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Group Living Frequently Asked Questions
Group Living Project – Common Questions General questions about the project: Page 1 Household Regulations: Page 3 Residential Care: Page 6 Advisory Committee: Page 9 Next Steps: Page 10 What is this project about and how long has it been going on? For the last two and a half years, Denver city planners have been working with residents, policy experts, advocates and service providers for vulnerable populations and other community members to update the Denver Zoning Code’s regulations on residential uses. These regulations govern everything from conventional households to group homes, shelters and assisted living facilities. Why do residential use rules need to be updated? Current rules create obstacles for residents who need flexible housing options and for providers who offer much-needed services to vulnerable populations. Current rules also perpetuate inequity by making it harder for certain communities to live in residential neighborhoods and near jobs, transit or other services they need. The project and the proposed changes aim to increase flexibility and housing options for residents, to streamline permitting processes for providers while fostering good relationships with neighbors, and to make it easier for those experiencing homelessness, trying to get sober or who have other special needs to live and access services with dignity. Why can’t we move more slowly with these changes? This project has been in progress for more than two years. The issues addressed have become even more urgent in the wake of the ongoing pandemic, job losses that are leading to a wave of evictions, the forthcoming loss of Denver’s existing community corrections resources, and our country’s long-overdue awakening to issues of equity. -
Denudation History and Internal Structure of the Front Range and Wet Mountains, Colorado, Based on Apatite-Fission-Track Thermoc
NEW MEXICO BUREAU OF GEOLOGY & MINERAL RESOURCES, BULLETIN 160, 2004 41 Denudation history and internal structure of the Front Range and Wet Mountains, Colorado, based on apatitefissiontrack thermochronology 1 2 1Department of Earth and Environmental Science, New Mexico Institute of Mining and Technology, Socorro, NM 87801Shari A. Kelley and Charles E. Chapin 2New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, NM 87801 Abstract An apatite fissiontrack (AFT) partial annealing zone (PAZ) that developed during Late Cretaceous time provides a structural datum for addressing questions concerning the timing and magnitude of denudation, as well as the structural style of Laramide deformation, in the Front Range and Wet Mountains of Colorado. AFT cooling ages are also used to estimate the magnitude and sense of dis placement across faults and to differentiate between exhumation and faultgenerated topography. AFT ages at low elevationX along the eastern margin of the southern Front Range between Golden and Colorado Springs are from 100 to 270 Ma, and the mean track lengths are short (10–12.5 µm). Old AFT ages (> 100 Ma) are also found along the western margin of the Front Range along the Elkhorn thrust fault. In contrast AFT ages of 45–75 Ma and relatively long mean track lengths (12.5–14 µm) are common in the interior of the range. The AFT ages generally decrease across northwesttrending faults toward the center of the range. The base of a fossil PAZ, which separates AFT cooling ages of 45– 70 Ma at low elevations from AFT ages > 100 Ma at higher elevations, is exposed on the south side of Pikes Peak, on Mt. -
Analysis and Correlation of Growth
ANALYSIS AND CORRELATION OF GROWTH STRATA OF THE CRETACEOUS TO PALEOCENE LOWER DAWSON FORMATION: INSIGHT INTO THE TECTONO-STRATIGRAPHIC EVOLUTION OF THE COLORADO FRONT RANGE by Korey Tae Harvey A thesis submitted to the Faculty and Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Master of Science (Geology). Golden, Colorado Date __________________________ Signed: ________________________ Korey Harvey Signed: ________________________ Dr. Jennifer Aschoff Thesis Advisor Golden, Colorado Date ___________________________ Signed: _________________________ Dr. Paul Santi Professor and Head Department of Geology and Geological Engineering ii ABSTRACT Despite numerous studies of Laramide-style (i.e., basement-cored) structures, their 4-dimensional structural evolution and relationship to adjacent sedimentary basins are not well understood. Analysis and correlation of growth strata along the eastern Colorado Front Range (CFR) help decipher the along-strike linkage of thrust structures and their affect on sediment dispersal. Growth strata, and the syntectonic unconformities within them, record the relative roles of uplift and deposition through time; when mapped along-strike, they provide insight into the location and geometry of structures through time. This paper presents an integrated structural- stratigraphic analysis and correlation of three growth-strata assemblages within the fluvial and fluvial megafan deposits of the lowermost Cretaceous to Paleocene Dawson Formation on the eastern CFR between Colorado Springs, CO and Sedalia, CO. Structural attitudes from 12 stratigraphic profiles at the three locales record dip discordances that highlight syntectonic unconformities within the growth strata packages. Eight traditional-type syntectonic unconformities were correlated along-strike of the eastern CFR distinguish six phases of uplift in the central portion of the CFR. -
