Cultural Heritage the Mountains and Foothills of North Carolina Have Over Many Centuries Fostered a Rich Mosaic of Cultural Heritage
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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. -
Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region. -
Regional and County Population Change in North Carolina
Regional and County Population Change in North Carolina A Summary of Trends from April 1, 2010 through July 1, 2016 North Carolina Office of State Budget and Management December 2017 Introduction The following document summarizes population trends for North Carolina using the certified county population estimates produced by the North Carolina Office of State Budget and Management (OSBM) released in September of 2017. These certified population estimates are as of July 1, 2016.1 Additional population tables that include statistics for all 100 counties can be obtained from https://www.osbm.nc.gov/demog/county‐estimates.2 Highlights: North Carolina grew by 620,254 people between April 1, 2010 and July 1, 2016, a 6.5% increase; Three of every four people added in this period were living in central North Carolina3; 95% of all growth occurred within metropolitan counties4; Among regional planning areas, only the Upper Coastal Plain Council of Governments experienced population decline; The fastest growing metropolitan statistical areas (MSAs) since April 1, 2010 were the North Carolina portion of the Myrtle Beach‐Conway‐North Myrtle Beach MSA, the Raleigh MSA, the North Carolina portion of the Charlotte‐Concord‐Gastonia MSA, and the Wilmington MSA. Only the Rocky Mount MSA experienced population decline since the last census, losing 4,460 people (a 2.9% decline); The Charlotte‐Concord‐Gastonia MSA remains the largest metropolitan area in the state (at 2.1 million people); Mecklenburg (1.1 million) and Wake (1.0 million) Counties remain -
Geologic Framework of the Catalina Foothills, Outskirts of Tucson (Pima County, Arizona)
GEOLOGIC FRAMEWORK OF THE CATALINA FOOTHILLS, OUTSKIRTS OF TUCSON (PIMA COUNTY, ARIZONA) W.R. DICKINSON Emeritus, Dept. of Geosciences University of Arizona ARIZONA GEOLOGICAL SURVEY CONTRIBUTED MAP CM-99-B MAY 1999 31 p., scale 1 :24,000 TIus report is preliminary and has not been edited or reviewed for confonnity with Arizona Geological Survey standards. ARIZONA GEOLOGICAL SURVEY CONTRIBUTED MAP CM-99-B (31 pp., 1 Plate) Geologic Framework of the Catalina Foothills, Outskirts of Tucson (Pima County, Arizona) [Text and Legend to Accompany 1:24,000 Map] William R. Dickinson, Department of Geosciences, University of Arizona May 1999 Introduction and Purpose Past geologic maps and accounts of the sedimentary, geomorphic, and structural geology of the piedmont of the Santa Catalina Mountains in the outskirts of Tucson by Voelger (1953), Pashley (1966), Davidson (1973), Creasey and Theodore (1975), Banks (1976), Anderson (1987), Pearthree et al. (1988), McKittrick (1988), and Jackson (1989) raised questions about the sedimentary evolution of the foothills belt that were left open or unresolved. Multiple dissected alluvial fans and pediments overlie much older faulted and tilted strata to form Cenozoic sedimentary assemblages of considerable stratigraphic and structural complexity. As a contribution to improved understanding of urban geology in the Tucson metropolitan area, systematic geologic mapping of the piedmont belt was undertaken to establish the overall geologic framework of the Catalina foothills (~ 175 2 km ) at a common scale (1 :24,000). The area studied extends from Oracle Road on the west to the vicinity of Rinconado Road on the east, and from the Rillito River and Tanque Verde Wash northward to the limit of bedrock exposures at the base of the Santa Catalina Mountains. -
Employment Assistance and Job Training Housing And/Or
