National Monument

Total Page:16

File Type:pdf, Size:1020Kb

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. 130 million years ago. formed by the Green and Yampa Rivers. The Yampa has also been active in canyon The National Park Service has recently Many remains of prehistoric Indian in­ Within its boundaries also is the Nation's carving. This river, rising in the Rabbit initiated a project to outline in high relief habitants are found in this area. Evidence richest deposit of dinosaur fossils. Here is Ears Range of northwestern Colorado, first some of the huge dinosaur bones in the up- of the earliest Indians was discovered at Head of Lodore Canyon Boating on the Yampa Steamboat Rock at Junction of Green and Yampa Rivers the rare opportunity to see these remains cut into relatively soft rock. Through a tilted fossil-bearing layer. A permanent Hell's Midden, in Castle Park where scien­ in place. The monument contains nearly long period of erosion its course was estab­ museum building will be constructed to en­ tists excavated a 17-foot refuse deposit. The 191,000 acres of Federal lands. lished in a series of bends or meanders. close this display. Already several partial lowest layers of this deposit showed that the The name "dinosaur" means "terrible Gradually, the soft rocks were worn away skeletons of dinosaurs have been exposed. earliest Indians did not practice agriculture, these excavations. Somewhat later pottery this early party crossed the Green River is slopes of the higher mountainsides. The formation about boating or for an appli­ lizard," an apt term to describe these pre­ and with uplift of the region the river en­ You are invited to observe these and to wit­ but lived solely by hunting and gathering was used. About this time these early In­ located along the headquarters approach road commoner varieties of wildflowers here are cation for a boating permit, please contact historic reptiles which have vanished from trenched its meanders into the underlying, ness reliefing operations. wild food plants, about 1500 to 500 B. C. dians moved into cave shelters where they near the monument boundary. sunflowers, goldenrod, sage-lily, evening- the superintendent's office at Vernal, Utah. the earth. There were many kinds, some more resistant strata. The resulting gorge, Dinosaur bones were first discovered here Sometime during the first few hundred lived, slept, and cooked their meals. They primrose, and bee flower. being of tremendous size. in a high plateau lying southeast of the in 1909 by Earl Douglass of the Carnegie years after Christ, agriculture was introduced never quite achieved the art of building per­ Eauna and Flora Dow To Get There Uinta Range, is not as deep as the canyons Museum. Fossils were removed by the mu­ in the area, for the remains of corncobs, manent house structures, for the caves sup­ of the Green but is equally impressive. River Boating The Canyon Country seum from 1909 to 1922. Quarrying was beans, and pumpkins have been found in plied the shelter they needed, and much of As in other areas of the National Park Monument headquarters and the Dinosaur Below the confluence with the Yampa, the their life was spent out-of-doors, tending System, the monument is a refuge for all Boating has become a popular and ad­ Quarry are reached by U. S. 40. The head­ Green River flows through Echo Park (Pats Through centuries of erosive action the their crops, hunting, and fishing. Sometime wildlife. Deer are common throughout the venturous way of enjoying the canyon won­ quarters-quarry area is open all year, but the Hole), a lonely valley where a hermit, Pat Green and Yampa Rivers have been fash­ Reliefing operation at the Dinosaur Quarry between A. D. 900 and 1000 the inhabitants monument, and bighorn (mountain sheep) ders. Trips of 1 to 6 days duration are roads to the scenic canyon country generally Lynch, lived for years. It swirls and plunges ioning their spectacular canyons. of this region moved away; for what reasons are occasionally seen. Coyotes and bobcats offered by competent guides at reasonable are closed by snow from October 15 to past Harpers Corner, through Whirlpool Tilted rock layers of the Uinta Mountains, we do not know. are common, but the wary mountain lion is rates. May 15. Canyon, Island Park, and