Eagle River Inventory and Assessment
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A History of Northwest Colorado
II* 88055956 AN ISOLATED EMPIRE BLM Library Denver Federal Center Bldg. 50, OC-521 P-O. Box 25047 Denver, CO 80225 PARE* BY FREDERIC J. ATHEARN IrORIAh ORADO STATE OFFICE BUREAU OF LAND MANAGEMENT 1976 f- W TABLE OF CONTENTS Wb Preface. i Introduction and Chronological Summary . iv I. Northwestern Colorado Prior to Exploitation . 1 II. The Fur Trade. j_j_ III. Exploration in Northwestern Colorado, 1839-1869 23 IV. Mining and Transportation in Early Western Colorado .... 34 V. Confrontations: Settlement Versus the Ute Indians. 45 VI. Settlement in Middle Park and the Yampa Valley. 63 VII. Development of the Cattle and Sheep Industry, 1868-1920... 76 VIII. Mining and Transportation, 1890-1920 .. 91 IX. The "Moffat Road" and Northwestern Colorado, 1903-1948 . 103 X. Development of Northwestern Colorado, 1890-1940. 115 Bibliography 2&sr \)6tWet’ PREFACE Pu£Eose: This study was undertaken to provide the basis for identification and evaluation of historic resources within the Craig, Colorado District of the Bureau of Land Management. The narrative of historic activities serves as a guide and yardstick regarding what physical evidence of these activities—historic sites, structures, ruins and objects—are known or suspected to be present on the land, and evaluation of what their historical significance may be. Such information is essential in making a wide variety of land management decisions effecting historic cultural resources. Objectives: As a basic cultural resource inventory and evaluation tool, the narrative and initial inventory of known historic resources will serve a variety of objectives: 1. Provide information for basic Bureau planning docu¬ ments and land management decisions relating to cultural resources. -
See the Notice
Notice Date: July 19, 2019 To: General Authorities; General Officers; Area Seventies; and the following leaders in the United States and Canada: Stake, Mission, and District Presidents; Bishops and Branch Presidents; Members of Stake and Ward Councils From: Priesthood and Family Department (1-801-240-2134) Subject: For the Strength of Youth (FSY) Conferences in the United States and Canada As part of the Children and Youth effort announced on May 8, 2018, the Church will begin holding For the Strength of Youth (FSY) conferences in the United States and Canada. These conferences have been held outside the U.S. and Canada for many years and have proven to be a strength to youth and also to the young single adults who serve as counselors. See the attached description of FSY conferences for more information. Beginning in 2021 and 2022, all stakes in the U.S. and Canada will participate in FSY conferences every other year. During 2020, a smaller number of FSY conferences will be held at locations in the U.S. and Canada to prepare for full implementation. Attached is the list of stakes participating in 2020. If your stake has been selected to participate in FSY in 2020, please do not plan treks or youth conferences to be held during that year. Young Women and Young Men camps may be held annually, as usual. If your stake has been selected but you believe your stake has an exceptional circumstance and cannot participate in FSY in 2020, please contact your Area Seventy. Dates, locations, financing arrangements, and other information, such as the calling of young single adults as counselors, will be shared at a later date. -
National Monument
