Geology of the Morningstar Mine Area, Greaterville Mining District, Pima County, Arizona

Total Page:16

File Type:pdf, Size:1020Kb

Geology of the Morningstar Mine Area, Greaterville Mining District, Pima County, Arizona Geology of the Morningstar mine area, Greaterville mining district, Pima County, Arizona Item Type text; Thesis-Reproduction (electronic) Authors Stewart, James Conrad, 1935- 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 27/09/2021 15:41:40 Link to Item http://hdl.handle.net/10150/566530 GEOLOGY OF THE MORNINGSTAR MINE AREA, GREATERVILLE MINING DISTRICT, PIMA COUNTY, ARIZONA by James Conrad Stewart A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE WITH A MAJOR IN GEOLOGY In the Graduate College THE UNIVERSITY OF ARIZONA 1 9 7 1 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. SIGNED: APPROVAL BY THESIS DIRECTOR This thesis has been approved on the date shown below: 2 0 (<jlf of Geology ACKNOWLEDGMENTS For their contributions which so greatly aided the undertaking, presentation, and completion of this study, I express my appreciation to Dr. John M. Guilbert, my major professor, and to Dr. William C. Peters, for their guidance and encouragement; to Mr. Eric Braun and Dr. William Rehrig, fellow students, for their assistance as survey rodmen; to Mr. G. A. Barber of The Anaconda Company for use of Ana­ conda's assay data from the Morning star mine; to Mr. Michael Gross, fellow student, for the benefit of our "geologizing" and discussions of the area; and to M iss Judy Margolis for her drafting work. To Mr. and Mrs. Fred Harm, lessees of the Morning star mine, go extra special thanks for the generous and enthusiastic donation of their time, efforts, and accommodations. Use of the living quarters at the mine and the splendid board prepared by M rs. Harm greatly facili­ tated the field work and made for a most pleasant and comfortable summer. Mr. Harm's familiarity with the area, acquired from long association and persistently diligent work, was an invaluable aid. Additionally, the actual physical assistance given by Mr. Harm made possible the study of underground workings otherwise inaccessible. For their steadfast encouragement and financial support, with­ out which this program would not have been possible, I am especially grateful to my parents, Mr. and Mrs. James A. Stewart. iii TABLE OF CONTENTS Page LIST OF ILLUSTRATIONS...................................................................................... v i ABSTRACT......................................................... v iii INTR O D U C TIO N ............................................................................ ..... 1 GEOLOGY................................................................................................ 8 R o c k s ............................................................ 8 Sedim entary R o c k s ............................................................................ 9 • Igneous Rocks ...................................................................................... 17 Metamorphic Rocks............................................................................ 19 . C o r r e la t io n ........................................ 20 A g e ........................................................................................................... 21 S tru ctu res....................................................... 23 Major Structures of the Sedimentary Rocks.......................... 23 Minor Structures of the Sedimentary Rocks.......................... 26 Structures in th e Igneous R o c k s .............................................. 35 MINERAL D E P O S I T S ......................... 36 The Morningstar M in e ....................................................... 36 M in e r a lo g y ............................................................................................ 40 V e i n s ...................................................................................................... 45 R o c k s ................................................................................................. 47 S tru ctu res........................................................................................... 51 Other Mineral D eposits ............................................................................ 54 V e in s........................................................................................................... 54 P la c e r s ...................................................................................................... 