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Trains of the Colorado Rockies
Trains of the Colorado Rockies Presented by San Bernardino County Museum Association Tour Information Presentation When: Thursday, November 4th Where: San Bernardino County Museum Association 2024 Orange Tree Lane, Redlands, CA 92374-4560 Time: 6:00 PM For more information call and to R.S.V.P. Please contact Lawanda Avery-Brown at (909) 307-2669 Ext. 225 [email protected] Day 1: Saturday, August 06, 2011 Denver, Colorado - Tour Begins August 06 - August 14, 2011 Traverse the Colorado Rockies with Collette Vacations as you journey through the beauty of Highlights... nature with Alpine lakes, towering peaks and rolling Denver • Rocky Mountain National Park • Georgetown Loop Railroad • Grand Junction • meadows at every turn. Your tour begins in the “Mile Colorado National Monument • Durango & High City” of Denver, Colorado. Silverton Railroad • Durango • Mesa Verde Today Dinner is included. National Park • Royal Gorge Railroad • Colorado Springs • Pike's Peak Cog Railway • Garden of the Gods • Day 2: Sunday, August 07, 2011 Denver - Boulder - Estes Park - Rocky Mountain 9 Days • 12 Meals: National Park - Denver 8 Breakfasts • 4 Dinners Travel to the resort village of Estes Park, famous for its Stanley Hotel, the inspiration for Stephen King's Per Person Rates*: novel, The Shining. Enjoy leisure time to meander Double $2349 among its unique shops and fine galleries. Next stop Single $2949 is Rocky Mountain National Park to discover the Triple $2319 true meaning of “panoramic” as you experience incredible views. Then, travel across the famed *Included in Price: Air Taxes and Fees/Surcharges of Trail Ridge Road* which forms the highest $50 (subject to increase until paid in full), Hotel Transfers, Round Trip Air from Ontario International. -
IOWNER of PROPERTY NAME Mayor Edward Piass
Form No. 10-300 (Rev. 10-74) UNITED STATES DEPARTMEiN T OF THE INTERIOR NATIONAL PARK SERVICE NATIONAL REGISTER OF HISTORIC PLACES INVENTORY -- NOMINATION FORM SEE INSTRUCTIONS IN HOW TO COMPLETE NATIONAL REGISTER FORMS TYPE ALL ENTRIES -- COMPLETE APPLICABLE SECTIONS I NAME HISTORIC Georgetown-Silver Plume Historic District AND/OR COMMON Georgetown-Silver Plume Historic District | LOCATION STREET& NUMBER Interstate 70 _NOT FOR PUBLICATION CITY. TOWN CONGRESSIONAL DISTRICT Georgetown __. VICINITY OF STATE CODE COUNTY CODE Colorado Clear Creek UCLA SSIFI c ATI ON CATEGORY OWNERSHIP STATUS PRESENT USE X^D I STRICT _ PUBLIC -^OCCUPIED _ AGRICULTURE _ MUSEUM _BUILDING(S) _ PRIVATE —UNOCCUPIED —COMMERCIAL —PARK —STRUCTURE X_BOTH —WORK IN PROGRESS _ EDUCATIONAL —PRIVATE RESIDENCE _SITE PUBLIC ACQUISITION ACCESSIBLE —ENTERTAINMENT —RELIGIOUS _OBJECT _IN PROCESS _YES: RESTRICTED _ GOVERNMENT —SCIENTIFIC _BEING CONSIDERED _XvES: UNRESTRICTED —INDUSTRIAL —TRANSPORTATION _ NO —MILITARY X_OTHER: IOWNER OF PROPERTY NAME Mayor Edward PIass City Hall, 6th Street CITY. TOWN STATE Georgetown VICINITY OF Colorado LOCATION OF LEGAL DESCRIPTION COURTHOUSE, Registry of Deeds, Clear Creek County Courthouse REGISTRY OF DEEDS, ETC. STREET& NUMBER Argentine Street CITY, TOWN STATE Georgetown Colorado TITLE DATE in progress —FEDERAL iSTATE _COUNTY _LOCAL DEPOSITORY FOR SURVEY RECORDS 1880 Gaylord Street CITY, TOWN STATE Denver Colorado DESCRIPTION CONDITION CHECK ONE CHECK ONE —EXCELLENT _DETERIORATED _UNALTERED _X_ORIGINALSITE MOVED DATF _X_GOOD __RUINS JC.ALTERED _FA|R __UNEXPOSED DESCRIBETHE PRESENT AND ORIGINAL (IF KNOWN) PHYSICAL APPEARANCE The Georgetown-Silver Plume Historic Mining District possesses remarkable integrity and the historic structures in the two towns are reminescent of a bygone era. Georgetown, in particular, is unique among Colorado's mining towns. -
1 1. Species: Mountain Plover (Charadrius Montanus) 2. Status