Split Mountain representing millions of years of geologic rare. Beaver, while not numerous, are The rivers are swift and turbulent in The monument cannot be reached by Gorge, and then slows to a more leisurely time, have been cut by the Green, the largest Escalante increasing. places. Skill in boating and knowledge of railway. Bus and airplane services are pace as it leaves the monument. tributary of the Colorado. Between the If you drive over Blue Mountain Plateau the streams are needed to traverse them available to Vernal, Utah, 20 miles west of 2,000-foot vertical walls of the Canyon of In 1776, a Spanish party of 10 men, led by from Harpers Corner or Pats Hole late in safely. Boating is not encouraged without headquarters, but there is no regularly Lodore the Green flows toward its junction The Dinosaur Quarry the Franciscan priest Escalante, camped for 3 the evening, you may observe deer, badger, a competent guide. scheduled transportation from there to the with the Yampa at Steamboat Rock, a great days on the banks of the Green River within porcupine, jack rabbit, cottontail, and the Ordinary rowboats, outboard motorboats, monument. monolith resembling the prow of a ship. The name of the monument is somewhat view of Split Mountain and the southwestern sage hen. Prairie dogs may be seen along foldboats, and canoes are not considered safe In 1869, Maj. J. W. Powell, famous pioneer misleading, for fossil dinosaur bones occur section of the monument. the road to Split Mountain Gorge. Golden- for running the rapids of the Green and Accommodations explorer, made a river trip between these in rocks which outcrop only in the southwest Not only did Escalante describe this region mantled ground squirrels and whiptail liz­ Yampa Rivers. Specially designed wooden Lodging is not available in the monument. in his journal, but Niera, his captain, pre­ ards are numerous near headquarters. and metal boats are used successfully by The nearest overnight accommodations are pared a map on which a portion of what is The plateaus adjacent to the canyons are some guides, but the most popular and per­ in Vernal, Utah. now Dinosaur National Monument is shown. typical examples of semidesert country, with haps the safest boats used by guides and The National Park System, of which this area is a unit, is dedicated to conserving the On this map, published in Spain in 1778, the greasewood, pinyon, junipers, and sage­ amateurs alike are the 7- and 10-man U. S. Back-country Travel scenic, scientific, and historic heritage of the United States for the benefit and enjoyment Green River appears as the Rio S. Buena­ brush growing in profusion. Stands of Navy rubber landing craft. of its people. ventura, and Split Mountain as Sierra aspen, Douglas-fir, ponderosa pine, and The boating season is normally from The back country is reached by unim­ Mineral. A stone marker at the site where mountain-mahogany grow on protected May 1 to September 1. For additional in­ proved dirt roads branching northward from U. S. 40. Those who wish to go there is located in both Colorado and Utah; hence, should first make inquiry at headquarters. a license is required from the State in which Cars should be equipped with spare tire, you wish to fish. jack, chains, shovel, ax, extra water for the radiator, and a full tank of gasoline. Pack Trips ROAD MAP Roads and Trails Regularly established guide services and pack trips are not provided, but you may DINOSAUR All areas numbered on the map can be arrange horseback trips from Island Park to reached by jeep or truck, except Jones Hole Jones Hole. DINOSAUR NATIONAL MONUMENT (9) which can be reached by a 7-mile foot UTAH -COLORADO or horse trail from Island Park Ranch (8), Let's Keep Dinosaur Unspoiled or by boat from Pats Hole (5).
Recommended publications
  • 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.
    [Show full text]
  • 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).
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Potential Petroleum Resources of Northeastern Utah and Northwestern Colorado Albert F
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/32 Potential petroleum resources of northeastern Utah and northwestern Colorado Albert F. Sanborn, 1981, pp. 255-266 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.