61 SUMMARY, INTERPRETATION, AND EVALUATION............................... 65 Order of E v e n t s .......................................................................... 66 R egional Folding of th e Sedim entary R o ck s.......................... 66 Regional Thrust F au ltin g ......................... 67 Quartz M onzonite I n t r u s io n ........................................................ 68 U p lift of G ranite M o u n t a i n ........................................................ 68 Local Minor Faulting ............................................................ 69 C la s sific a tio n o f M ineral D e p o s i t s ......................... 70 Economic Evaluation of Mineral Deposits .................................... 71 The M orningstar M i n e .................................................................. 71 Other M ineral D e p o s i t s ........................................ 72 iv V TABLE OF CONTENTS— Continued Page APPENDIX: ASSAY DATA, MORNINGSTAR M IN E .................... ..... 74 REFERENCES 77 LIST OF ILLUSTRATIONS Figure Page 1. Location Map ............................................................................................ ..... 2 2. Geologic Interpretation Map Morningstar Mine Area . in pocket' 3 . Geologic Outcrop Map Morningstar Mine Area .... in p ock et 4. Stratigraphic Column Morningstar Mine Area .... in p ock et — 5 . C ross S ectio n s M orningstar M ine A r e a ..............................in p ock et 6 . S h a l e ................................................................................................................ 10 7. Silts tone . ..................................................................................................... 12 8 . A rgillite . ............................................................................................ 12 9 . Rock C la s s ific a tio n D ia g r a m .....................•........................................ 14 10. Q u a rtzite........................................................................................................... 15 11. Arkose R id g e s................................................................................................. 15 12. Quartz M o n z o n ite ....................................................................................... 18 13. Folds near the Morningstar Mine ................................................... 27 14. Folds North of the Morningstar M ine .............................. 27 15. Folded L im e s t o n e ....................................................................................... 29 16. Bedding Plane Fault ......................... 33 17. Morningstar Mine ....................................................................................... 38 18. Block Diagram of the Morningstar Mine .............................. in p o ck et 19. Composite Level Plan Map of the Morningstar Mine . in pocket 20. Cross Section of the Morningstar Mine Shaft .... in p o ck et 21. Gold-bearing Quartz Vein in Argillite ......................... 44 22. Quartz Vein Cutting A rgillite ............................................................. 56 vi vii LIST OF ILLUSTRATIONS— C ontinued Figure Page 23 . A L enticular Quartz V e i n ........................................................................ 56 2 4 . Quartz Vein in Quartz M o n z o n i t e ..................................................... 59 • 25. Stream Bench G ravels ............................................................................ 62 26. Gold Nuggets ................................................................................ 64 ABSTRACT The Morningstar mine area is located in the Greaterville mining district, Pima County, Arizona. The area constitutes a north-trending, east-dipping, 2,000-foot thick sequence of arkose, quartzite, and shale regionally folded into anticlines and synclines plunging to the southeast. Later thrusting placed younger rocks in the southeast over older rocks to the northwest. Probably Cretaceous in age, the sedimentary rocks are cut by the small Tertiary quartz monzonite Granite Mountain stock. The stock produced local hornfelsic alteration
Recommended publications
  • Maricopa County Regional Trail System Plan
