not detract appreciably from the quality of the research nor the clarity of presentation of the results. -
A GUIDE to the GEOLOGY of the Santa Catalina Mountains, Arizona: the Geology and Life Zones of a Madrean Sky Island
A GUIDE TO THE GEOLOGY OF THE SANTA CATALINA MOUNTAINS, ARIZONA: THE GEOLOGY AND LIFE ZONES OF A MADREAN SKY ISLAND ARIZONA GEOLOGICAL SURVEY 22 JOHN V. BEZY Inside front cover. Sabino Canyon, 30 December 2010. (Megan McCormick, flickr.com (CC BY 2.0). A Guide to the Geology of the Santa Catalina Mountains, Arizona: The Geology and Life Zones of a Madrean Sky Island John V. Bezy Arizona Geological Survey Down-to-Earth 22 Copyright©2016, Arizona Geological Survey All rights reserved Book design: M. Conway & S. Mar Photos: Dr. Larry Fellows, Dr. Anthony Lux and Dr. John Bezy unless otherwise noted Printed in the United States of America Permission is granted for individuals to make single copies for their personal use in research, study or teaching, and to use short quotes, figures, or tables, from this publication for publication in scientific books and journals, provided that the source of the information is appropriately cited. This consent does not extend to other kinds of copying for general distribution, for advertising or promotional purposes, for creating new or collective works, or for resale. The reproduction of multiple copies and the use of articles or extracts for comer- cial purposes require specific permission from the Arizona Geological Survey. Published by the Arizona Geological Survey 416 W. Congress, #100, Tucson, AZ 85701 www.azgs.az.gov Cover photo: Pinnacles at Catalina State Park, Courtesy of Dr. Anthony Lux ISBN 978-0-9854798-2-4 Citation: Bezy, J.V., 2016, A Guide to the Geology of the Santa Catalina Mountains, Arizona: The Geology and Life Zones of a Madrean Sky Island. -
Coconino National Forest Draft Land Management Plan – February 2011 Iii
United States Coconino National Department of Agriculture Forest Forest Draft Land Service Southwestern Region Management Plan February 2011 Notes for reviewers: • This document is an initial draft of the Coconino National Forest’s revised land management plan. It was made available for public review in February 2011. • Language highlighted in gray is incomplete or needs further attention. Draft Revised Land Management Plan Prepared for: The Coconino National Forest 1824 S. Thompson St. Flagstaff, AZ 86001 and USDA Forest Service Southwestern Region 333 Broadway SE Albuquerque, New Mexico 87102 Submitted by: Plan Revision Team Coconino National Forest Contents Draft Revised Land Management Plan ........... i Chapter 1. Background ................................................................................................................. 1 Introduction ............................................................................................................................... 1 Purpose of the Land Management Plan .................................................................................... 1 Summary of the Analysis of the Management Situation ........................................................... 1 Plan Content .............................................................................................................................. 2 Plan Decisions ..................................................................................................................... 2 Other Content ..................................................................................................................... -
Mammals of the Rincon Mountain District, Saguaro National Park
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Mammals of the Rincon Mountain District, Saguaro National Park Natural Resource Report NPS/SODN/NRR—2011/437 ON THE COVER Jaguar killed in Rincon Mountains in 1902, photographed at saloon in downtown Tucson. Photograph courtesy Arizona Historical Society. Mammals of the Rincon Mountain District, Saguaro National Park Natural Resource Report NPS/SODN/NRR—2011/437 Author Don E. Swann With contributions by Melanie Bucci, Matthew Caron, Matthew Daniels, Ronnie Sidner, Sandy A. Wolf, and Erin R. Zylstra Saguaro National Park 3693 South Old Spanish Trail Tucson, Arizona 85730-5601 Editing and Design Alice Wondrak Biel Sonoran Desert Network 7660 E. Broadway Blvd., Suite 303 Tucson, AZ 85710 August 2011 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service’s Natural Resource Stewardship and Science offi ce, in Fort Collins, Colo- rado, publishes a range of reports that address natural resource topics of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the informa- tion is scientifi cally credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. -