1. Species: Mountain Plover (Charadrius montanus) 2. Status: Table 1 summarizes the current status of this species or subspecies by various ranking entity and defines the meaning of the status. Table 1. Current status of Charadrius montanus Entity Status Status Definition NatureServe G3 Species is Vulnerable At moderate risk of extinction or elimination due to a fairly restricted range, relatively few populations or occurrences, recent and widespread declines, threats, or other factors. CNHP S2B Species is Imperiled At high risk of extinction or elimination due to restricted range, few populations or occurrences, steep declines, severe threats, or other factors. (B=Breeding) Colorado SGCN, Tier 1 Species of Greatest Conservation Need State List Status USDA Forest R2 Sensitive Region 2 Regional Forester’s Sensitive Species Service USDI FWSb BoCC Included in the USFWS Bird of Conservation Concern list a Colorado Natural Heritage Program. b US Department of Interior Fish and Wildlife Service. The 2012 U.S. Forest Service Planning Rule defines Species of Conservation Concern (SCC) as “a species, other than federally recognized threatened, endangered, proposed, or candidate species, that is known to occur in the plan area and for which the regional forester has determined that the best available scientific information indicates substantial concern about the species' capability to persist over the long-term in the plan area” (36 CFR 219.9). This overview was developed to summarize information relating to this species’ consideration to be listed as a SCC on the Rio Grande National Forest, and to aid in the development of plan components and monitoring objectives. 3. Taxonomy Genus/species Charadrius montanus is accepted as valid (ITIS 2015). -
PEAK to PRAIRIE: BOTANICAL LANDSCAPES of the PIKES PEAK REGION Tass Kelso Dept of Biology Colorado College 2012
!"#$%&'%!(#)()"*%+'&#,)-#.%.#,/0-#!"0%'1%&2"%!)$"0% !"#$%("3)',% &455%$6758% /69:%8;%+<878=>% -878?4@8%-8776=6% ABCA% Kelso-Peak to Prairie Biodiversity and Place: Landscape’s Coat of Many Colors Mountain peaks often capture our imaginations, spark our instincts to explore and conquer, or heighten our artistic senses. Mt. Olympus, mythological home of the Greek gods, Yosemite’s Half Dome, the ever-classic Matterhorn, Alaska’s Denali, and Colorado’s Pikes Peak all share the quality of compelling attraction that a charismatic alpine profile evokes. At the base of our peak along the confluence of two small, nondescript streams, Native Americans gathered thousands of years ago. Explorers, immigrants, city-visionaries and fortune-seekers arrived successively, all shaping in turn the region and communities that today spread from the flanks of Pikes Peak. From any vantage point along the Interstate 25 corridor, the Colorado plains, or the Arkansas River Valley escarpments, Pikes Peak looms as the dominant feature of a diverse “bioregion”, a geographical area with a distinct flora and fauna, that stretches from alpine tundra to desert grasslands. “Biodiversity” is shorthand for biological diversity: a term covering a broad array of contexts from the genetics of individual organisms to ecosystem interactions. The news tells us daily of ongoing threats from the loss of biodiversity on global and regional levels as humans extend their influence across the face of the earth and into its sustaining processes. On a regional level, biologists look for measures of biodiversity, celebrate when they find sites where those measures are high and mourn when they diminish; conservation organizations and in some cases, legal statutes, try to protect biodiversity, and communities often struggle to balance human needs for social infrastructure with desirable elements of the natural landscape. -
Train Buff Bucket-List Getaway
Published on Colorado.com (https://www.colorado.com) Train Buff Bucket List Getaway 5 days More Itineraries Hear the shrill whistle signaling you're about to start your train journey as you traverse Colorado's breathtaking scenery on each day of this trip. Starting in Denver, you'll spot wildlife, stay in historic hotels and maybe even soak in a hot spring along the way. Sustainability Activity How to Give Back to These Special Places: There are special places and unique vistas around nearly every Colorado corner. You can help ensure these places exist for generations to come by staying on roads and trails, keeping speeds in check, leaving campsites and picnic spots just as you found them, and following instructional signs while you?re out and about in our state. Day 1 ACTIVITY Forney Museum of Transportation Explore one of the largest and most unique transportation collections! See Union Pacific's "Big Boy", Amelia Earhart's Kissel