Badlands National Park Geologic Resource Evaluation Report
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South Dakota to Nebraska
Geological Society of America Special Paper 325 1998 Lithostratigraphic revision and correlation of the lower part of the White River Group: South Dakota to Nebraska Dennis O. Terry, Jr. Department of Geology, University of Nebraska—Lincoln, Lincoln, Nebraska 68588-0340 ABSTRACT Lithologic correlations between type areas of the White River Group in Nebraska and South Dakota have resulted in a revised lithostratigraphy for the lower part of the White River Group. The following pedostratigraphic and lithostratigraphic units, from oldest to youngest, are newly recognized in northwestern Nebraska and can be correlated with units in the Big Badlands of South Dakota: the Yellow Mounds Pale- osol Equivalent, Interior and Weta Paleosol Equivalents, Chamberlain Pass Forma- tion, and Peanut Peak Member of the Chadron Formation. The term “Interior Paleosol Complex,” used for the brightly colored zone at the base of the White River Group in northwestern Nebraska, is abandoned in favor of a two-part division. The lower part is related to the Yellow Mounds Paleosol Series of South Dakota and rep- resents the pedogenically modified Cretaceous Pierre Shale. The upper part is com- posed of the unconformably overlying, pedogenically modified overbank mudstone facies of the Chamberlain Pass Formation (which contains the Interior and Weta Paleosol Series in South Dakota). Greenish-white channel sandstones at the base of the Chadron Formation in Nebraska (previously correlated to the Ahearn Member of the Chadron Formation in South Dakota) herein are correlated to the channel sand- stone facies of the Chamberlain Pass Formation in South Dakota. The Chamberlain Pass Formation is unconformably overlain by the Chadron Formation in South Dakota and Nebraska. -
The Cheyenne River 2
BEFORE THE PUBLIC UTILITIES COMMISSION OF THE STATE OF SOUTH DAKOTA ) IN THE MATIER OF THE APPLICATION BY ) HP14-001 TRANSCANADA KEYSTONE PIPELINE, LP ) FOR A PERMIT UNDER THE SOUTH DAKOTA) APPLICATION FOR ENERGY CONVERSION AND TRANSMISSION) PARTY STATUS BY FACILITIES ACT TO CONSTRUCT THE ) THE CHEYENNE RIVER KEYSTONE XL PROJECT ) SIOUX TRIBE ) COMES NOW, the Cheyenne River Sioux Tribe, by and through its undersigned signatory, and pursuant to SDCL §49-41B-17(2)(3) petitions to be granted party-status in the above referenced matter. The petitioner's interests are as follows: 1. The Cheyenne River Sioux Tribe is a federally- recognized Indian Tribe residing on the Cheyenne River Sioux Reservation of South Dakota. The address of the Tribal government headquarters is Post Office Box 590, Eagle Butte, South Dakota 57625. 2. The Keystone XL project would cross lands that has been adjudged by the U.S. Indian Claims Commission and the U.S. Court of Claims to be the aboriginal and Treaty-titled land of the petitioner Cheyenne River Sioux Tribe. United States v. Sioux Nation ofIndians, 601 F.2d 1157, 1172 (Ct. Cl. 1975) aff'd 448 U.S. 384 (1980); Sioux Nation v. United States, 21 Ind. CL Comm. 371, 382 (1974). 3. The proposed Keystone XL (KXL) pipeline threatens to contaminate the source of water for our Mni Waste Water System. The pipeline is proposed to run through our aboriginal homelands just south of the western border of our present reservation. The proposed route of the pipeline will cross the Cannonball River, Grand River, Moreau River, and Cheyenne River in the Dakotas and these rivers individually and collectively enter the Missouri River in Lake Oahe, the Pick Sloan Reservoir immediately upstream from our intake. -
Black-Tailed Prairie Dog Management Plan
Badlands National Park – North Unit Environmental Assessment U.S. Department of the Interior National Park Service Badlands National Park, North Unit Pennington and Jackson Counties, South Dakota Black-Tailed Prairie Dog Management Plan Environmental Assessment August 2007 Badlands National Park – North Unit Environmental Assessment National Park Service Prairie Dog Management Plan U.S. Department of the Interior National Park Service Black-Tailed Prairie Dog Management Plan Environmental Assessment Badlands National Park, North Unit Pennington and Jackson Counties, South Dakota Executive Summary The U.S. Department of Interior, National Park Service (NPS) proposes to implement a comprehensive black-tailed prairie dog management plan for the North Unit of Badlands National Park where prairie dog populations have increased from approximately 2,070 acres in 1979 to 6,363 acres in 2006, or 11% of the approximately 60,000 acres of available suitable habitat. The principal objectives of the management plan are to ensure that the black-tailed prairie dog is maintained in its role as a keystone species in the mixed-grass prairie ecosystem on the North Unit, while providing strategies to effectively manage instances of prairie dog encroachment onto adjacent private lands. The plan also seeks to manage the North Unit’s prairie dog populations to sustain numbers sufficient to survive unpredictable events that may cause high mortality, such as sylvatic plague, while at the same time allowing park managers to meet management goals for other North Unit resources. Primary considerations in developing the plan include conservation of the park’s natural processes and conditions, identification of effective tools for prairie dog management, implementing strategies to deal with prairie dog encroachment onto adjacent private lands, and protection of human health and safety. -