Historical Stand-Replacing Fire in Upper Montane Forests of the Madrean Sky Islands and Mogollon Plateau, Southwestern USA
Fire Ecology Volume 7, Issue 3, 2011 Margolis et al.: Historical Stand-Replacing Fire doi: 10.4996/fireecology.0703088 Page 88 RESEARCH ARTICLE HISTORICAL STAND-REPLACING FIRE IN UPPER MONTANE FORESTS OF THE MADREAN SKY ISLANDS AND MOGOLLON PLATEAU, SOUTHWESTERN USA Ellis Q. Margolis1*, Thomas W. Swetnam1, and Craig D. Allen2 1University of Arizona Laboratory of Tree-Ring Research, 105 W. Stadium, Tucson, Arizona 85721, USA 2US Geological Survey Jemez Mountains Field Station, HCR 1, Box 1, Number 15, Los Alamos, New Mexico 87544, USA *Corresponding author: Tel.: 001-520-626-2733; e-mail: [email protected] ABSTRACT The recent occurrence of large fires with a substantial stand-replacing component in the southwestern United States (e.g., Cerro Grande, 2000; Rodeo-Chedeski, 2002; Aspen, 2003; Horseshoe 2, Las Conchas, and Wallow, 2011) has raised questions about the his- torical role of stand-replacing fire in the region. We reconstructed fire dates and stand-re- placing fire patch sizes using four lines of tree-ring evidence at four upper montane forest sites (>2600 m) in the Madrean Sky Islands and Mogollon Plateau of Arizona and New Mexico, USA. The four lines of tree-ring evidence include: (1) quaking aspen (Populus tremuloides) and spruce-fir age structure, (2) conifer death dates, (3) traumatic resin ducts and ring-width changes, and (4) conifer fire scars. Pre-1905 fire regimes in the upper montane forest sites were variable, with drier, south-facing portions of some sites record- ing frequent, low-severity fire (mean fire interval of all fires ranging from 5 yr to 11 yr among sites), others burning with stand-replacing severity, and others with no evidence of fire for >300 yr. -
Coronado National Forest
CORONADO NATIONAL FOREST FIRE MANAGEMENT PLAN Reviewed and Updated by _/s/ Chris Stetson ___________ Date __5/18/10 __________ Coronado Fire Management Plan Interagency Federal fire policy requires that every area with burnable vegetation must have a Fire Management Plan (FMP). This FMP provides information concerning the fire process for the Coronado National Forest and compiles guidance from existing sources such as but not limited to, the Coronado National Forest Land and Resource Management Plan (LRMP), national policy, and national and regional directives. The potential consequences to firefighter and public safety and welfare, natural and cultural resources, and values to be protected help determine the management response to wildfire. Firefighter and public safety are the first consideration and are always the priority during every response to wildfire. The following chapters discuss broad forest and specific Fire Management Unit (FMU) characteristics and guidance. Chapter 1 introduces the area covered by the FMP, includes a map of the Coronado National Forest, addresses the agencies involved, and states why the forest is developing the FMP. Chapter 2 establishes the link between higher-level planning documents, legislation, and policies and the actions described in FMP. Chapter 3 articulates specific goals, objectives, standards, guidelines, and/or desired future condition(s), as established in the forest’s LRMP, which apply to all the forest’s FMUs and those that are unique to the forest’s individual FMUs. Page 1 of 30 Coronado Fire Management Plan Chapter 1. INTRODUCTION The Coronado National Forest developed this FMP as a decision support tool to help fire personnel and decision makers determine the response to an unplanned ignition. -
Density and Elevational Distribution of the San Francisco Peaks Ragwort, Packera Franciscana (Asteraceae), a Threatened Single-Mountain Endemic
