Bent's Old Fort National Historic Site Geologic Resource
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A Revised Taxonomy of the Iguanodont Dinosaur Genera and Species
ARTICLE IN PRESS + MODEL Cretaceous Research xx (2007) 1e25 www.elsevier.com/locate/CretRes A revised taxonomy of the iguanodont dinosaur genera and species Gregory S. Paul 3109 North Calvert Station, Side Apartment, Baltimore, MD 21218-3807, USA Received 20 April 2006; accepted in revised form 27 April 2007 Abstract Criteria for designating dinosaur genera are inconsistent; some very similar species are highly split at the generic level, other anatomically disparate species are united at the same rank. Since the mid-1800s the classic genus Iguanodon has become a taxonomic grab-bag containing species spanning most of the Early Cretaceous of the northern hemisphere. Recently the genus was radically redesignated when the type was shifted from nondiagnostic English Valanginian teeth to a complete skull and skeleton of the heavily built, semi-quadrupedal I. bernissartensis from much younger Belgian sediments, even though the latter is very different in form from the gracile skeletal remains described by Mantell. Currently, iguanodont remains from Europe are usually assigned to either robust I. bernissartensis or gracile I. atherfieldensis, regardless of lo- cation or stage. A stratigraphic analysis is combined with a character census that shows the European iguanodonts are markedly more morpho- logically divergent than other dinosaur genera, and some appear phylogenetically more derived than others. Two new genera and a new species have been or are named for the gracile iguanodonts of the Wealden Supergroup; strongly bipedal Mantellisaurus atherfieldensis Paul (2006. Turning the old into the new: a separate genus for the gracile iguanodont from the Wealden of England. In: Carpenter, K. (Ed.), Horns and Beaks: Ceratopsian and Ornithopod Dinosaurs. -
SPIDER in the RIVER: a COMPARATIVE ENVIRONMENTAL HISTORY of the IMPACT of the CACHE LA POUDRE WATERSHED on CHEYENNES and EURO- AMERICANS, 1830-1880 John J
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations, Theses, & Student Research, History, Department of Department of History Spring 4-21-2015 SPIDER IN THE RIVER: A COMPARATIVE ENVIRONMENTAL HISTORY OF THE IMPACT OF THE CACHE LA POUDRE WATERSHED ON CHEYENNES AND EURO- AMERICANS, 1830-1880 John J. Buchkoski University of Nebraska-Lincoln Follow this and additional works at: http://digitalcommons.unl.edu/historydiss Part of the Cultural History Commons, and the United States History Commons Buchkoski, John J., "SPIDER IN THE RIVER: A COMPARATIVE ENVIRONMENTAL HISTORY OF THE IMPACT OF THE CACHE LA POUDRE WATERSHED ON CHEYENNES AND EURO-AMERICANS, 1830-1880" (2015). Dissertations, Theses, & Student Research, Department of History. 83. http://digitalcommons.unl.edu/historydiss/83 This Article is brought to you for free and open access by the History, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations, Theses, & Student Research, Department of History by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. SPIDER IN THE RIVER: A COMPARATIVE ENVIRONMENTAL HISTORY OF THE IMPACT OF THE CACHE LA POUDRE WATERSHED ON CHEYENNES AND EURO-AMERICANS, 1830-1880 By John J. Buchkoski A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For the Degree of Master of Arts Major: History Under the Supervision of Professor Katrina L. Jagodinsky Lincoln, Nebraska April, 2015 SPIDER IN THE RIVER: A COMPARATIVE ENVIRONMENTAL HISTORY OF THE IMPACT OF THE CACHE LA POUDRE WATERSHED ON CHEYENNES AND EURO-AMERICANS, 1830-1880 John Buchkoski, M.A. -
Sedimentology of Mesa Rica Sandstone in Tucumcari Basin, New Mexico