JOBSTART COUNTY RESOURCE LIST HAYWOOD COUNTY Resources to Support Your Employment and Life Plans NORTH CAROLINA CARE-LINE 1-800-662-7030 This is a number that you can call to find out about community resources all over North Carolina. Employment Assistance and Job Training Mountain Projects This program helps people with Comments/Appointments Phone: 704-452-1447 low incomes that want to get a job. Haywood County JobLink Center/ Employment Security Commission 1170 N. Main Street Waynesville, NC 28786 Phone: 828-456-6061 Vocational Rehabilitation Office Sylva Unit Office 485-D East Main Street Sylva, NC 28779 Phone: 828-586-4032 Haywood Community College 185 Freedlander Drive Clyde, NC 28721 Phone: 828-627-2821 Housing and/or Emergency Shelter REACH of Haywood County This service helps people who PO Box 206 have been victims of sexual Waynesville, NC 28786 assault or domestic violence. Phone: 704-456-7898 CROSSROADS Offers emergency shelter and food PO Box 126 assistance Waynesville, NC 28786 Community Action Offers emergency shelter and food Route 1, Box 732 assistance Waynesville, NC 28786 Phone: 704-452-1447 Salvation Army Offers emergency shelter and food PO Box 358 assistance Waynesville, NC 28786 Phone: 704-456-7111 or 704-452-9054 Transportation, Food and Clothing Note: For Driver License Information, See Important Documents Section. REACH of Haywood County This service helps people who PO Box 206 have been victims of sexual Waynesville, NC 28786 assault or domestic violence. Phone: 704-456-7898 www.haywoodnc.org/government/haywoodcountygovt.html Page 1 JOBSTART COUNTY RESOURCE LIST HAYWOOD COUNTY Resources to Support Your Employment and Life Plans NORTH CAROLINA CARE-LINE 1-800-662-7030 This is a number that you can call to find out about community resources all over North Carolina. -
Quartz Crystal Deposits of Southwestern Virginia and Western North Carolina
Quartz Crystal Deposits of Southwestern Virginia and Western North Carolina GEOLOGICAL SURVEY BULLETIN 1072-D Quartz Crystal Deposits of Southwestern Virginia and Western North Carolina By JOHN B. MERTIE, JR. CONTRIBUTIONS TO ECONOMIC GEOLOGY GEOLOGICAL SURVEY BULLETIN 1072-D A detailed report on quart* crystals from 37 sources and an explanation of their origins UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U. S. Geological Survey Library has cataloged this publication as follows: Mertie, John Beaver, 1888- Quartz crystal deposits of southwestern Virginia and western North Carolina. Washington, U. S. Govt. Print. Off., 1958. iv, 233-298 p. maps, tables. 25 cm. (U. S. Geological Survey. Bulletin 1072-D. Contributions to economic geology) "A detailed report on quartz crystals from 37 sources and an ex planation of their origins." Bibliography: p. 295-296. 1. Quartz. i. Title. (Series: U. S. Geological Survey. Bul letin 1072-D. Series: U. S. Geological Survey. Contributions to economic geology) 553.8 For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price 30 cents (paper cover) CONTENTS PagC Abstract.._._----.---._______-_______._--__. ...__. ________ 233 Introduction.___-_-__---___--__--_--__--_-------_-_-__---.-_---___ 234 Present investigation_____________________________________________ 235 Sites of deposits.____--_-_____-__--___-___-_____________-_-________ -
City Bio Asheville, North Carolina Is Located in Western North Carolina; It Is Located in Buncombe County
City Bio Asheville, North Carolina is located in Western North Carolina; it is located in Buncombe County. It is known as the largest city in Western North Carolina and is the 11th largest city in North Carolina overall. The city of Asheville is known for its art and architecture. Fun Fact The National Climate Data Center (NCDC) is located in Ashville and is known as the world’s largest active archive of weather data. You can take a tour of the NCDC, which is located at 151 Patton Avenue. Places to See Biltmore Estates: is the largest privately owned house in the United States, owned by the Vanderbilt family. From the complex, to the gardens, to the winery, to the shopping and outdoor activities there is plenty to see at the Estate and is said to take up a long portion of your day, so plan accordingly. Located at 1 Lodge Street. Basilica of Saint Lawrence: is a Roman Catholic Church, a minor basilica thanks to the upgraded status from Pope John Paul II, it is on the National Register of Historic Places. Located at 97 Haywood Street. North Carolina Arboretum: is a great place to walk, bike and educate, the location is full of gardens, national parks with great views and educational sites. There are activities for both younger and older children. Located at 100 Frederick Law Olmsted Way. Asheville Zipline Canopy Adventures: is a 124 acre zipline course that takes you into 150 year old trees that overlook historic downtown and the Blue Ridge Mountains. The experience takes around 2-3 hours long so plan accordingly. -
South Carolina Landform Regions (And Facts About Landforms) Earth Where Is South Carolina? North America United States of America SC