DINOSAUR NATIONAL MONUMENT COLORADO UTAH corner of the monument. The original 80 renewed in 1923-24 by the National Mu acres of this area were set aside in 1915 to seum, Washington, D. C, and the University DINOSAUR preserve these fossil bones. The boundaries of Utah. Twenty-six nearly complete skele were extended in 1938 to include the scenic tons and a great number of partial ones canyon country. were recovered. Twelve dinosaur species National Monument At monument headquarters, 6 miles north were represented. The longest skeleton— of Jensen, Utah, is a temporary museum con Dipledocus—was 84 feet, the shortest— taining exhibits which will help you under Laosaurus—6 feet. Many of the bones have A semiarid wilderness plateau, cut by deep canyons and con stand the local geology and the story of the been assembled as complete skeletons which taining rich deposits of skeletal remains of prehistoric reptiles. dinosaurs. The Dinosaur Quarry is a quarter you may see in museums in Pittsburgh; of a mile by trail from the museum. It is Washington, D. C.; New York City; Lin an excavation in the top of a ridge where coln, Nebr.; Denver; Salt Lake City; and IN DINOSAUR NATIONAL MONU towering canyon walls. He named numerous rock layers have been removed to expose the Toronto, Canada. MENT you will find a vast wilderness geographic features, including the treach fossil-bearing strata of the Morrison forma little changed by man. Its principal scenic erous Disaster Falls, where he lost one of tion of Jurassic age, deposited approximately Early Indians features are the deep and narrow canyons his boats. -
Pennsylvanian Minturn Formation, Colorado, U.S.A
Journal of Sedimentary Research, 2008, v. 78, 0–0 Research Articles DOI: 10.2110/jsr.2008.052 DEPOSITS FROM WAVE-INFLUENCED TURBIDITY CURRENTS: PENNSYLVANIAN MINTURN FORMATION, COLORADO, U.S.A. 1 2 2 3 2 M. P. LAMB, P. M. MYROW, C. LUKENS, K. HOUCK, AND J. STRAUSS 1Department of Earth & Planetary Science, University of California, Berkeley, California 94720, U.S.A. 2Department of Geology, Colorado College, Colorado Springs, Colorado 80903, U.S.A. 3Department of Geography and Environmental Sciences, University of Colorado, Denver, Colorado, 80217-3363 U.S.A. e-mail: [email protected] ABSTRACT: Turbidity currents generated nearshore have been suggested to be the source of some sandy marine event beds, but in most cases the evidence is circumstantial. Such flows must commonly travel through a field of oscillatory flow caused by wind-generated waves; little is known, however, about the interactions between waves and turbidity currents. We explore these interactions through detailed process-oriented sedimentological analysis of sandstone event beds from the Pennsylvanian Minturn Formation in north-central Colorado, U.S.A. The Minturn Formation exhibits a complex stratigraphic architecture of fan-delta deposits that developed in association with high topographic relief in a tectonically active setting. An , 20–35-m- thick, unconformity-bounded unit of prodelta deposits consists of dark green shale and turbidite-like sandstone beds with tool marks produced by abundant plant debris. Some of the sandstone event beds, most abundant at distal localities, contain reverse- to-normal grading and sequences of sedimentary structures that indicate deposition from waxing to waning flows. In contrast, proximal deposits, in some cases less than a kilometer away, contain abundant beds with evidence for deposition by wave- dominated combined flows, including large-scale hummocky cross-stratification (HCS). -
Figure 12B-01. Mountainous Volcanic Region
108°W 106°W F Ancestral ron t Rang LARIMER Uinta Sand Upl e ift Little Snake River Wash Ba North Platte River MOFFAT s Yampa River in JACKSON Park-Gore Range Axial ROUTT Ba s in Up li h ft rc as A ek e Dougl Cr White River GRAND 40°N Whi EXPLANATION RIO BLANCO 40°N te Ri Neogene Volcanics ver Upli Neogene Sediments ft Paleogene Volcanics Eagle River Blue River Paleocene-Cretaceous Intrusives Piceance Basin Roaring ForkCentral River Colorado TroughEAGLE Cretaceous Seaway Sediment GARFIELD Eagle River Sawatch Range Aquifers SUMMIT Mesozoic Sediment Aquifers Ancestral Rockies Basins Colorado River Precambrian Basement PITKIN Arkansas River East Muddy Creek Mountainous Region MESA LAKE PARK Unc Mountainous Valleys ompa ghre Up Colorado Plateaus Region lif DELTA t Laramide Basin