    Maricopa County Regional Trail System Plan Adopted August 16, 2004 Maricopa Trail Maricopa County Trail Commission Maricopa County Department of Transportation Maricopa County Parks and Recreation Maricopa County Planning and Development Flood Control District of Maricopa County We have an obligation to protect open spaces for future generations. Maricopa County Regional Trail System Plan VISION Our vision is to connect the majestic open spaces of the Maricopa County Regional Parks with a nonmotorized trail system. The Maricopa Trail Maricopa County Regional Trail System Plan - page 1 Credits Maricopa County Board of Supervisors Andrew Kunasek, District 3, Chairman Fulton Brock, District 1 Don Stapley, District 2 Max Wilson, District 4 Mary Rose Wilcox, District 5 Maricopa County Trail Commission Supervisor Max Wilson, District 4 Chairman Supervisor Andrew Kunasek, District 3 Parks Commission Members: Citizen Members: Laurel Arndt, Chair Art Wirtz, District 2 Randy Virden, Vice-Chair Jim Burke, District 3 Felipe Zubia, District 5 Stakeholders: Carol Erwin, Bureau of Reclamation (BOR) Fred Pfeifer, Arizona Public Service (APS) James Duncan, Salt River Project (SRP) Teri Raml, Bureau of Land Management (BLM) Ex-officio Members: William Scalzo, Chief Community Services Officer Pictured from left to right Laurel Arndt, Supervisor Andy Kunasek, Fred Pfeifer, Carol Erwin, Arizona’s Official State Historian, Marshall Trimble, and Art Wirtz pose with the commemorative branded trail marker Mike Ellegood, Director, Public Works at the Maricopa Trail
    [Show full text]
  • Coconino National Forest Land and Resource Management Plan Document the Analysis and Decisions Resulting from the Planning Process
    ' " United States (. Il). Department of \~~!J'~~':P Agriculture CoconinoNational Forest Service ForestPlan Southwestern Region -""""" IU!S. IIIII.IIIIII... I I i I--- I I II I /"r, Vicinity Map @ , " .. .' , ",', '. ',,' , ". ,.' , ' ' .. .' ':':: ~'::.»>::~: '::. Published August 1987 Coconino N.ational Forest Land and Resource Management Plan This Page Intentionally Left Blank Coconino Foresst Plan TABLE OF CONTENTS 1. INTRODUCTION Purpose of the Plan. 1 Organization of the Forest Plan Documentation. 2 Planning Area Description. 2 2. ISSUES Overview . 5 Issues . 5 Firewood . 6 Timber Harvest Levels. 7 The Availability of Recreation Options . 8 Off-Road Driving . 9 Wildlife Habitat . 9 Riparian Habitat . 11 Geothermal Development . .. 11 Management of the Transportation System . 12 Use of the Public Lands . 13 Law Enforcement . 13 Landownership Adjustment . 14 Opportunities . 14 Public Affairs . 14 Volunteers . 15 3. SUMMARY OF THE ANALYSIS OF THE MANAGEMENT SITUATION Overview . 17 Prior Allocations . 18 4. MANAGEMENT DIRECTION Overview . 21 Mission . 21 Goals . 21 Objectives . 26 Regional Guide/Forest Plan . 26 Outputs & Range of Implementation . 26 Management Prescriptions . 46 Management Area Description . 46 Management Emphasis . 46 Program Components . 46 Activities . .. 47 Standards and Guidelines . 47 How to Apply Prescriptions . .. 47 Coordinating Requirements . .. 47 Coconino National Forest Plan – Partial Cancellation of Amendment No. 15 -3/05 Replacement Page i Coconino Forest Plan Table of Contents continued Standards and Guidelines . 51 Forest-wide . 51 MA 1 Wildernesses . 98 MA 2 Verde Wild and Scenic River . .. 113 MA 3 Ponderosa Pine and Mixed Conifer, Less Than 40 Percent Slopes. .. 116 MA 4 Ponderosa Pine and Mixed Conifer, Greater Than 40 Percent Slopes. 138 MA 5 Aspen . 141 MA 6 Unproductive Timber Land .
    [Show full text]
  • Kaibab National Forest
    United States Department of Agriculture Kaibab National Forest Forest Service Southwestern Potential Wilderness Area Region September 2013 Evaluation Report The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or part of an individual’s income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means of communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at (202) 720-2600 (voice and TTY). To file a complaint of discrimination, write to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, SW, Washington, DC 20250-9410, or call (800) 795-3272 (voice) or (202) 720-6382 (TTY). USDA is an equal opportunity provider and employer. Cover photo: Kanab Creek Wilderness Kaibab National Forest Potential Wilderness Area Evaluation Report Table of Contents Introduction ................................................................................................................................................. 1 Inventory of Potential Wilderness Areas .................................................................................................. 2 Evaluation of Potential Wilderness Areas ...............................................................................................