Circular 157 1977 Sedimentology of Mesa Rica Sandstone in Tucumcari Basin, New Mexico by J. E. Gage and G. B. Asquith New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY documenting New Mexico mineral resources since 1927 Circular 157 New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY Sedimentology of Mesa Rica Sandstone in Tucumcari Basin, New Mexico by J. E. Gage and G. B. Asquith SOCORRO 1977 11 Published by Authority of State of New Mexico, NMSA 1953 Sec. 63-1-4 Printed by University of New Mexico Printing Plant, June 1977 Available from New Mexico Bureau of Mines & Mineral Resources, Socorro, NM 87801 Price $2.50 Contents iv 5 Abstract The Mesa Rica Sandstone (Lower Cretaceous) in the Tucumcari Basin of east-central New Mexico represents deposits from a lobate sand-rich delta complex. Log-probability curves of the grain-size distributions when compared to the work of Visher (1969) indicate environments ranging from distributary channels to marine wave deposits. The Mesa Rica delta prograded into the marine Tucumcari Basin from the north as shown by the south-trending to southwest-trending paleocurrent directions, and the decrease in mean grain size and thickness to the southeast, south, and southwest (lobate geometry). Also, a decrease in percent cross stratification to the southeast, south, and southwest (accompanied by an increase in percent bioturbation and burrowing) indicates a transition from predominantly fluvial to predominantly marine conditions. If the Mesa Rica Sandstone is correlative with the lower fluvial interval of the Dakota Sandstone north and northwest of the Tucumcari Basin as suggested by Scott (1970), then the Dakota Sandstone represents the fluvial facies of the Mesa Rica marine delta complex. -
Geohydrology of the Oklahoma Panhandle Beaver, Cimarron And
GEOHYDROLOGY OF THE OKLAHOMA PANHANDLE, BEAVER, CIMARRON, AND TEXAS COUNTIES By D. l. Hart Jr., G. l. Hoffman, and R. L. Goemaat U. S. GEOLOGICAL SURVEY Water Resources Investigation 25 -75 Prepared in cooperation with OKLAHOMA WATER RESOURCES BOARD April 1976 UNITED STATES DEPARTMENT OF THE INTERIOR Thomas Kleppe, Secretary GEOLOGICAL SURVEY v. E. McKelvey, Director For additional information write to~ U.S. Geological Survey Water Resources Division 201 N. W. 3rd Street, Room 621 Oklahoma City, Oklahoma 73102 ii CONTENTS Pa,;e No. Factors to convert English units to metric units ..•..................... v Ab s t raet .. .. .. .. .. .. .. .. .. .. .. I' of '" " " of .. .. ••• .. of " •, '" 7 I ntroduc t ion. ......•....•............................................... 8 Purpose and scope of investigation 8 Location and general features of the area.••..........•............ 8 Previous investigations .•.......................................... 10 Well-numbering system.•...............................•............ 10 Acknowledgments. .......•......................................... .. 13 Geology. ....•.•....................................................... .. 13 ~ Regional geology ill .. II II II oil II oil It It It "" oil 13 Geologic units and their water-bearing properties 16 Permian System...•.......................•.................... 16 Permian red beds undifferentiated...............•........ 16 Triassic System..•.•.........•...........•.................... 16 Dockt.JIn Group ~ 4 ~ #' ., of ,. '" ., # of ,. ,. .. ". 16 Jurassic -
The Environmental History of Sand Creek Massacre National Historic Site
CENTER FOR PUBLIC HISTORY AND ARCHAEOLOGY COLORADO STATE UNIVERSITY The Environmental History of Sand Creek Massacre National Historic Site Final Draft Elizabeth Michell July 31 2009 An abbreviated version intended as guide for visitors OYL/iJ INTRODUCTION On late spring day visitor stands on slight rise on the banks of Big Sandy Creek from where across Cheyenne chief Black Kettles village once stood whole lot of he nothing comments laconically It is quiet place its peacefulness giving it timeless But quality the visitor is wrong and the timelessness is deceptive You can never visit the past again The Sand Creek Massacre National Historic Site is in southeastern fifteen Colorado about miles northeast of the small town of Eads This is high plains country dusty and flat the drab greens of grass and scrub melding into the relentless browns of desiccated vegetation sand and soil The surrounding landscape is crisscrossed dirt by trails and fence lines dotted with windmills outbuildings and stock watering tanks At the site groves of cottonwoods tower along the gently sloping banks of Big Sandy Creek in fact it would be difficult to follow the stream course without the line of trees For most of the year water does not flow and the creek bed is choked with sand sagebrushes and other the site dry prairie species Though is part of shortgrass most of the land is prairie actually sandy bottomland that may eventually become It in Black Kettles tallgrass prairie was dry time and it is still dry evident by how much more sagebrush species there are now -