Outlines Laramide Uplift Axis Uncompaghre Uplift G un Taylor River CHAFFEE nison Laramide Basin Axis GUNNISON Upl Ancestral Rockies Uplift Axis Uncompahgre River South Arkansas River ift Ancestral Rockies Basin Axis Paradox Basin FREMONT MONTROSE San Lui CUSTER s OURAY Up San Miguel River li ft 38°N SAN MIGUEL SAGUACHE 38°N Animas River HINSDALE DOLORES SAN JUAN Rio Grande MINERAL ag Dolores River n S West Dolores River ua J RIO GRANDE ALAMOSA e San MONTEZUMA n Dom Jua Archuleta Anticlinorium San Los Pinos River LA PLATA COSTILLA San Juan Piedra River Basin CONEJOS Tusas Uplift COSTILLA ARCHULETA COSTILLA 108°W 106°W 0 10 20 30 40 50 Miles Geology modified from Tweto (1979); structural features from Hemborg (1996). 0 10 20 30 40 50 Kilometers Figure 12b-01. -
Historical Range of Variability and Current Landscape Condition Analysis: South Central Highlands Section, Southwestern Colorado & Northwestern New Mexico
Historical Range of Variability and Current Landscape Condition Analysis: South Central Highlands Section, Southwestern Colorado & Northwestern New Mexico William H. Romme, M. Lisa Floyd, David Hanna with contributions by Elisabeth J. Bartlett, Michele Crist, Dan Green, Henri D. Grissino-Mayer, J. Page Lindsey, Kevin McGarigal, & Jeffery S.Redders Produced by the Colorado Forest Restoration Institute at Colorado State University, and Region 2 of the U.S. Forest Service May 12, 2009 Table of Contents EXECUTIVE SUMMARY … p 5 AUTHORS’ AFFILIATIONS … p 16 ACKNOWLEDGEMENTS … p 16 CHAPTER I. INTRODUCTION A. Objectives and Organization of This Report … p 17 B. Overview of Physical Geography and Vegetation … p 19 C. Climate Variability in Space and Time … p 21 1. Geographic Patterns in Climate 2. Long-Term Variability in Climate D. Reference Conditions: Concept and Application … p 25 1. Historical Range of Variability (HRV) Concept 2. The Reference Period for this Analysis 3. Human Residents and Influences during the Reference Period E. Overview of Integrated Ecosystem Management … p 30 F. Literature Cited … p 34 CHAPTER II. PONDEROSA PINE FORESTS A. Vegetation Structure and Composition … p 39 B. Reference Conditions … p 40 1. Reference Period Fire Regimes 2. Other agents of disturbance 3. Pre-1870 stand structures C. Legacies of Euro-American Settlement and Current Conditions … p 67 1. Logging (“High-Grading”) in the Late 1800s and Early 1900s 2. Excessive Livestock Grazing in the Late 1800s and Early 1900s 3. Fire Exclusion Since the Late 1800s 4. Interactions: Logging, Grazing, Fire, Climate, and the Forests of Today D. Summary … p 83 E. Literature Cited … p 84 CHAPTER III. -
Pleistocene Drainage Changes in Uncompahgre Plateau-Grand
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/32 Pleistocene drainage changes in Uncompahgre Plateau-Grand Valley region of western Colorado, including formation and abandonment of Unaweep Canyon: a hypothesis Scott Sinnock, 1981, pp. 127-136 in: Western Slope (Western Colorado), Epis, R. C.; Callender, J. F.; [eds.], New Mexico Geological Society 32nd Annual Fall Field Conference Guidebook, 337 p. This is one of many related papers that were included in the 1981 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Packet, and Kailey Rosema, Our Water Quality Coordinator, Will Present on This Topic As Part of the Operations Report in April
MEMORANDUM TO: Board of Directors FROM: Catherine Hayes, Board Secretary DATE: April 18, 2019 RE: April 25, 2019, Regular Board Meeting This memorandum shall serve as notice of the Regular Board of Directors Meeting of the Eagle River Water & Sanitation District: Thursday, April 25, 2019 11:30 a.m. Eagle River Water & Sanitation District Office Walter Kirch Room 846 Forest Road Vail, CO 81657 Cc public items: Board Materials via Email: ERWSD Managers Bob Armour, Vail resident Ken Marchetti, Marchetti & Weaver, PC Caroline Bradford, Independent Consultant Robert Lipnick, Vail resident Rick Sackbauer, Vail resident BOARD OF DIRECTORS