    [Show full text]
  • Structural Evolution of the Mcdowell Mountains Maricopa County
    Structural Evolution of the McDowell Mountains Maricopa County, Arizona by Brad Vance A Thesis Presented in Partial Fulfillment of the Requirements for the Degree Master of Science Approved November 2012 by the Graduate Supervisory Committee: Stephen Reynolds, Chair Steven Semken Edmund Stump ARIZONA STATE UNIVERSITY December 2012 ABSTRACT The accretion of juvenile island-arc lithosphere by convergent tectonism during the Paleoproterozoic, in conjunction with felsic volcanism, resulted in the assembly, ductile to partial brittle deformation, uplift, and northwest-directed thrusting of rocks in the McDowell Mountains region and adjacent areas in the Mazatzal Orogenic belt. Utilizing lithologic characteristics and petrographic analysis of the Proterozoic bedrock, a correlation to the Alder series was established, revising the stratigraphic sequences described by earlier works. The central fold belt, composed of an open, asymmetric syncline and an overturned, isoclinal anticline, is cut by an axial-plane parallel reactivated thrust zone that is intruded by a deformed Paleoproterozoic mafic dike. Finite strain analyses of fold geometries, shear fabrics, foliations, fold vergence, and strained clasts point to Paleoproterozoic northwest-directed thrusting associated with the Mazatzal orogen at approximately 1650 million years ago. Previous studies constrained the regional P-T conditions to at least the upper andalusite-kyanite boundary at peak metamorphic conditions, which ranged from 4-6 kilobars and 350-450⁰ Celsius, although the plasticity of deformation in a large anticlinal core suggests that this represents the low end of the P-T conditions. Subsequent to deformation, the rocks were intruded by several granitoid plutons, likely of Mesoproterozoic age (1300-1400 Ma). A detailed analysis of Proterozoic strain solidly places the structure of the McDowell Mountains within the confines of the Mazatzal Orogeny, pending any contradictory geochronological data.
    [Show full text]
  • Environmental Change in Aravaipa, 1870 - 1970 an Ethnoecological Survey
    BUREAU OF LAND MANAGEMENT ARIZONA - Environmental Change in Aravaipa, 1870 - 1970 An Ethnoecological Survey Diana Hadley Peter Warshall Don Bufkin CULTURAL RESOURCE SERIES No. 7 1991 Environmental Change in Aravaipa, 1870 - 1970 An Ethnoecological Survey Prepared by Hadley Associates Diana Hadley, Historian Peter Warshall, Ph.D., Ecologist Don Bufkin, Cartographer Cultural Resource Series Monograph No. 7 Published by the Arizona State Office of the Bureau of Land Management 3707 N. 7th Street Phoenix, Arizona 85014 September 1991 EDITOR'S FORWARD The preface to this document expresses the hope that this ethnoecological survey of Aravaipa " . will provide local managers with a greater time- depth and feeling for the ways in which humans and natural events have intertwined to shape Aravaipa's present condition and the appearance of Aravaipa's resources. Wise future management cannot be divorced from the cumulative impacts and decisions of the past. Future management can benefit from the knowledge, the admitted mistakes, and beneficial decisions made by former residents." I cannot think of a clearer statement of the manner in which cultural resource information can be made relevant to our lives today. Archaeologists and historians are often asked to justify the usefulness of their efforts in relation to the realities of modern-day living. In response, we say that the lessons of the past can teach us how to live better in the present. By building on the successes of those who came before us, and avoiding mistakes that they have made, we can do a better job of managing our resources now and can plan more effectively for the future.