MADRON˜ O, Vol. 57, No. 4, pp. 213–219, 2010 DENSITY AND ELEVATIONAL DISTRIBUTION OF THE SAN FRANCISCO PEAKS RAGWORT, PACKERA FRANCISCANA (ASTERACEAE), A THREATENED SINGLE-MOUNTAIN ENDEMIC JAMES F. FOWLER AND CAROLYN HULL SIEG USFS Rocky Mountain Research Station, 2500 S Pine Knoll Drive, Flagstaff, AZ 86001 [email protected] ABSTRACT Packera franciscana (Greene) W. A. Weber and A. Lo¨ve is endemic to treeline and alpine habitats of the San Francisco Peaks, Arizona, USA and was listed as a threatened species under the Endangered Species Act in 1983. Species abundance data are limited in scope, yet are critical for recovery of the species, especially in light of predictions of its future extinction due to climate change. This study defined baseline population densities along two transects which will allow the detection of future population trends. Packera franciscana ranged from 3529 to 3722 m elevation along the outer slope transect and densities were 4.18 and 2.74 ramets m22 in 2008 and 2009, respectively. The overall P. franciscana 2009 density estimate for both transects was 4.36 ramets m22 within its elevational range of occurrence, 3471–3722 m. The inner basin density was higher, 5.62 ramets m22, than the estimate for outer slopes, 2.89 ramets m22. The elevation of the 2009 population centroid for both transects was at 3586 (610 SE) m with the inner basin centroid significantly lower than the outer slopes centroid: 3547 (67 SE) m vs. 3638 (67 SE) m, respectively. In mid-September, 6–9% of the P. franciscana ramets were flowering and/or fruiting in 2008–2009. -
Fire Facility Sunset Crater Volcano National Monument Coconino County, Arizona
National Park Service Sunset Crater Volcano U.S. Department of the Interior Sunset Crater Volcano National Monument Arizona Fire Facility Sunset Crater Volcano National Monument Coconino County, Arizona Environmental Assessment / Assessment of Effect June 2006 Note to Reviewers and Respondents If you wish to comment on the environmental assessment, you may mail comments to the name and address below or post comments online at http://parkplanning.nps.gov/. This environmental assessment will be on public review for 30 days. It is the practice of the NPS to make all comments, including names and addresses of respondents who provide that information, available for public review following the conclusion of the environmental assessment process. Individuals may request that the NPS withhold their name and/or address from public disclosure. If you wish to do this, you must state this prominently at the beginning of your comment. Commentators using the website can make such a request by checking the box "keep my contact information private." NPS will honor such requests to the extent allowable by law, but you should be aware that NPS may still be required to disclose your name and address pursuant to the Freedom of Information Act. We will make all submissions from organizations, businesses, and from individuals identifying themselves as representatives or officials of organizations or businesses available for public inspection in their entirety. Please Address Comments to: Flagstaff Area National Monuments Attn: Scott Travis, Superintendent 6400 N. Hwy 89 Flagstaff, Arizona 86004 EXPERIENCE YOUR AMERICA Summary The National Park Service (NPS) is planning for a Fire Facility at Sunset Crater Volcano National Monument. -
Viability Analyses for Vascular Plant Species Within Prescott National Forest, Arizona
Viability analyses for vascular plant species within Prescott National Forest, Arizona Marc Baker Draft 4 January 2011 1 Part 1. Description of Ecological Context (Adapted from: Ecological Sustainability Report, Prescott National Forest, Prescott, Arizona, April 2009) Description of the Planning Unit Prescott National Forest (PNF) includes mostly mountains and associated grassy valleys of central Arizona that lie between the forested plateaus to the north and the arid desert region to the south. Elevations range between 3,000 feet above sea level along the lower Verde Valley to 7,979 feet at the top of Mount Union, the highest natural feature on the Forest. Roughly half of the PNF occurs west of the city of Prescott, Arizona, in the Juniper, Santa Maria, Sierra Prieta, and Bradshaw Mountains. The other half of the PNF lies east of Prescott and takes in the terrain of Mingus Mountain, the Black Hills, and Black Mesa. The rugged topography of the PNF provides important watersheds for both the Verde and Colorado Rivers. Within these watersheds are many important continuously or seasonally flowing stream courses and drainages. A portion of the Verde River has been designated as part of the National Wild and Scenic Rivers System. Vegetation within PNF is complex and diverse: Sonoran Desert, dominated by saguaro cacti and paloverde trees, occurs to the south of Bradshaw Mountains; and cool mountain forests with conifer and aspen trees occur within as few as 10 miles upslope from the desert . In between, there are a variety of plant and animal habitats including grasslands, hot steppe shrub, chaparral, pinyon-juniper woodlands, and ponderosa pine forests. -