    [Show full text]
  • THE HISTORY of a PORTION of Yal\Ipa RIVER, COLORADO, and ITS POSSIBLE BEARING on THAT of GREEN RIVER
    THE HISTORY OF A PORTION OF YAl\iPA RIVER, COLORADO, AND ITS POSSIBLE BEARING ON THAT OF GREEN RIVER. By E. T. HANCOCK. Few regions offer more interesting geologic problems relating to drainage than the Uinta Mountains, in Utah and Colorado, and the ar3a immediately east of them. In fact, the writer's attention was primarily attracted to this field by the diversity of opinion regarding the ante­ cedent origin of Green River. Although the present paper deals mainly with that portion of Yampa River 2ast of Juniper Mountain, the conclusions reached are believed to have a definite bearing on the Green River problem itself. The paper is introduced by a brief discussion of the structural features of the region east of the Uinta Mountains, for a clear understanding of the relation of the minor uplifts to the great Uinta fold will better enable the reader to appreciate the possible bearing which the writer's conclusions may have in the solution of that problem. The main range of the Uinta Mountain::; is a broad, .flat-topped anticline, which has an easterly trend and a length of over 150 miles and which separates the Green River Basin on the north from the Uinta Basin on the south. The conspicuous portion of the Uinta fold terminates in northwestern Colorado, but along the continuation of its axis to the east lies a long, gentle anticline which reaches the foothills of the Park Range. This anticline was called by ·White 1 "the inceptive portion of the Uinta fold." The axis of the anticline is coincident with the low, broad valley known as Axial Basin, and in a recent report Gale 2 refers to it as .
    [Show full text]
  • The Abundance, Migration and Management of Mule Deer in Dinosaur National Monument
    Utah State University DigitalCommons@USU All Graduate Theses and Dissertations Graduate Studies 5-1968 The Abundance, Migration and Management of Mule Deer in Dinosaur National Monument Robert W. Franzen Utah State University Follow this and additional works at: https://digitalcommons.usu.edu/etd Part of the Other Life Sciences Commons Recommended Citation Franzen, Robert W., "The Abundance, Migration and Management of Mule Deer in Dinosaur National Monument" (1968). All Graduate Theses and Dissertations. 1685. https://digitalcommons.usu.edu/etd/1685 This Thesis is brought to you for free and open access by the Graduate Studies at DigitalCommons@USU. It has been accepted for inclusion in All Graduate Theses and Dissertations by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. THE ABUNDANCE, MIGRATION AND MANAGEMENT OF MULE DEER IN DINOSAUR NATIONAL MONUMENT by Robert W. Franzen A thesi.s submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in Wildlife Biology Approve. d~ {\failA' Professor "'ead of Deoartment Dean ~ Graduate Studies UTAH STATE UNIVERSITY Logan, Utah 1968 ii ACKNOWLEDGMENTS I wish to express my sincere app-reciation to Dr. Jessop B•. Low, Leader, Utah Cooperative Wildlife Research Unit, for his guidance, encouragement, and constructive criticism throughout the study period. I am grateful to the National Park Service for providing housing and many items necessary during the study. The invaluable cooperation received from the Monument staff will long be remembered. The assistance given by ranger Larry Hanneman is particularly appreciated. I also would like to thank Dr. Jim B. Grumbles for his interest and suggestions concerning the vegetation analysis methods used.
    [Show full text]
  • Constraining the Timing of River Incision in the Upper Colorado Drainage Basin Using Apatite (U-Th)/He Thermochronology in the Elk Mountains, Western Colorado
    Constraining the Timing of River Incision in the Upper Colorado Drainage Basin Using Apatite (U-Th)/He Thermochronology in the Elk Mountains, Western Colorado Coleman Hiett Department of Geological Sciences University of Colorado, Boulder Departmental Honors Thesis April 10, 2017 Thesis Advisor: Lon Abbott, Department of Geological Sciences Defense Committee Members: Charles Stern, Department of Geological Sciences Lisa Barlow, Baker Residential Academic Program ABSTRACT This study utilizes apatite (U-Th)/He, or AHe, to produce a vertical transect of cooling histories along the height of the partially exhumed Crystal Pluton in the Elk Mountains of west/central Colorado. These cooling histories are interpreted to reflect exhumation controlled by the incision of the Crystal River – a tributary of the Colorado River. A period of rapid exhumation is observed from 8 – 11 Ma, likely beginning earlier, that is consistent with previous AHe data taken from nearby exhumed plutons in the Elk and northern West Elk Mountains. This period of exhumation predates the incision of a low relief surface that developed in northwestern Colorado by ca. 10 Ma, and is therefore not believed to have been controlled by the incision of the Colorado River. A review of previously noted incision constraints suggests that post-10 Ma Colorado River incision has become more rapid in the last 1 – 3 Ma, suggesting that climate change, rather than epeirogenic uplift, is the major driver for recent river incision. 1. INTRODUCTION 1.1 Concerns of the Colorado River For more than a century, geologists have struggled to better understand the geologic evolution of the western United States.