SCSouth Carolina Landform Regions (and facts about Landforms) Earth Where is South Carolina? North America United States of America SC Here we are! South Carolina borders the Atlantic Ocean. SC South Carolina Landform Regions Map Our state is divided into regions, starting at the mountains and going down to the coast. Can you name these? Blue Ridge Mountains Landform Regions SC The Blue Ridge Mountain Region is only 2% of the South Carolina land mass. Facts About the Blue Ridge Mountains . ◼ It is the smallest of the landform regions ◼ It includes the state’s highest point: Sassafras Mountain. ◼ The Blue Ridge Mountains are part of the Appalachian Mountain Range Facts About the Blue Ridge Mountains . ◼ The Blue Ridge Region is mountainous and has many hardwood forests, streams, and waterfalls. ◼ Many rivers flow out of the Blue Ridge. Blue Ridge Mountains, SC Greenville Spartanburg Union Greenwood Rock Hill Abbeville Piedmont Landform Regions SC If you could see the Piedmont Region from space and without the foliage, you would notice it is sort of a huge plateau. Facts About the Piedmont Region . ◼ The Piedmont is the largest region of South Carolina. ◼ The Piedmont is often called The Upstate. Facts About the Piedmont Region . ◼ It is the foothills of the mountains and includes rolling hills and many valleys. ◼ Piedmont means “foot of the mountains” ◼ Waterfalls and swift flowing rivers provided the water power for early mills and the textile industry. Facts About the Piedmont Region . ◼ The monadnocks are located in the Piedmont. ◼ Monadnocks – an isolated or single hill made of very hard rock. -
HELP Resource Guide Se Habla Espan
The Federal Government’s definition of homelessness under the McKinney-Vento Act refers to anyone who: Lacks regular, fixed, and adequate nighttime HELP Resource Guide residence. Is sharing housing due to economic struggles, The following is a list of resources designed to coordinate (doubled-up). services for homeless youth and families, in accordance with Is living in a shelter, hotel or motel. the McKinney-Vento Act. To address the provisions set forth in the act, Henderson County Public Schools has adopted Is sleeping in a place that is not designed for “HELP”, the Homeless Education Link Project, with two sleeping (cars, parks). working case managers available during the school year. The Is an unaccompanied youth. goal of this project is to help identify and address the needs of Is a child or youth abandoned in a hospital. homeless students and their families, to develop enrollment Is a child or youth awaiting foster care placement. procedures to ensure ongoing education success for homeless Is living in a substandard and/or inadequate students, and to serve as liaisons between schools, qualifying students, and services within the community. housing. Is a migrant child who qualifies under any of the above. HELP Case Managers serve as homeless liaisons for youth in each of the public schools in Henderson County. The HELP Case Managers of HCPS can provide For more information contact: support, resources and information regarding the Christine Craft ~~~~ 828-388-0294 rights of students to any in the area with school age children. [email protected] Troy Bradley ~~~~ 828-388-0266 Se Habla Espanol [email protected] 2 Table of Contents ADULT EDUCATION Adult Education . -
2012 Piedmont Triad Region Freight Movement Report
2012 Piedmont Triad Region Freight Movement Report September 12, 2012 Report Prepared by: C. David Hauser, Project Manager Transportation Institute NC A&T State University In Partnership with the: The Piedmont Authority for Regional Transportation, and In cooperation with The Burlington-Graham Metropolitan Planning Organization, The Greensboro Metropolitan Planning Organization, The High Point Metropolitan Planning Organization, and The Winston-Salem Metropolitan Planning Organization Table of Contents 1 Introduction 1.1 Purpose of chapter 1.2 Relevance to the Transportation System and the Plan 2 Existing Conditions and Trends 2.1 Entire Freight System: Statewide and Regional Conditions and Trend 2.2 Highway Freight: National Conditions and Trends 2.3 Highway Freight: Statewide and Regional Conditions and Trends 2.4 Highway Freight: Conditions and Trends in the Piedmont Triad Study Area 2.5 Rail Freight: National Conditions and Trends 2.6 Rail Freight: Statewide and Regional Conditions and Trends 2.7 Rail Freight: Condition and Trends in the Piedmont Triad Study Area 3 Current and Future Issues 3.1 Entire Freight System: Statewide and Regional Current and Future issues 3.2 