THE COLORADO MAGAZINE Published Bi-Monthly by the State Historical Society of Colorado
THE COLORADO MAGAZINE Published bi-monthly by The State Historical Society of Colorado Vol. XXlll Denver, Colorado, July, 1946 No.4 Prehistoric Peoples of Colorado 1 FRANK H. H. RoBERTS, JR.* Colorado is commonly regarded as one of the younger states in the Union, a state with a relatively short history. yet within its boundaries there is evidence to show that it was one of the earliest occupied areas in North America. In the closing days of the last Ice Age when the climate was cooler and more moist than that of today and when large glaciers still lingered in the nearby moun tains small groups of hunters roamed the plains east of the foothills, some even drifted westward into the San Luis Valley, following the herds of game upon which they relied for sustenance. These nomads were part of one of the first in a series of migrations from north eastern Asia that was to populate the New World with what, millenia later, Columbus mistakenly called Indians. 2 The most likely route of travel for the earliest of these movements was by way of the Bering Strait region. 3 During the last stage of the Pleisto cene the lowlands bordering Bering Sea and the Arctic Coast were not glaciated and following the climax of the period, although large portions of North America were still covered by remnants of the Wisconsin ice sheet, there was an open corridor along the eastern slopes of the Rocky Mountains. Consequently it was possible for men and animals to pass from Central Asia to Alaska, eastward to the Mackenzie River and thence southward into the Northern Plains. -
Devil's Backbone Management Plan Update
Devil’s Backbone Management Plan Update 1 2 Adoption of the Resource Management and Implementation Plan for Devil’s Backbone Open Space The Resource Management and Implementation Plan for Devil’s Backbone Open Space was recommended for adoption by the Larimer County Open Lands Advisory Board on January 22, 2015 and adopted by the Larimer County Manager and City of Fort Collins Manager. Linda Hoffmann, Larimer County Manager Date I I Darin Atteberry, Fort Collins City Manager Date 3 The Larimer County Natural Resources Department celebrated our 60th Anniversary in 2014. During this period, the help preserve open spaces sales tax was passed and one of the first open spaces we developed for public access was Devil’s Backbone Open Space. Today, approximately 70,000 people per year visit the Backbone to hike, mountain bike and horseback ride. Devil’s Backbone Open Space continues to be one of the most popular outdoor recreation areas near Loveland and we expect visitation to rise. Devil’s Backbone Open Space is popular because it provides something for everyone. The rock feature is a local icon and hundreds of students come from Larimer, Boulder and Weld counties to study the geology. The scenery and views from the open space are fantastic, whether you look west through the Keyhole feature or hike through Indian Creek valley. Wildlife is abundant and visitors are likely to see deer, golden eagles, songbirds, butterflies and flowering plants throughout the open space. Hikers rave about these natural features and mountain bikers love to ride the technical terrain through Laughing Horse Loop or the gentle sections along the north end of the Blue Sky Trail. -
Late Albian Kiowa-Skull Creek Marine Transgression, Lower Dakota Formation, Eastern Margin of Western Interior Seaway R.L