REGULAR MEETING April 25, 2019, 11:30 a.m. 1. Consultant/Guest Introduction 2. Public Comment• 3. Action Items 3.1. Meeting Minutes of March 28, 2019, Special Meeting☼ 3.2. Meeting Minutes of March 28, 2019, Joint Meeting with UERWA☼ 3.3. Resolution Consenting to Overlapping Boundaries – Jim Collins☼ 3.4. Resolution re Bighorn Terrace Sanitation Subdistrict Budget – James Wilkins☼ 3.5. Consent Agenda: Contract Log☼ 4. Strategy Items 4.1. Board Member Input 5. General Manager Report – Linn Brooks* 5.1. General Manager Information Items 5.1.1. Recruiting.com Video – Ali Kelkenberg and Amy Vogt 5.1.2. Climate Action Collaborative 2018 Annual Report* 5.1.3. Stillwater Update – James Wilkins 5.2. Operations Report* 5.2.1. Lead and Copper Sampling – Kailey Rosema* 5.3. Engineering Report – Jason Cowles* 5.3.1. Eagle Park Reservoir Comprehensive Dam Safety Evaluation* 5.4. Public Affairs Report – Diane Johnson* 5.5. Monthly Reports 5.5.1. Development Report* 5.5.2. Authority March Meeting Summary – draft* 5.5.3. -
Primitive Areas Gore Range-Eagles Nest And
OC1 LO STUDIES RELATED TO WILDERNESS PRIMITIVE AREAS OHIO GEOLOGICAL SURVEt OCT 2 r iQ70 GORE RANGE-EAGLES NEST AND VICINITY, COLORADO GEOLOGICAL SURVEY BULLETIN 1319-C f* MINERAL RESOURCES of the GORE RANGE-EAGLES NEST PRIMITIVE AREA and VICINITY, COLORADO Crest of Gore Range and head of middle fork of Black Creek. View is westward. Mount Powell (alt 13,534 ft) is massive peak at right of cen ter. Eagles Nest Mountain is at far right. Duck Lake is in right foreground. Trough above right end of lake marks fault zone of north-northwest trend. Dark area on steep front of rock glacier at left in photograph is typical "wet front" suggesting ice core in rock glacier. Mineral Resources of the Gore Range-Eagles Nest Primitive Area and Vicinity, Summit and Eagle Counties, Colorado By OGDEN TWETO and BRUCE BRYANT, U.S. GEOLOGICAL SURVEY, and by FRANK E. WILLIAMS, U.S. BUREAU OF MINES c STUDIES RELATED TO WILDERNESS PRIMITIVE AREAS GEOLOGICAL SURVEY BULLETIN 1319-C An evaluation of the mineral potential of the area UNITED STATES GOVERNMENT PRINTING OFFICE. WASHINGTON : 1970 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 78-607129 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 ^. STUDIES RELATED TO WILDERNESS PRIMITIVE AREAS The Wilderness Act (Public Law 88-577, Sept. 3, 1964) and the Conference Report on Senate bill 4, 88th Congress, direct the U.S. Geological Survey and the U.S. Bureau of Mines to make mineral surveys of wilderness and primitive areas. -
Stratigraphic Correlation Chart for Western Colorado and Northwestern New Mexico
New Mexico Geological Society Guidebook, 32nd Field Conference, Western Slope Colorado, 1981 75 STRATIGRAPHIC CORRELATION CHART FOR WESTERN COLORADO AND NORTHWESTERN NEW MEXICO M. E. MacLACHLAN U.S. Geological Survey Denver, Colorado 80225 INTRODUCTION De Chelly Sandstone (or De Chelly Sandstone Member of the The stratigraphic nomenclature applied in various parts of west- Cutler Formation) of the west side of the basin is thought to ern Colorado, northwestern New Mexico, and a small part of east- correlate with the Glorieta Sandstone of the south side of the central Utah is summarized in the accompanying chart (fig. 1). The basin. locations of the areas, indicated by letters, are shown on the index map (fig. 2). Sources of information used in compiling the chart are Cols. B.-C. shown by numbers in brackets beneath the headings for the col- Age determinations on the Hinsdale Formation in parts of the umns. The numbers are keyed to references in an accompanying volcanic field range from 4.7 to 23.4 m.y. on basalts and 4.8 to list. Ages where known are shown by numbers in parentheses in 22.4 m.y. on rhyolites (Lipman, 1975, p. 6, p. 90-100). millions of years after the rock name or in parentheses on the line The early intermediate-composition volcanics and related rocks separating two chronostratigraphic units. include several named units of limited areal extent, but of simi- No Quaternary rocks nor small igneous bodies, such as dikes, lar age and petrology—the West Elk Breccia at Powderhorn; the have been included on this chart. -