GYMOAZ07-19 Mount Baldy
Mount Baldy Wilderness: East Fork Trail from Gabaldon Campground I drove to the Gabaldon Campground, just south of the East Fork Trail of the Mount BaldyWilderness #95, to meet up with a Monday hiking group comprised of 11 hikers led by TRACKS member and trail guide George Tichenor. There is a connector trail from the campground and it is very convenient for horseback riders — each campsite has a corral. We weren’t riding horses but it was a great place to start after a 30+ minute drive from Pinetop because of the large parking area but most important -- its outhouse. We followed the connector trail through a meadow and then crossed the Little Colorado River just before connecting to the East Fork Trail. The Trail travels through meadows and tunnels and climbs through a forest of Colorado blue spruce, white fir, Douglas fir, Ponderosa pine, white pine and ancient aspen — Pines so tall and so wide, we couldn’t connect hands while trying to wrap our arms around the trunks. We hiked past giant boulders and spires that towered over the trail and continued hiking until we reached the rock cliffs. It was here that we stopped and feasted on watermelon that was trekked in by Ron Miller, avid hiker, climber of highest peaks and retiree from the BIA, then turned around and headed back. The hike back descends a gravel trail -- where I gracefully slid and fell (saving my camera) -- and Miller, who was hiking ahead of me, turned around and said “Oh, let me help you” as he tripped over an exposed root crossing the trail, nearly falling himself and then appropriately named it “the root of all evil.” I have to say that there is a sense of camaraderie on this trail (or any trail). -
Recent Debris Flows and Floods in Southern Arizona
nrizonaVal. 36. No. 3 Geology FALL 2006 Published by the Arizona geological Survey 1 THE STATE AGENCY FOR GEOLOGIC INFORMATION Recent Debris Flows and Floods in Southern Arizona Phiip A. Pearthree and Ann Youberg Widespread damage Southeastern Arizona experienced an extremely wet interval near the end of July 2006 that generated floods and numerous debris flows (sediment-rich slurries) in some of the mountain ranges of this region. Flooding damaged homes and other property, roads, and infi-astructure along Aravaipa Creek and several watercourses in the Tucson area. The most impressive geologic phenomenon, however, consisted of intense debris flow activity in the Santa Catalina Mountains near Tucson, in the northern Chiricahua Mountains near Ft. Bowie and in the Huachuca Mountains near the border with Mexico. Hundreds of debris flows occurred on steep mountain slopes and larger debris flows coursed down several canyons (Figure 1).~c&ss to Sabino Canyon in the Santa ~ataling~oun&ns and Coronado National Memorial in the southern Huachuca Mountains was temporarily closed due to debris flows and flood damage, and ~t.~ekon Highway was damaged in several places. Debris flows have previously been recognized as a signtficant hazard in mountain areas in Arizona (Wohl and I Pearthree, 1991; Melis et al., 1997; Pearthree, 2004). Nonetheless, the number and size of debris flows that occurred at the end of July was surprising, and they remind us that rare meteorological / hydrological / geological events present si@cant hazards and are very important in shaping the landscape in Arizona. Meteorology and precipitation More than one-half of the annual precipitation in south- Figure 1. -
The Geology of the Canada Del Oro Headwaters, Santa Catalina Mountains, Arizona
The geology of the Canada del Oro headwaters, Santa Catalina Mountains, Arizona Item Type Thesis-Reproduction (electronic); text Authors Suemnicht, Gene Arthur,1948- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 01/10/2021 20:01:10 Link to Item http://hdl.handle.net/10150/191658 THE GEOLOGY OF THE CANADA DEL ORO HEADWATERS, SANTA CATALINA MOUNTAINS, ARIZONA by Gene Arthur Suemnicht A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 1977 STATEMENT BY AUTHOR This thesis has been submitted in partial fulfillment of re- quirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this thesis are allowable without special permission, provided that accurate acknowledgment of source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the head of the major department or the Dean of the Graduate College when in his judg- ment the proposed use of the material is in the interests of scholar- ship. In all other instances, however, permission must be obtained from the author.