    [Show full text]
  • White Tank Mountain Regional Park
    White Tank Mountain Regional Park Master Plan Update 2014-2034 {This page intentionally left blank.} {This page intentionally left blank.} {This page intentionally left blank.} Acknowledgements This master plan update was a collaborative process that involved the guidance and expertise of many. The Maricopa County Parks and Recreation Department would like to thank the Planning Team who committed their time to monthly meetings and document review; likewise to the Stakeholder Advisory Group who took time out of their personal lives to provide their invaluable input. Planning Team Stakeholder Advisory Group R.J. Cardin, Director Jamil Coury Jennifer Waller, Operations Manager Linda Gilgosch Jennifer Johnston, West Side Superintendent John Pesock Raymond Schell, Park Supervisor Frank Salowitz Michele Kogl, Planning and Development Manager Allen Ockenfels, Trails Development Manager Fareed Abou-Haidar, GIS Technician Leigh Johnson, Park Planner This Master Plan update was also made possible by the contributions and guidance of the following: • Maricopa County Board of Supervisors o Denny Barney, District 1 o Steve Chucri, District 2 o Andy Kunasek, District 3 o Clint L. Hickman, District 4 o Mary Rose Wilcox, District 5 • Maricopa County Parks and Recreation Commission o Jack Stapley, District 2 o Anne Lynch, District 3 o Dr. Robert Branch, District 4 o Carlton Yoshioka , Member-at-Large o Rod Jarvis, Member-at-Large • Maricopa County Parks and Recreation Department staff • Maricopa County Sheriff’s Office, Mountain Patrol Division • Bill “Doc” Talboys, Interpretive Ranger, MCPRD (retired) • Shelly Rasmussen, Interpretive Ranger, MCPRD (retired) • Public meeting participants The Department would also like to thank its agency partners at the City of Surprise, City of Buckeye, Arizona Game and Fish Department, and the Bureau of Land Management - Phoenix District Office for their input and guidance.
    [Show full text]
  • Bedrock Geology of the Santan Mountains, Pinal and Maricopa
    BEDROCK GEOLOGY OF THE SANTAN MOUNTAINS,PINAL AND MARICOPA COUNTIES, ARIZONA by Charles A. Ferguson, and Steven J. Skotnicki Arizona Geological Survey Open-File Report 96-9 June 1996 Arizona Geological Survey 416 W. Congress, Suite #100, Tucson, Arizona 85701 Includes 1:24,000 scale geologic map, cross-sections (2 sheets), and 22 page text Jointly funded by the Arizona Geological Survey and the u.S. Geological Survey STATEMAP Program Contract#1434-95-A-1353 This report is preliminary and has not been edited or reviewed for conformity with Arizona Geological Survey standardS 2 INTRODUCTION The Santan Mountains are a 25 Ian long, west-northwest trending uplift composed chiefly of Proterozoic and Cretaceous crystalline rocks overlain in the central and eastern part of the range by Mid-Tertiary sedimentary and volcanic rocks. Santan Mountain at an elevation of 3010 feet is the range's highest point, rising nearly 1700 feet above the basin floor. Elevations decrease rapidly to the southeast towards the Gila River. The eastern two thirds of the range are composed of low hills connected by extensive areas of pedimented bedrock where relief is rarely greater than 400 feet. The range is bounded to the north by the Higley basin, and no extensive, pedimented bedrock surfaces exist here. Instead, abrupt thickening of the basin fill is suggested by the numerous earth fissures along the range's north edge (Harris, 1994; Sank, 1975). To the south, like the east, an extensive dissected granitic pediment extends all the way to the Gila river. Extensive pediments in the Sacaton Mountains to the southwest also probably extend northward to the Gila River, suggesting that the low area between the two ranges was created more by erosional processes than by tectonic processes.