Stratigraphy of the Project Area
I BRITISH &! COLUMBLA Ministry of Employment and Investment ENERGY AND MINERALS DIVISION Hon. Dan Miller. Minister Geological Survey Branch THE STIKINE PROJECT GEOLOGY OF WESTERN TELEGRAPH CREEK MAP AREA, NORTHWESTERN BRITISH COLUMBIA (NTS 104G/5,6, llW, 12 AND 13) By Derek A. Brown1 , Michael H. Gunning2 and Charles J. Greig3 Appendix 3 - Conodont identifications by "I. Orchard, Geological Survey of Canada 1. Geological Surve Branch, British Colunlhia Ministry of Employment andYlnvestment 2. Department of Geology, University of Western Ontario, London, Ontario 3. C.G. Greig and Associates Ltd., Penticton, B.C. BULLETIN 95 Canadian Cataloguing in Publication Data Brawn. Derek Anlhony. 1959- The Stikine project : geology of western Telegraph Creek map area. nonhwenlem British Columbia (NTS.lMG15. 6, IIW. 12and 13) Issued by Geological Survey Branch. Includes bibliographical references: p ISBN 0-7726-2502-6 1, Geology -British Columbia -Telegraph Creek Region 2. Geochemistry - British Columbia - Telegraph Creek VICTORIA Region. 3. Geology. Economic - British Columbia - BRITISH COLUMBIA Telegraph Creek Region. 4. Mines and mineral resources - CANADA British Columbia - Telegraph Creek Region. 1. Gunning. Michael H. 11. Greig.Charles James, 1956- . 111. British Columbia. Ministry of Employment and Investmenl. IV. MAY 1996 BritishColumbia. Geological Survey Branch. V. Title. VI. Title: Geology of western Telegraph Creek maparea, nanhwertern British Columbia (NTS 1WG15.6. 1 IW. 12 and 13). V11. Series: Bulletin (British Columbia. Ministry of Employment and Investment) ;95. QE187.B76 1996 557.11’185 (395-960208-9 Frontispiece. View north along the Scud Glacier. Ambition Mountainis underlain by Permian limestone and metavolcanic rocks. Ministry of Emp/oyment and Inveshent TABLE OF CONTENTS CHAPTER 1 Chemistry ..................... -
Memorial to W.A. “Bill” Cobban (1916–2015) NEAL L
Memorial to W.A. “Bill” Cobban (1916–2015) NEAL L. LARSON Larson Paleontology Unlimited, LLC, Keystone, South Dakota 57745, USA; [email protected] NEIL H. LANDMAN American Museum of Natural History, Division of Paleontology (Invertebrates), New York, New York 10024, USA; [email protected] STEPHEN C. HOOK Atarque Geologic Consulting, LLC, Socorro, New Mexico 87810, USA; [email protected] Dr. W.A. “Bill” Cobban, one of the most highly re- spected, honored and published geologist-paleontologists of all time, passed away peacefully in his sleep in the morning of 21 April 2015 at the age of 98 in Lakewood, Colorado. Bill was an extraordinary field collector, geologist, stratigrapher, biostratigrapher, paleontologist, and mapmaker who spent nearly his entire life working for the U.S. Geo- logical Survey (USGS). In a career that spanned almost 75 years, he fundamentally changed our understanding of the Upper Cretaceous Western Interior through its fossils, making it known throughout the world. William Aubrey “Bill” Cobban was born in 1916 near Great Falls, Montana. As a teenager, he discovered a dinosaur in the Kootenai Formation catching the attention of Barnum Brown, premier dinosaur collector at the American Museum of Natural History, where the dinosaur now resides. A few years later, as Bill told, he read about the discovery of fossil bones in Shelby, Montana, during excavation of the Toole County Courthouse. The bones turned out to actually be baculites and other iridescent ammonites. These ammonites made such an impression on Bill they would change his life forever. He attended Montana State University in 1936, where he met a geology professor who encouraged an already developing love for geology and paleontology and received his B.S. -
RE-EVALUATION, Mileposts 149 to 161
RE-EVALUATION, Mileposts 149 to 161 Interstate 25 Improvements through the Colorado Springs Area Environmental Assessment PALEONTOLOGY TECHNICAL MEMO April 2012 Prepared for: CDOT Region 2 Prepared by: Doug Eberhart, Telephone (719) 520-5800 Introduction The Colorado Department of Transportation (CDOT) has prepared this technical memorandum to update findings with regards to the paleontological resources described in the original 2004 I-25 Environmental Assessment (EA) with regard to the portion of the Proposed Action between Woodmen Road (Exit 149) in Colorado Springs and State Highway 105 in Monument (Exit 161). The purpose of the EA’s Proposed Action is to relieve existing traffic congestion and address project future congestion on I-25 within the Colorado Springs Urbanized Area. The I-25 EA originally evaluated impacts for the widening of I-25 between South Academy Boulevard (Exit 135) and SH 105, together with reconstruction of various I-25 interchanges within this corridor. Page 2-10 of the EA stated that, “Consistent with projected traffic demand in the I-25 corridor, the conceptual phasing for the Proposed Action calls for: (1) initially six-laning through central Colorado Springs, then (2) six-laning in northern El Paso Figure 1. I -25 EA Re -evaluation Project Vicinity County, and finally (3) adding HOV [High-Occupancy Vehicle] lanes through central Colorado Springs and widening to six lanes south to South Academy Boulevard.” For the year 2012, CDOT has received funding to begin the second phase, meaning to widen I-25 to six lanes in northern El Paso County. The EA calls for eventually widening I-25 all the way to SH105. -