car & special rotating exhibits. Open year-round Mon.? Sat.10am?5pm ... Insider's Tip Head West to Golden: Soak in the views of the Rockies as you head west: Your next stop is the charming town of Golden. LUNCH Old Capitol Grill & Smokehouse The Old Capitol Grill & Smokehouse offers up a full menu of smoked meats and classic American fare with some unique twists, in an historic setting.... ACTIVITY Colorado Railroad Museum Bringing Colorado railroad history to life year-round. Stroll the Museum's 15-acre railyard featuring more than 100 historic railcars. Also, tour exhibit galleries, a renowned library,... DINNER Buffalo Rose Saloon An authentic American West saloon and restaurant featuring some of Colorado's best live entertainment, inspiring indoor and outdoor seating environments and creative cuisine. -
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. -
Geochronology Database for Central Colorado
Geochronology Database for Central Colorado Data Series 489 U.S. Department of the Interior U.S. Geological Survey Geochronology Database for Central Colorado By T.L. Klein, K.V. Evans, and E.H. DeWitt Data Series 489 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2010 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: T.L. Klein, K.V. Evans, and E.H. DeWitt, 2009, Geochronology database for central Colorado: U.S. Geological Survey Data Series 489, 13 p. iii Contents Abstract ...........................................................................................................................................................1 Introduction.....................................................................................................................................................1 -
Rail System ' 0 ° 1
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Newsletter-379-Apr1991
Rocky. MountahiliiK REPOT THE ROCKY MOUNTAIN RAILROAD CLUB MEETING SCHEDULE: April, 1991........................................... No. 379 Club Telephone........................ (303) 431-4354 P. 0. Box 2391........ Denver, Colorado 80201 April 9, 1991 -- 7:30 p.m. CURRENT NEWS AND HISTORICAL NOTES OF ROCKY Southeast wing of Christ Episcopal Church, MOUNTAIN RAILROADING PUBLISHED MONTHLY FOR 2950 South University at Bates. Off-street ITS MEMBERS BY THE ROCKY MOUNTAIN RAILROAD parking at rear (east) of meeting hall. CLUB. Please use the building's south entrance. Jim Trowbridge....................................... Editor CLUB MEMBERSHIP Les Grenz.............................. Associate Editor David W. Salter................................ President Membership in the Rocky Mountain Railroad Joe Priselac.......................... Vice President Club may be obtained by sending $19.00 Bill Gordon........................................ Secretary ($15.00 annual dues plus enrollment fee Bert Bidwell ;................................... Treasurer of $4.00) to: ROCKY MOUNTAIN RAILROAD CLUB, P. 0. Box 2391, Denver, Colorado 80201. An Send all items for publication to: Rocky Associate Membership for Spouses and Mountain Rail Report, c/o Jim Trowbridge, Children is also available for a yearly Editor, 502 South Cody Street, Lakewood, rate of $7.50. On regular memberships, new Colorado 80226. members joining after April of each year may obtain membership for a payment of COPY DEADLINE ALL copy for publication $4.00 enrollment fee plus $1.25 for each in the May, 1991 Rail Report is due month remaining in the calendar year, Dues no later than April 9, 1991!! for the next year are solicited in November of the current year. APRIL 9 PROGRAM MEMBERSHIP INQUIRIES Please refer address changes, new member The event of the year has arrived!! April ships, lost newsletters, missing newsletter is the Annual Potpourri Night Program. -
Profiles of Colorado Roadless Areas