Dinosaur National Monument, Usa
Fire Ecology Volume 8, Issue 2, 2012 Sherrill and Romme: Spatial Variation in Postfire Cheatgrass doi: 10.4996/fireecology.0802038 Page 38 RESEARCH ARTICLE SPATIAL VARIATION IN POSTFIRE CHEATGRASS: DINOSAUR NATIONAL MONUMENT, USA Kirk R. Sherrill1* and William H. Romme2 1National Park Service, Natural Resource Stewardship and Science, Inventory and Monitoring Program, 1201 Oakridge Drive, Fort Collins, Colorado 80525, USA 2Natural Resource Ecology Laboratory, Colorado State University, 1231 East Drive, Fort Collins, Colorado 80523-1499, USA *Corresponding author: Tel.: 001-970-267-2166; e-mail: [email protected] ABSTRACT A major environmental problem in semi-arid landscapes of western North America is the invasion of native vegetation by cheatgrass (Bromus tectorum L.), an annual Eurasian grass that covers >40 million ha of range and woodland in the western US. Cheatgrass can be especially problematic after fire—either prescribed fire or wildfire. Although cheatgrass is known to generally thrive in regions of moderate temperatures, dry sum- mers, and reliable winter precipitation, the spatial patterns of postfire cheatgrass invasion are not well characterized at finer spatial scales (e.g., within most individual landscapes). We used boosted regression trees to develop a spatial model of cheatgrass abundance 0 yr to 19 yr postfire in an 8000 km2 semiarid landscape centered on Dinosaur National Monu- ment (Colorado and Utah, USA). Elevation, a deterministic variable, was the strongest single predictor, with higher cheatgrass cover occurring below 1600 meters. Two other contingent variables, fire severity and climatic conditions in the year after the fire, -in creased the model’s predictive power. The influence of fire severity differed with the scale of analysis. -
2018 Open Lands Plan Update a Plan for Open Space, Trails and the Use of Town Lands
2018 OPEN LANDS PLAN UPDATE A PLAN FOR OPEN SPACE, TRAILS AND THE USE OF TOWN LANDS An element of the Vail Comprehensive Plan Adopted on October 16th, 2018 Resolution #37, Series 2018 TOWN COUNCIL Dave Chapin, Mayor Kim Langmaid Jenn Bruno, Mayor Protem Jen Mason Dick Cleveland Greg Moffet Kevin Foley Travis Coggin PLANNING AND ENVIRONMENTAL COMMISSION John Rediker Brian Gillette Ludwig Kurz Karen Marie Perez Brian Stockmar John Ryan Lockman Pam Hopkins Rollie Kjesbo TOWN OF VAIL STAFF George Ruther Director of Community Development ACKNOWLEDGEMENTS Kristen Bertuglia Environmental Sustainability Manager Chris Neubecker Planning Manager Matt Panfil Planner Mark Hoblitzell Environmental Sustainability Coordinator Peter Wadden Water Quality Education Coordinator Gregg Barrie Landscape Architect Greg Hall Director of Public Works and Transportation Sean Koenig GIS Coordinator Suzanne Silverthorn Director of Communications BRAUN ASSOCIATES, INC. Tom Braun Tim Halbakken Nick Braun SE GROUP Gabby Voeller Scott Prior 2018 Open Lands Plan Update TABLE OF CONTENTS EXECUTIVE SUMMARY - Other Trail Improvements - Trail Types and Standards - Regional Context of Vail’s Trails - Process for Evaluation of Trail Ideas NTRODUCTION 1. I 1 - Easements From Private Land Owners - Need to Update the 1994 Open Lands Plan - Goals for Updating the 1994 Plan 5. ACTION PLAN 44 - Approach to this Update Process - 2018 Action Plan - Community Involvement - Organization of this Plan 6. IMPLEMENTATION 53 - Environmentally Sensitive Lands 2. ENVIRONMENTALLY SENSITIVE LANDS 6 - Public Facilities and Community Needs/Use and - Community Input Management of Town Lands - Environmentally Sensitive Lands - Recreational Trails - Evaluation of Undeveloped Privately-Owned Lands - Conclusion - Protection of Environmentally Sensitive Lands - Designated Open Space Lands 7.