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Papers in Natural Resources Natural Resources, School of 2000 Late Albian Kiowa-Skull Creek Marine Transgression, Lower Dakota Formation, Eastern Margin of Western Interior Seaway R.L. Brenner Iowa Department of Natural Resources G.A. Ludvigson Iowa Department of Natural Resources B.J. Witzke Iowa Department of Natural Resources A.N. Zawistoski Indiana University E.P. Kvale Indiana University See next page for additional authors Follow this and additional works at: https://digitalcommons.unl.edu/natrespapers Part of the Natural Resources and Conservation Commons, Natural Resources Management and Policy Commons, and the Other Environmental Sciences Commons Brenner, R.L.; Ludvigson, G.A.; Witzke, B.J.; Zawistoski, A.N.; Kvale, E.P.; Ravn, R.L.; and Joeckel, R.M., "Late Albian Kiowa-Skull Creek Marine Transgression, Lower Dakota Formation, Eastern Margin of Western Interior Seaway" (2000). Papers in Natural Resources. 1009. https://digitalcommons.unl.edu/natrespapers/1009 This Article is brought to you for free and open access by the Natural Resources, School of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in Natural Resources by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors R.L. Brenner, G.A. Ludvigson, B.J. Witzke, A.N. Zawistoski, E.P. Kvale, R.L. Ravn, and R.M. Joeckel This article is available at DigitalCommons@University of Nebraska - Lincoln: https://digitalcommons.unl.edu/natrespapers/1009 LATE ALBIAN KIOWA±SKULL CREEK MARINE TRANSGRESSION, LOWER DAKOTA FORMATION, EASTERN MARGIN OF WESTERN INTERIOR SEAWAY, U.S.A. R.L. BRENNER1, G.A. -
Geologic Characterization 111 Date 7/31/91 List of Appendices
Characterization GEOLOGIC Prepared by ? TABLE OF CONTENTS Section Page 1.0 INTRODUCTION ....................................... 1 1.1 Purpose ........................................... 1 1.2 Scope of Characterization .............................. 1 1.2.1 Literature Search .... ........................... 1 1.2.2 Core Processing and Description ..................... 2 1.2.3 Reprocessing of Seismic Data ........................ 2 1.2.4 Grain Size Analysis .............................. 2 1.2.5 Geologic Report ................................ 3 1.3 Location and General Setting ...., ........................ 3 1.4 Previous Studies ...................................... 5 2.0 STRATIGRAPHY ....................................... 7 Precambrian ......................................... 2.1 7 2.2 Paleozoic And Mesozoic Sedimentary Section ................ 2.2.1 Fountain Formation (PennsylvanianPermian) ............ 7 2.2.2 Lyons Sandstone Formation (Permian) ................ 7 2.2.3 Lykins Formation (PermianrTriassic) ................. 10 2.2.4 Ralston Creek Formation (Jiurassic) .................. 10 2.2.5 Momson Formation (Jurassic) ...................... 10 2.2.6 Dakota Group (Lower Cretaceous) ................... 10 2.2.7 Benton Shale Formation (Lower/Upper Cretaceous) ....... 11 2.2.8 Niobrara Formation (Upper Cretaceous) ............... 11 2.2.9 Pierre Shale Formation (Upper Cretaceous) ............. 11 2.2.10 Fox Hills Sandstone Formation (Upper Cretaceous) ....... 12 2.2.1 1 Laramie Formation (Upper Cretaceous) ............... 12 2.2.12 -
Structural Evolution of the Oil Well Flats Detachment System, Cañon City Embayment, Colorado
STRUCTURAL EVOLUTION OF THE OIL WELL FLATS DETACHMENT SYSTEM, CAÑON CITY EMBAYMENT, COLORADO by Lauren C. Cross A thesis submitted to the Faculty and Board of Trustees of the Colorado School of Mines in partial fulillment of the requirements for the degree of Master of Science (Geology). Golden, Colorado Date ________________ Signed: _______________________ Lauren Cross Signed: _______________________ Dr. Bruce D. Trudgill Thesis Advisor Golden, Colorado Date ________________ Signed: _______________________ Dr. Paul Santi Professor and Head of Department of Geology and Geological Engineering ii ABSTRACT The Cañon City Embayment, located at the southern end of the Denver Basin, Colorado, is an understudied area with a complex structural history affected by major tectonic events such as the Ancestral Rocky Mountain Orogeny, Laramide Orogeny, regional epeirogenic uplift events, and Cenozoic extension. This area is of interest