PROFILES OF COLORADO ROADLESS AREAS Prepared by the USDA Forest Service, Rocky Mountain Region July 23, 2008 INTENTIONALLY LEFT BLANK 2 3 TABLE OF CONTENTS ARAPAHO-ROOSEVELT NATIONAL FOREST ......................................................................................................10 Bard Creek (23,000 acres) .......................................................................................................................................10 Byers Peak (10,200 acres)........................................................................................................................................12 Cache la Poudre Adjacent Area (3,200 acres)..........................................................................................................13 Cherokee Park (7,600 acres) ....................................................................................................................................14 Comanche Peak Adjacent Areas A - H (45,200 acres).............................................................................................15 Copper Mountain (13,500 acres) .............................................................................................................................19 Crosier Mountain (7,200 acres) ...............................................................................................................................20 Gold Run (6,600 acres) ............................................................................................................................................21 -
The Geologic Story of Colorado's Sangre De Cristo Range
The Geologic Story of Colorado’s Sangre de Cristo Range Circular 1349 U.S. Department of the Interior U.S. Geological Survey Cover shows a landscape carved by glaciers. Front cover, Crestone Peak on left and the three summits of Kit Carson Mountain on right. Back cover, Humboldt Peak on left and Crestone Needle on right. Photograph by the author looking south from Mt. Adams. The Geologic Story of Colorado’s Sangre de Cristo Range By David A. Lindsey A description of the rocks and landscapes of the Sangre de Cristo Range and the forces that formed them. Circular 1349 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2010 This and other USGS information products are available at http://store.usgs.gov/ U.S. Geological Survey Box 25286, Denver Federal Center Denver, CO 80225 To learn about the USGS and its information products visit http://www.usgs.gov/ 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Lindsey, D.A., 2010, The geologic story of Colorado’s Sangre de Cristo Range: U.S. Geological Survey Circular 1349, 14 p. iii Contents The Oldest Rocks ...........................................................................................................................................1 -
Isotopic Age Determinations, Unaltered and Hydrothermally Altered Igneous Rocks, North-Central Colorado Mineral Belt A.A
Isotopic age determinations, unaltered and hydrothermally altered igneous rocks, north-central Colorado mineral belt A.A. Bookstrom, C.W. Naeser, and J.R. Shannon Isochron/West, Bulletin of Isotopic Geochronology, v. 49, pp. 13-20 Downloaded from: https://geoinfo.nmt.edu/publications/periodicals/isochronwest/home.cfml?Issue=49 Isochron/West was published at irregular intervals from 1971 to 1996. The journal was patterned after the journal Radiocarbon and covered isotopic age-dating (except carbon-14) on rocks and minerals from the Western Hemisphere. Initially, the geographic scope of papers was restricted to the western half of the United States, but was later expanded. The journal was sponsored and staffed by the New Mexico Bureau of Mines (now Geology) & Mineral Resources and the Nevada Bureau of Mines & Geology. All back-issue papers are available for free: https://geoinfo.nmt.edu/publications/periodicals/isochronwest This page is intentionally left blank to maintain order of facing pages. 13 ISOTOPIC AGE DETERMINATIONS, UNALTERED AND HYDROTHERMALLY ALTERED IGNEOUS ROCKS, NORTH-CENTRAL COLORADO MINERAL BELT ARTHUR A. BOOKSTROM 1805 Glen Ayr Dr., Lakewood, CO 80215 CHARLES W. NAESER U.S. Geological Survey, Denver, CO 80225 JAMES R. SHANNON Department of Geology, Colorado School of Mines, Golden, CO 80401 Monzonite and granodiorite intrusions of the Empire Fission-track age determinations were done in the fission- district are early Tertiary (65 Ma) in age, as dated by track laboratory of the U.S. Geological Survey in Denver, Simmons and Hedge (1978). Monzonite and granodiorite and at the University of Utah Research Institute. People intrusions of the Alma district have yielded isotopic ages who cooperated in this study include Mark Coolbaugh, ranging from 71 to 41 Ma (Bookstrom, in press).