    [Show full text]
  • Geochemical and Geochronological Characterization of Grand Mesa Volcanic Field, Western Colorado R
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/68 Geochemical and geochronological characterization of Grand Mesa Volcanic Field, western Colorado R. Cole, A. Stork, W. Hood, and M. Heizler, 2017, pp. 103-113 in: The Geology of the Ouray-Silverton Area, Karlstrom, Karl E.; Gonzales, David A.; Zimmerer, Matthew J.; Heizler, Matthew; Ulmer-Scholle, Dana S., New Mexico Geological Society 68th Annual Fall Field Conference Guidebook, 219 p. This is one of many related papers that were included in the 2017 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.
    [Show full text]
  • Stratigraphic Correlations Between the Eagle Valley Evaporite and Minturn Formation, Eagle Basin, Northwest Colorado
    Stratigraphic Correlations Between the Eagle Valley Evaporite and Minturn Formation, Eagle Basin, Northwest Colorado U.S. GEOLOGICAL SURVEY BULLETIN 1787-GG AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with the last offerings, are given in the current-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Survey publications released prior to the current year are listed in the most recent annual "Price and Availability List." Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated monthly, which is for sale in microfiche from the U.S. Geological Survey Books and Open-File Reports Sales, Box 25286, Denver, CO 80225. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Tech­ Books of the U.S. Geological Survey are available over the niques of Water-Resources Investigations, Circulars, publications counter at the following U.S. Geological Survey offices, all of of general interest (such as leaflets, pamphlets, booklets), single which are authorized agents of the Superintendent of Documents. copies of periodicals (Earthquakes & Volcanoes, Preliminary De­ termination of Epicenters), and some miscellaneous reports, includ­ ANCHORAGE, Alaska-4230 University Dr., Rm.
    [Show full text]
  • Climate of Colorado
    Climate of Colorado Climatography of the United States No. 60 (updated 1/2003) Prepared by Nolan J. Doesken, Roger A. Pielke, Sr., and Odilia A.P. Bliss Colorado Climate Center, Atmospheric Science Department, Colorado State University, Fort Collins, CO TOPOGRAPHIC FEATURES To understand the regional and local climates of Colorado, you must begin with a basic knowledge of Colorado’s topography. Colorado lies astride the highest mountains of the Continental Divide. Nearly rectangular, its north and south boundaries are the 41° and 37° N. parallels, and the east and went boundaries are the 102° and 109° W. meridians. It is eighth in size among the 50 states, with an area of over 104,000 square miles. Although known for its mountains, nearly 40 percent of its area is taken up by the eastern high plains. Of particular importance to the climate are Colorado’s interior continental location in the middle latitudes, the high elevation of the entire region, and the mountains and ranges extending north and south approximately through the middle of the State. With an average altitude of about 6,800 feet above sea level, Colorado is the highest contiguous State in the Union. Roughly three- quarters of the Nation’s land above 10,000 feet altitude lies within its borders. The State has 59 mountains 14,000 feet or higher, and about 830 mountains between 11,000 and 14,000 feet in elevation. Emerging gradually from the plains of Kansas and Nebraska, the high plains of Colorado slope gently upward for a distance of some 200 miles from the eastern border to the base of the foothills of the Rocky Mountains.
    [Show full text]