Fossil Amphibians and Reptiles from the Neogene Locality of Maramena (Greece), the Most Diverse European Herpetofauna at the Miocene/Pliocene Transition Boundary
Palaeontologia Electronica palaeo-electronica.org Fossil amphibians and reptiles from the Neogene locality of Maramena (Greece), the most diverse European herpetofauna at the Miocene/Pliocene transition boundary Georgios L. Georgalis, Andrea Villa, Martin Ivanov, Davit Vasilyan, and Massimo Delfino ABSTRACT We herein describe the fossil amphibians and reptiles from the Neogene (latest Miocene or earliest Pliocene; MN 13/14) locality of Maramena, in northern Greece. The herpetofauna is shown to be extremely diverse, comprising at least 30 different taxa. Amphibians include at least six urodelan (Cryptobranchidae indet., Salamandrina sp., Lissotriton sp. [Lissotriton vulgaris group], Lissotriton sp., Ommatotriton sp., and Sala- mandra sp.), and three anuran taxa (Latonia sp., Hyla sp., and Pelophylax sp.). Rep- tiles are much more speciose, being represented by two turtle (the geoemydid Mauremys aristotelica and a probable indeterminate testudinid), at least nine lizard (Agaminae indet., Lacertidae indet., ?Lacertidae indet., aff. Palaeocordylus sp., ?Scin- cidae indet., Anguis sp., five morphotypes of Ophisaurus, Pseudopus sp., and at least one species of Varanus), and 10 snake taxa (Scolecophidia indet., Periergophis micros gen. et sp. nov., Paraxenophis spanios gen. et sp. nov., Hierophis cf. hungaricus, another distinct “colubrine” morphotype, Natrix aff. rudabanyaensis, and another dis- tinct species of Natrix, Naja sp., cf. Micrurus sp., and a member of the “Oriental Vipers” complex). The autapomorphic features and bizarre vertebral morphology of Perier- gophis micros gen. et sp. nov. and Paraxenophis spanios gen. et sp. nov. render them readily distinguishable among fossil and extant snakes. Cryptobranchids, several of the amphibian genera, scincids, Anguis, Pseudopus, and Micrurus represent totally new fossil occurrences, not only for the Greek area, but for the whole southeastern Europe. -
Hyracodons and Subhyracodons Early Rhinoceros by Ryan C
The Fossils of the White River Badlands http://whiteriver.weebly.com/hyracodons.html Hyracodons and Subhyracodons Early rhinoceros by Ryan C. The discovery of rhinoceros in the Badlands of the American West was very exciting, most people never suspecting that such primitive forms of rhinoceros existed in North America. Today, living rhinoceroses consist of four genera that contain five species. Two are found in Africa; three others are restricted to Asia. Most are browsing animals but the largest species, the white rhinoceros of Africa, is a grazer. All living species possess "horns" that are composed of keratinized hair which decomposes at death and are not normally preserved in the fossil record. Although most New World rhinoceroses did not have horns, the widely distributed, males of the pig-sized Menoceros of the early Miocene had a lateral pair of horns. In North America, "rhinoceroses" of three similar lineages appeared from Asia during the Middle Eocene. Consisting of hippo-like Amynodontidae, "running rhinos" or Hyracodontidae, and true rhinoceroses, Rhinocerotidae, only true rhinoceroses adapted and diversified enough to survive into the early Pliocene. Amynodontids entered North America during the Bridgerian NALMA. Apparently adapted for a warm humid environment typified by lush forests, most amynodontids physically and ecologically resembled the hippopotamus of Africa. Remaining undiversified, only four genera are recognized and three of them contain but a single species. The massive and best known species is Metamynodon planifrons, a form characterized by having massive teeth with large tusks that give it the appearance of a hippopotamus. Some skeletons were 10 ft in length. Due to their skull structure, some believe this group supported a proboscis similar to that of a modern tapir. -
The Brule-Gering (Oligocene-Miocene) Contact in the Wildcat Ridge Area of Western Nebraska
CORE Metadata, citation and similar papers at core.ac.uk Provided by UNL | Libraries University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Bulletin of the University of Nebraska State Museum Museum, University of Nebraska State 1967 The Brule-Gering (Oligocene-Miocene) Contact in the Wildcat Ridge Area of Western Nebraska C. Bertrand Schultz University of Nebraska Charles H. Falkenbach Nebraska State Museum Carl F. Vondra American Museum of Natural History Follow this and additional works at: https://digitalcommons.unl.edu/museumbulletin Part of the Entomology Commons, Geology Commons, Geomorphology Commons, Other Ecology and Evolutionary Biology Commons, Paleobiology Commons, Paleontology Commons, and the Sedimentology Commons Schultz, C. Bertrand; Falkenbach, Charles H.; and Vondra, Carl F., "The Brule-Gering (Oligocene-Miocene) Contact in the Wildcat Ridge Area of Western Nebraska" (1967). Bulletin of the University of Nebraska State Museum. 58. https://digitalcommons.unl.edu/museumbulletin/58 This Article is brought to you for free and open access by the Museum, University of Nebraska State at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Bulletin of the University of Nebraska State Museum by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. BULLETIN OF The University of Nebraska State Museum VOLUME 6 , NUMBER 4 SEPTEMBER 1967 C. Bertrand Schultz Charles H. Falkenbach Carl F. Vondra The Brule-Gering (Oligocene-Miocene) Contact in the Wildcat Ridge Area of Western Nebraska A Guide for the Stratigraphic Collecting of Fossil Mammals The University of Nebraska The Board of Regents RICHARD E. ADKINs J. G. ELLIOTI B. N. GREENBERG, M.D. RICHARD L. -