    [Show full text]
  • Hike Database
    Hike Database October 1, 2011 TABLE OF CONTENTS Section Subject Page 1 General Information 3 2 Hike Ratings, Pace, and Elevation Change 5 3 Special Conditions 7 4 Glossary 8 5 Hike Descriptions 9 Agua Caliente Hill / La Milagrosa Ridge / Molino Basin… 10 Babad Do‟ag Trail 26 Cactus Forest Area 31 David Yetman Trail 35 El Capitan Canyon (lower) 37 Fifty-Year Trail Area Loop 38 Gardner Canyon to Kentucky Camp 40 Hamburg Trail 43 Incinerator Ridge 45 Josephine Peak 45 Kentucky Camp Hike and Hot Dog Cookout 46 La Milagrosa Ridge / AZT from Redington Rd. 47 Madera Canyon Kent Springs - Bog Springs Loop 48 Newman Peak 55 Oracle Ridge / Red Ridge Loop 55 Palisade Trail / Mud Spring 56 Quantrell Mine 62 Ragged Top / Silverbell Mountains 62 Sabino Canyon - Bear Canyon Loop (no Trams) 64 Table Mountain 75 Ventana Canyon – Lower Level 79 Wasson Peak at Sunset and Moonrise 80 6 Hikes by Area and Number 83 Hikes by Area 83 Hikes Sorted by Number 88 7 Driving Directions 93 8 References 97 October 1, 2011 Page 2 GENERAL INFORMATION All hikes leave from the first, left (when entering from MountainView Blvd.) parking lot in front of the MountainView Clubhouse (just east of the tennis courts), unless otherwise noted. Voluntary driver donations will be shown in the “Hikes Offered” table in the Club Newsletter. These costs will change from time to time with significant fluctuations in gasoline prices. There may be other fees for tram shuttles, entry to areas such as national parks, monuments, wilderness areas, special tours and exhibits, permits, state parks, overnight stays, etc.
    [Show full text]
  • Arizona Geological Survey | 2Mcdowell Sonoran Field Institute
    QUARTZ VEIN INVESTIGATION, MCDOWELL SONORAN PRESERVE, SCOTTSDALE, MARICOPA COUNTY, ARIZONA Brian F. Gootee1 & Daniel G. Gruber2 1Arizona Geological Survey | 2McDowell Sonoran Field Institute State geological survey employees collecting geothermal data. OPEN-FILE REPORT OFR-15-03 July 2015 Arizona Geological Survey www.azgs.az.gov | repository.azgs.az.gov Arizona Geological Survey M. Lee Allison, State Geologist and Director Manuscript approved for publication in July 2015 Printed by the Arizona Geological Survey All rights reserved For an electronic copy of this publication: www.repository.azgs.az.gov Printed copies are on sale at the Arizona Experience Store 416 W. Congress, Tucson, AZ 85701 (520.770.3500) For information on the mission, objectives or geologic products of the Arizona Geological Survey visit www.azgs.az.gov. This publication was prepared by an agency of the State of Arizona. The State of Arizona, or any agency thereof, or any of their employees, makes no warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed in this report. Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the State of Arizona. ___________________________ Recommended Citation: Gootee, B.F. and Gruber, D.G., 2015, Quartz vein investigation, McDowell Sonoran Preserve, Scottsdale, Maricopa County, Arizona. Arizona Geological Survey Open File Report,
    [Show full text]
  • WEB 01-20 GYMOAZ-01-20The Monument Man V3-Annemarie
    The Monument Man – “Wood” Treasure Hunting in the Salt River Mountains by Annemarie Eveland I like hiking and I am enchanted with the Superstition Mountains and our Four Peaks area. So, when I heard about someone who had spent twenty-some years investigating historical Spanish monuments in these areas, I went to investigate. This is part of the interview with “Wood”, the monument man. AE: Tell me about yourself. Why do they call you” Wood,” the monument man? W: I am nicknamed WOOD because it is part of my middle name. I have had an intense fascination with -- and have done extensive, long-time research on the monuments of the Southwest. These monuments were created first by Indians, then secondly by Spaniards and Jesuits marking their trails. In 1978, I started seriously hiking in the wilderness of the Superstition Mountains and the Four Peaks areas. I was 22 years old then. I backpacked -- sometimes a week at a time -- exploring and photographing the surrounding nature that I came upon. Along the trails in these different areas, I noticed rocks that resembled Indian heads -- and a myriad of different animals -- such as turtles, snakes, dogs and such. Upon closer inspection, I began to realize that these had been created by unknown hands. They were chiseled and fashioned by persons unknown to me at that time. With many of the ones that I inspected, I noticed they had a common theme. It showed the general direction to take -- or the eyes on the animals were pointing in certain directions. After years of taking pictures and studying these monuments, I came to the realization that many of them were very old and Jesuit and Spanish in nature, leading to different locations in the mountains.