Geology and Hydrology, Front Range Urban Corridor, Colorado
Bibliography and Index of Geology and Hydrology, Front Range Urban Corridor, Colorado By FELICIE CHRONIC and JOHN CHRONIC GEOLOGICAL SURVEY BULLETIN 1306 Bibliographic citations for more than 1,800 indexed reports, theses, and open-file releases concerning one of the Nation's most rapidly growing areas UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1974 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 74-600045 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D. C. 20402- Price $1.15 (paper cover) Stock Number 2401-02545 PREFACE This bibliography is intended for persons wishing geological information about the Front Range Urban Corridor. It was compiled at the University of Colorado, funded by the U.S. Geological Survey, and is based primarily on references in the Petroleum Research Microfilm Library of the Rocky Mountain Region. Extensive use was made also of U.S. Geological Survey and American Geological Institute bibliographies, as well as those of the Colorado Geological Survey. Most of the material listed was published or completed before July 1, 1972; references to some later articles, as well as to a few which were not found in the first search, are appended at the end of the alphabetical listing. This bibliography may include more references than some users feel are warranted, but the authors felt that the greatest value to the user would result from a comprehensive rather than a selective listing. Hence, we decided to include the most significant synthesizing articles and books in order to give a broad picture of the geology of the Front Range Urban Corridor, and to include also some articles which deal with geology of areas adjacent to, and probably pertinent to, the corridor. -
Church Properties for Sale Colorado
Church Properties For Sale Colorado recogniseNeville remains his peevishness. pleasurable Conciliarafter Morley Brandy centrifugalize disfeatures parcel easily or while tweezes Corky any always Oldham. hams Hush-hush his mousses and brush-uptinsel Kennedy incognita, interlard he tetanised so smilingly so opposite. that Vernen RMCLT utilizes a scattered site challenge to homeownership our homes and families are scattered throughout the better of Colorado Springs and El Paso County. Please select areas that were an affordable homeownership; or colorado square retail center is located in short on the school year and councilman ed vela have. Together we carry A to Z commercial real estate development services to User. Sale Lease Properties NAI Shames Makovsky. Beyond Just Homes with Pamela Church Real Estate in. The sale to fix them includes large retail centers properties for sale whose setting. Church Properties Duhs Commercial. Text or scheduled conference room, no end and east facing with rewards and gift ideas about school activities for rent a pin leading commercial properties for sale offering such. Beautiful gown in Walsenburg CO This judge a religious facility built in 1929. Colorado Retail Properties For Sale Cityfeet. Durango Commercial Real Estate For Sale Durango CO. Commercial Real Estate for Sale & Rent Colorado Springs. Properties For excellent in Colorado Historic Homes United. See 15 Colorado Churches Religious Facilities for country Access photos 3D tours and accident on the 1 commercial real estate site. Littleton CO 0123 UNDER one Sale Price 1350000 16512 psf CAP Rate 734 Building Size 176 sf Lot Size 3177 SF 73 acres. The content relating to real estate for sale under this Web site comes in fee from the. -
Cretaceous and Tertiary Formations Op the Wasatch Plateau, Utah * by Edmund M
BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA VOL. 36. PP. 439*454 SEPTEMBER 30. 1925 CRETACEOUS AND TERTIARY FORMATIONS OP THE WASATCH PLATEAU, UTAH * BY EDMUND M. SPIEKER AND JOHN B. REESIDE, JR. {Read before the Geological Society December SO, 1925) CONTENTS Page Introduction.......................................................................................................................... 435 General features of plateau........................................................................................... 436 Location and surface features............................................................................. 436 Structure.......................................................................................................................436 Mancos shale........................................................................................................................ 436 General statement...................................................................................................... 436 Lower shale member................................................................................................. 437 Ferron sandstone member...................................................................................... 438 Middle shale member............................................................................................... 438 Emery sandstone member...................................................................................... 439 Upper shale member...........................................................................'....................439 -
Abdullin Colostate 0053N 11378.Pdf (3.002Mb)