County of Riverside General Plan Reche Canyon/Badlands Area Plan
County of Riverside General Plan Reche Canyon/Badlands Area Plan COUNTY OF RIVERSIDE Transportation and Land Management Agency 4080 Lemon Street, 12th Floor Riverside, CA 92501-3634 Phone: (951) 955-3200, Fax: (951) 955-1811 October 2011 County of Riverside General Plan Reche Canyon/Badlands Area Plan TABLE OF CONTENTS Vision Summary.......................................................................................................................................................... iv Introduction ................................................................................................................................................................. 1 A Special Note on Implementing the Vision ........................................................................................................ 2 Location ........................................................................................................................................................................ 3 Features ........................................................................................................................................................................ 7 Setting ....................................................................................................................................................................... 7 Unique Features ........................................................................................................................................................ 7 Badlands/Norton Younglove Preserve -
Hoganson, J.W., 2009. Corridor of Time Prehistoric Life of North
Corridor of Time Prehistoric Life of North Dakota Exhibit at the North Dakota Heritage Center Completed by John W. Hoganson Introduction In 1989, legislation was passed that directed the North Dakota and a laboratory specialist, a laboratory for preparation of Geological Survey to establish a public repository for North fossils, and a fossil storage area. The NDGS paleontology staff, Dakota fossils. Shortly thereafter, the Geological Survey signed now housed at the Heritage Center, consists of John Hoganson, a Memorandum of Agreement with the State Historical Society State Paleontologist, and paleontologists Jeff Person and Becky of North Dakota which provided space in the North Dakota Gould. This arrangement has allowed the Geological Survey, in Heritage Center for development of this North Dakota State collaboration with the State Historical Society of North Dakota, Fossil Collection, including offices for the curator of the collection to create prehistoric life of North Dakota exhibits at the Heritage Center and displays of North Dakota fossils at over 20 other museums and interpretive centers around the state. The first of the Heritage Center prehistoric life exhibits was the restoration of the Highgate Mastodon skeleton in the First People exhibit area (fig. 1). Mastodons were huge, elephant- like mammals that roamed North America at the end of the last Ice Age about 11,000 years ago. This exhibit was completed in 1992 and was the first restored skeleton of a prehistoric animal ever displayed in North Dakota. The mastodon exhibit was, and still is, a major attraction in the Heritage Center. Because of its popularity, it was decided that additional prehistoric life displays should be included in the Heritage Center exhibit plans. -
Grand Canyon National Park Service U.S
National Park Grand Canyon National Park Service U.S. Department of the Interior The Painted Map by Erwin Ralsz WHAT IS The Painted Desert is a well-known Formation. While several rock layers in THE PAINTED DESERT? Arizona landscape of very colorful "bad northeastern Arizona are colorful, it is the lands" extending across northeastern particular beauty of the Chinle Formation Arizona. (Badlands are intricately dis that gave rise to the notion of a Painted sected, barren, and rounded landscapes that Desert. Although the Chinle Formation can typically occur in arid regions where weak be seen elsewhere, in the Painted Desert the rock is prevalent). The Painted Desert is exposure of this rock is long and continu distinctly defined by exposures of a rock ous. layer known as the Chinle (Chin-lee) The Painted Desert is exposed in a of Winslow, Arizona along State Highway WHERE TO SEE band of rock trending northwest from 87. Winslow is 140 miles from Grand THE PAINTED DESERT Holbrook, Arizona to The Gap, Arizona. Canyon's South Rim. This band is wider in the Holbrook area and narrows significantly to the northwest. Few Closest to Grand Canyon, the Painted roads provide access to the Painted Desert. Desert is exposed in a narrow band along U.S. Highway 89 from about 3 miles north Unquestionably, the most famous part of Cameron, Arizona (at milepost#470) to of the Painted Desert is at Petrified Forest the small village of The Gap farther north. National Park, 190 miles from the South A small but visually striking example of the Rim of Grand Canyon. -