    [Show full text]
  • Vegetation and Flora of the Mcdowell Sonoran Preserve, Maricopa County, Arizona
    VEGETATION AND FLORA OF THE MCDOWELL SONORAN PRESERVE, MARICOPA COUNTY, ARIZONA Steve Jones and Chelsey Hull McDowell Sonoran Conservancy 16345 N. Scottsdale Rd. Suite 110 Scottsdale, AZ 85254 ABSTRACT This study is part of an effort to establish a baseline assessment of the biotic condition of the City of Scottsdale’s McDowell Sonoran Preserve. The study area is in northeastern Scottsdale and includes the McDowell Mountain range and areas to the north of the range. In total, 379 taxa in 61 families were identified between February 2011 and September 2013. The McDowell Sonoran Conservancy's Field Institute trained volunteer citizen scientists to participate in collecting specimens for the study. Seedbank samples were collected and cultivated in a greenhouse to simulate a wet spring season. Plant families with the largest presence in the preserve include Asteraceae (65 taxa), Poaceae (49), Fabaceae (19), Boraginaceae (22), and Cactaceae (17). Major biotic communities were identified and described. INTRODUCTION In 1995 and 2004, the citizens of the City of Scottsdale approved taxation mechanisms for funding the purchase of the McDowell Mountains and surrounding lands. As the land was assembled, the City designated it the McDowell Sonoran Preserve (MSP). Assemblage of the preserve is ongoing. This study is part of a larger baseline assessment of the biotic condition of the MSP, and of land under consideration for addition to the MSP. Assessments of arthropods, reptiles, birds and mammals were undertaken at roughly the same time. The studies were organized under the auspices of the McDowell Sonoran Field Institute (MSFI), the research center of the McDowell Sonoran Conservancy (MSC).
    [Show full text]
  • Sbhc Hike Database 06-01-10
    Hike Database June 1, 2010 TABLE OF CONTENTS Section Subject Page 1 General Information 3 2 Hike Ratings, Pace, and Elevation Change 4 3 Special Conditions 5 4 Glossary 6 5 Hike Descriptions 7 Agua Caliente Hill / La Milagrosa Ridge / Molino Basin 8 Babad Do‟ag Trail 15 Cactus Forest Area 20 David Yetman Trail 24 El Capitan Canyon (lower) 25 Fifty-Year Trail - North End 26 Gardner Canyon to Kentucky Camp 28 Hamburg Trail 31 Incinerator Ridge 32 Josephine Peak 33 King Canyon Loop 33 La Milagrosa Ridge/AZT from Redington Rd. 34 Madera Canyon Kent Springs - Bog Springs Loop 35 Nugget Canyon (short version) 40 Oracle Ridge / Red Ridge Loop 41 Palisade Trail / Mud Spring 42 Quantrell Mine 47 Ragged Top / Silverbell Mountains 48 Sabino Canyon - Bear Canyon Loop (no Trams) 50 Table Mountain 60 Ventana Canyon - Lower Level 64 Wasson Peak at Sunset and Moonrise 64 6 Hikes by Area and Number 67 Hikes by Area 67 Hikes Sorted by Number 71 7 Driving Directions 76 8 References 80 June 1, 2010 Page 2 GENERAL INFORMATION All hikes leave from the first, left (when entering from MountainView Blvd.) parking lot in front of the MountainView Clubhouse (just east of the tennis courts), unless otherwise noted. Voluntary driver donations will be shown in the “Hikes Offered” table in the Club Newsletter. These costs will change from time to time with significant fluctuations in gasoline prices. There may be other fees for tram shuttles, entry to areas such as national parks, monuments, wilderness areas, special tours and exhibits, permits, state parks, overnight stays, etc.
    [Show full text]