to the petroleum industry in part due to its proximity to Florence-Cañon City Oil Field, which produces from shallow, heavily fractured Pierre Shale and is the oldest continuously working oil ield in the United States. Detailed ield mapping identiied a ~3 km2 detachment fault system in the Oil Well Flats area, located in the northern part of the Cañon City Embayment, which is currently mapped as Quaternary alluvium and landslide deposits. The structure exhibits several topographically high, repeating blocks of Cretaceous Dakota Group sandstones, separated by topographically low valleys that are likely underlain by shale, -
Osteology of a Near-Complete Skeleton of Tenontosaurus Tilletti (Dinosauria: Ornithopoda) from the Cloverly Formation, Montana, USA
Osteology of a Near-Complete Skeleton of Tenontosaurus tilletti (Dinosauria: Ornithopoda) from the Cloverly Formation, Montana, USA A report submitted in partial fulfilment of the requirements for the degree of MEarthSci Geology (Hons.), University of Manchester Jonathan Tennant 70406912 MEarthSci Geology (Hons.) School of Earth, Atmospheric and Environmental Sciences University of Manchester Williamson Building Oxford Road Manchester M13 9PL Osteology of Tenontosaurus tilletti Contents Figures and Tables..............................................................................................................................................3 1.0 Abstract .............................................................................................................................................................6 2.0 Introduction ......................................................................................................................................................7 2.1 Aims and Objectives....................................................................................................................................7 2.2 Institutional Abbreviations ........................................................................................................................9 3.0 Previous Work ............................................................................................................................................... 11 3.1 The Cloverly Formation .......................................................................................................................... -
The Rangelands of Colorado
RANGELANDS 15(5), October 1993 213 The Rangelands of Colorado John E. Mitchell To understand the rangelands of Utah border also receives very little Physlographic Regions Colorado,one should first look at its precipitation. Note: It is not com- Physiographers have dividedColo- physiography. Colorado can right- monly known that the stretch of the the be called the"zenith" of the Uni- ColoradoRiver between Grand Lake rado into three major provinces: fully and ted States; on is the and its confluence with Green Great Plains, Rocky Mountains, average, it high- the From a est state in elevation with morethan River in eastern Utah was called the Colorado Plateaus (Fig. 1). of time, these 50 peaks exceeding 14,000 ft. Moun- GrandRiver by early pioneers (Stan- perspective geological Iandforms are young.The pres- tain passes crossingthe Continental ton 1965).] quite Divide in ent Rocky Mountains were uplifted Colorado frequently are Like other western states, Colo- The Great above ft. The lowest in radois The only 60 million years ago. 11,000 point predominantly rangeland. ofalluvial mater- the state, the Arkansas River 1979 Assessment of the U.S. Forest Plainsare composed along ial that eroded from these where it enters is and mandated uplifting Kansas, only slightly Rangeland Situation, and were over below 3,400 ft., while about 95% of the Renewable Resources Plan- mountains deposited by thick mantles of ancient worn Colorado'sland area is morethan "a Act of estimated that 47.5 gravels ning 1974, from ancestral Rockiesformed mile The headwaters of four million ac., or 72°Jo ofthe state's lands away highl" the Paleozoic Era major rivers can be found in the are About 55%of this during (Chronic grazed.