The Cretaceous-Tertiary Boundary Interval in Badlands National Park, South Dakota
The Cretaceous-Tertiary Boundary Interval in Badlands National Park, South Dakota Philip W. Stoffer1 Paula Messina John A. Chamberlain, Jr. Dennis O. Terry, Jr. U.S. Geological Survey Open-File Report 01-56 2001 U.S. DEPARTMENT OF THE INTERIOR Gale A. Norton, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director The Cretaceous/Tertiary (K-T) boundary study interval at the Rainbow Colors Overlook along Badlands Loop Road, North Unit of Badlands National Park. This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey (USGS) editorial standards or with the North American Stratigraphic Code. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1345 Middlefield Road, Menlo Park, CA 94025 http://geopubs.wr.usgs.gov/open-file/of01-056/ ABSTRACT A marine K-T boundary interval has been identified throughout the Badlands National Park region of South Dakota. Data from marine sediments suggest that deposits from two asteroid impacts (one close, one far away) may be preserved in the Badlands. These impact- generated deposits may represent late Maestrichtian events or possibly the terminal K-T event. Interpretation is supported by paleontological correlation, sequence stratigraphy, magnetostratigraphy, and strontium isotope geochronology. This research is founded on nearly a decade of NPS approved field work in Badlands National Park and a foundation of previously published data and interpretations. The K-T boundary occurs within -
The New Adaption Gallery
Introduction In 1991, a group of Heritage Center staff began meeting informally after work to discuss a Heritage Center expansion. This “committee” was formalized in 1992 by Jim Sperry, Superintendent of the State Historical Society of North Dakota, and became known as the Space Planning About Center Expansion (SPACE) committee. The committee consisted of several Historical Society staff and John Hoganson representing the North Dakota Geological Survey. Ultimately, some of the SPACE committee ideas were rejected primarily because of anticipated high cost such as a planetarium, arboretum, and day care center but many of the ideas have become reality in the new Heritage Center expansion. In 2009, the state legislature appropriated $40 million for a $52 million Heritage Center expansion. The State Historical Society of North Dakota Foundation was given the task to raise the difference. On November 23, 2010 groundbreaking for the expansion took place. Planning for three new galleries began in earnest: the Governor’s Gallery (for large, temporary, travelling exhibits), Innovation Gallery: Early Peoples, and Adaptation Gallery: Geologic Time. The Figure 1. Partial Stratigraphic column of North Dakota showing Figure 2. Plate tectonic video. North Dakota's position is indicated by the the age of the Geologic Time Gallery displays. red symbol. JULY 2014 1 Orientation Featured in the Orientation area is an interactive touch table that provides a timeline of geological and evolutionary events in North Dakota from 600 million years ago to the present. Visitors activate the timeline by scrolling to learn how the geology, environment, climate, and life have changed in North Dakota through time. -
North and South Dakota
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR BtELIiETIN 575 «v^L'l/"k *. GEOLOGY OP THE NORTH AND SOUTH DAKOTA BY W. R. CALVERT, A. L. BEEKLY, V. H. BARNETT AND M. A. PISHEL WASHINGTON GOVERNMENT FEINTING OFFICE 1914 vti.'CS i«\ IJ) C -«"PA4 £, * 0 CONTENTS. Introduction.............................................................. 5 Field work............................................................... 6 Previous examinations........:............................................ 6 Geography. .............................................................. 7 Location and extent of area............................................ 7 Relief................................................................ 7 Drainage.............................................................. 8 Culture. ....................................................v .......... 8 Descriptive geology........................................................ 9 Stratigraphy.......................................................... 9 Occurrence of the rocks. ........................................... 9 Cretaceous system (Montana group)................................ 9 Pierre shale.................................................. 9 Character and distribution................................. 9 Age..................................................... 11 Fox Hills^sandstone.......................................... 11 Character and distribution................................. 11 Age......................................................