THESIS GEOPHYSICAL CONSTRAINTS ON THE FLEXURAL SUBSIDENCE OF THE DENVER BASIN Submitted by Ayrat Abdullin Department of Geosciences In partial fulfillment of the requirements For the Degree of Master of Science Colorado State University Fort Collins, Colorado Fall 2012 Master’s Committee: Advisor: Dennis L. Harry Sven Egenhoff Michael Lefsky ABSTRACT GEOPHYSICAL CONSTRAINTS ON THE FLEXURAL SUBSIDENCE OF THE DENVER BASIN The Denver Basin is an asymmetric Laramide (Late Cretaceous through Eocene) foreland basin covering portions of eastern Colorado, northwestern Kansas, southwestern Nebraska, and southeastern Wyoming, USA. It is bordered on the west by the Rocky Mountain Front Range Uplift, a basement cored Laramide anticline bounded by thrust faults, and on the east by the Great Plains and stable North American craton. A ~400 mGal negative Bouguer gravity anomaly exists over the Denver Basin and Front Range Uplift, with its minimum located over the highest topography in the central part of the uplift, approximately 100 km west of the Denver Basin. This study examines three hypotheses concerning the isostatic state of the basin and adjacent Front Range Uplift. These hypotheses are that the modern shape of the basin is due to: 1) flexure of the lithosphere under the surface load of the current topography, or 2) flexure under a subsurface load beneath the Rocky Mountains, or 3) a combination of both surface and subsurface loads. To test these hypotheses, spectral analysis and forward gravity modeling was conducted along three profiles located in the northern, central, and southern parts of the basin. Bouguer gravity power spectra along the profiles reveal 5 major density interfaces interpreted to represent the base of the lithosphere (at depths of 132 to 153 km), base of the crust (45-55 km), a mid-crustal boundary (about 20 km), the top of Precambrian basement (1-2 km), and a boundary between the Pierre Shale and Niobrara Formations within the pre-Laramide sedimentary section (-1-0 km). -
The Rocky Mountain Front, Southwestern USA
The Rocky Mountain Front, southwestern USA Charles E. Chapin, Shari A. Kelley, and Steven M. Cather New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, New Mexico 87801, USA ABSTRACT northeast-trending faults cross the Front thrust in southwest Wyoming and northern Range–Denver Basin boundary. However, Utah. A remarkable attribute of the RMF is The Rocky Mountain Front (RMF) trends several features changed from south to north that it maintained its position through multi- north-south near long 105°W for ~1500 km across the CMB. (1) The axis of the Denver ple orogenies and changes in orientation from near the U.S.-Mexico border to south- Basin was defl ected ~60 km to the north- and strength of tectonic stresses. During the ern Wyoming. This long, straight, persistent east. (2) The trend of the RMF changed from Laramide orogeny, the RMF marked a tec- structural boundary originated between 1.4 north–northwest to north. (3) Structural tonic boundary beyond which major contrac- and 1.1 Ga in the Mesoproterozoic. It cuts style of the Front Range–Denver Basin mar- tional partitioning of the Cordilleran fore- the 1.4 Ga Granite-Rhyolite Province and gin changed from northeast-vergent thrusts land was unable to penetrate. However, the was intruded by the shallow-level alkaline to northeast-dipping, high-angle reverse nature of the lithospheric fl aw that underlies granitic batholith of Pikes Peak (1.09 Ga) faults. (4) Early Laramide uplift north of the RMF is an unanswered question. in central Colorado. -
Colorado Agriculture Bibliography 2005 Subject Areas: Mining And
Colorado Agriculture Bibliography 2005 A Bibliography of Primary and Secondary Material Published 1820-1945 Subject Areas: Mining and Geology Type of Materials: Serials Produced by the Colorado State University Libraries Copyright by Colorado State University Libraries Applies Overview This portable document file (.pdf ) is part of the Colorado Agriculture Bibliography project and includes bibliographic information on a variety of topics related to Colorado’s agricultural and rural past. The topics covered in this project are varied but include agriculture, education, water, mining, tourism, recreation, and more. The bibliography contains information about but not full-text for books, journals, dissertations, theses, archival collections, maps, photos, pamphlets, and more. The Web site and bibliography reflects Colorado’s contribution to the Preserving the History of United States Agriculture and Rural Life Project. This nation-wide effort aims to identify and preserve state and locally significant literature. The project involves the National Endowment for the Humanities (NEH), Cornell University, the United States Agricultural Information Network (USAIN), the National Agricultural Library (NAL), and other land-grant universities. The records in this bibliography may cover several subject areas and are listed alphabetically by author. A searchable website of the bibliography is also available if you would like to create searches and find information on other topics. The bibliography of Colorado history project was funded in part by a grant from the National Endowment for the Humanities (NEH). The project is part of the United States Agriculture Information Network (USAIN) Preservation Program. Cornell University coordinated the grant project. 1 1. _______ (1886-1890). The Mining industry . Denver, Colo.: [s.n.].