Highway Freight: National Current and Future Issues 3.3 Highway Freight: Statewide and Regional Current and Future Issues 3.4 Rail Freight: National Current and Future Issues 3.5 Rail Freight: Statewide and Regional Current and Future Issues 3.6 Freight System: Current and Future Issues Within the Piedmont Triad Study Area 4 NC ports 5 Airports 5.1 Piedmont Triad International Airport 5.2 Smith Reynolds Airport 5.3 Additional Piedmont Triad Regional Airports 6 Safety and Security 7 Recommendations for Piedmont Triad Study Area 7.1 Truck Route Recommendations 7.2 Summary Recommendations 2012 Piedmont Triad Region Freight Movement Report 1 Introduction 1.1 Purpose of chapter Freight movement is critical to an advanced industrial economy, and the ease of freight movement is a component of a region’s economic competitiveness. -
Bennett College Brevard College Greensboro College High Point University Pfeiffer University Western North Carolina Conference
REQUIREMENTS 1. All applicants must apply in writing to 6. All applicants are to be interviewed the Chair of the Scholarship Committee. each year by the Scholarship Committee, or be interviewed by a 2. All applicants must be members of person selected by the Chair of the the United Methodist Church and reside Scholarship Committee, prior to granting within the bounds of the Western North scholarships. Interviews will be held in Carolina Conference. Scholarship the spring. recipients shall pursue an academic course in one of the five United 7. No applicant will be considered Methodist-supported colleges or until all requirements are met. A universities in the Western North small, non-returnable picture attached to Bennett College Carolina Conference. the application will be helpful to the Brevard College Scholarship Committee. All applications Greensboro College 3. All applicants must have references are due by March 1 each year. from the following people: The High Point University applicant’s pastor, a faculty member of Pfeiffer University the school last attended, a peer group Additional information and person, and a business or professional application forms may be obtained from: person who knows the applicant through some experience outside the church. Forms will be provided. Cathy McCauley WNCC UMW Scholarship Chairperson 4. All applicants recently graduated 6835 Farmingdale Dr. Apt. A must supply a transcript of this high Charlotte, NC 28212 school record. In the case of a second- Phone: 704-965-6566 cell career applicant who has not been in Email: [email protected] school recently, a transcript will not be required. 5. -
New Particle Formation Infrequently Observed in Himalayan Foothills – Why?
Atmos. Chem. Phys., 11, 8447–8458, 2011 www.atmos-chem-phys.net/11/8447/2011/ Atmospheric doi:10.5194/acp-11-8447-2011 Chemistry © Author(s) 2011. CC Attribution 3.0 License. and Physics New particle formation infrequently observed in Himalayan foothills – why? K. Neitola1, E. Asmi1, M. Komppula2, A.-P. Hyvarinen¨ 1, T. Raatikainen1,3, T. S. Panwar4, V. P. Sharma4, and H. Lihavainen1 1Finnish meteorological Institute, Helsinki, Finland 2Finnish meteorological Institute, Kuopio, Finland 3Georgia Institute of Technology, Atlanta, Georgia, USA 4Energy and Resource Institute, New Delhi, India Received: 10 December 2010 – Published in Atmos. Chem. Phys. Discuss.: 29 April 2011 Revised: 29 July 2011 – Accepted: 16 August 2011 – Published: 19 August 2011 Abstract. A fraction of the Himalayan aerosols originate 1 Introduction from secondary sources, which are currently poorly quan- tified. To clarify the climatic importance of regional sec- Secondary particle formation from gaseous precursors is ondary particle formation in the Himalayas, data from 2005 largely recognised as an important worldwide mechanism in- to 2010 of continuous aerosol measurements at a high- creasing the number of atmospheric particles (Kulmala et al., altitude (2180 m) Indian Himalayan site, Mukteshwar, were 2004; Spracklen et al., 2006, 2009). While in the atmo- analyzed. For this period, the days were classified, and the sphere, these particles are affected by several physical and particle formation and growth rates were calculated for clear chemical processes influencing the particle climatic proper- new particle formation (NPF) event days. The NPF events ties, such as their scattering and absorbing characteristics and showed a pronounced seasonal cycle. The frequency of the their ability to act as Cloud Condensation Nuclei (CCN).