Department of Geology and Geological Engineering 2020 Alumni Newsletter
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VIDEO SCRIPT TITLE: Stories From The Skies SERIES: Dakota Pathways: A History WRITER: Paul Higbee PRODUCER: Jim Sprecher DRAFT: Final with Scene Numbers SCRIPT NUMBER: 2 DATE: September 14, 2003 Approved : ______ ”Stories From The Skies” • 9/14/2003 • 1 VISUAL AUDIO 1. OPEN MONTAGE (:20) Kids at NAT SOUND UP AND UNDER Cultural Center with guide MUSIC UP. MUSIC UNDER 2. WS: Car traveling down country NARRATOR: road…white clouds, blue sky. No matter where you travel in South Dakota… 3. WS: Airliner taking off into …no matter how you travel, you can’t help beautiful sky over Sioux Falls. noticing the sky. 4. WS: Treeless sky On the treeless prairies, the sky looks immense. 5. DISSOLVE TO: Harvey Dunn That’s why South Dakota artists have painted it painting with beautiful sky. big and colorful. 6. WS Low Angle: Cathedral spires The sky serves as a backdrop for our most in Sioux Falls. inspiring buildings 7. WS: Crazy Horse Memorial in and monuments. Custer, against skies. 8. XCU: Rain on young corn crop. From the skies have come both life-giving rains… 9. XCU: Rain on puddle with cloudy sky reflection on water. 10. WS: Tornado tearing up land. and life-threatening dangers. 11. WS: Lightening from storm clouds. 12. MS: Pheasant flying up into South Dakota skies deliver sport… pretty sky. stories… 13. MS: Bi-plane doing aerial stunts. and mysteries. 14. WS: Brooding but colorful sunset. 15. MONTAGE: Sky shots, fast MUSIC UP AND UNDER moving clouds, ending in time- lapse sunrise. ERT: 13:40 Approved : ______ ”Stories From The Skies” • 9/14/2003 • 2 VISUAL AUDIO 16. -
Environmental Assessment Agriculture
United States Department of Environmental Assessment Agriculture Forest Service Byway Lakes Enhancement Project August 2013 Hell Canyon Ranger District, Black Hills National Forest Custer & Pennington Counties, South Dakota T02S, R05E Sections 11 T02S, R06E Sections 27, 28 T03S, R05E Sections 15, 22 Horsethief Lake 1938 For Information Contact: David Pickford 330 Mt. Rushmore Road Custer, SD 57730 Phone: (605) 673-4853 Email: [email protected] The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or part of an individual’s income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large-print, audiotape, etc.) should contact USDA’s TARGET Center at (202)720-2600 (voice and TDD). To file a complaint of discrimination, write to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, S.W., Washington, D.C. 20250-9410, or call (800)795-3272 (voice) or (202)720-6382 (TDD). USDA is an equal opportunity provider and employer. Table of Contents SUMMARY ..................................................................................................................................... i CHAPTER 1: INTRODUCTION -
Black Hills National Forest
United States Department of Agriculture Forest Service Rocky Black Hills Mountain Region Black Hills National National Forest Forest Custer South Dakota March 2006 Land and Resource Management Plan 1997 Revision Phase II Amendment LIST OF ABBREVIATIONS/ACRONYMS ACHP President’s Advisory Council on MMBF Million Board Feet Historic Preservation MMCF Million Cubic Feet A.F.F. Agricultural, Forestry, and Fishing MOU Memorandum of Understanding Services MPB Mountain Pine Beetle AMP Allotment Management Plan NAAQS National Ambient Air Quality AOI Annual Operating Instructions Standards ARC At-risk Communities NEPA National Environmental Policy Act ASQ Allowable Sale Quantity NF National Forest ATV All Terrain Vehicle NFMA National Forest Management Act AUM Animal Unit Month NFP National Fire Plan BA Botanical Areas NFPA National Forest Protection BA Biological Assessment Association BBC Birds of Conservation Concern NFS National Forest System BBS Breeding Bird Survey National Register National Register of Historic Places BCR Bird Conservation Regions NIC Non-Interchangeable Component BE Biological Evaluation NOA Notice of Availability BHNF Black Hills National Forest NOAA National Oceanic and Atmospheric Black Hills Black Hills Ecoregion Administration BLM Bureau of Land Management NOI Notice of Intent BMP Best Management Practices NWCG National Wildland Fire Coordinating BOR Bureau of Recreation Group BTU British Thermal Unit OHV Off Highway Vehicle CEQ Council on Environmental Quality PCPI Per Capita Personal Income CF Cubic Feet PIF Partners -
THE AFTERMATH of the 1972 RAPID CITY FLOOD Arnett S
THE AFTERMATHOF THE 1972 RAPID CITY FLOOD Arnett S. Dennis Rapid City, South Dakota Abstract. The aftermath of the 1972 Rapid City flood included a controversy over the propriety of cloud seeding on the day of the flood and a lawsuit against the U. S. Government.Preparation of the defense against the suit involved analyses of hourly rainfall accumulations, radar data from the seeded clouds, and possible microphysical and dynamic effects of seeding clouds with powdered sodium chloride (salt). Recent developments in numerical modeling offer some hope of improved understanding of the storm. However, mesoscale systems remain somewhat unpredictable, and realization of this fact has inhibited research dealing with the deliberate modification of large convective clouds. 1. ORIGIN OF THE CONTROVERSY until about 6:00 p.m. This storm was immediately recognized by our meteorologists as dangerous and The Institute of Atmospheric Sciences (IAS) was never seeded by our group," The Governor’s of the South Dakota School of Mines and Tech- office accepted Schleusener’s report and issued nology (School of Mines) conducted two cloud a statement asking the public to refrain from seeding flights at the eastern edge of the Black Hills spreading rumors. An investigative team sent on Friday, 9 June 1972. Late that evening, a flash to Rapid City by the Bureau of Reclamation flood swept down Rapid Creek and devastated (Reclamation) of the U. S. Departmentof the Interior Rapid City. On the following day, the IAS Director, (Interior), which sponsored the IAS cloud seeding Dr. Richard Schleusener, organized a telephone experiments, also reported in an internal memo- "tree," which produced the gratifying news that all randum dated 21 June that cloud seeding did not IAS staff membersand their immediate families cause the flood. -
Full Investigations and Windshield Surveys
Appendix 2: Full Investigations and Windshield Surveys During Phase III of the update project, the RCHPC sponsored the creation of nine focused investigations that explored specific aspects of Rapid City’s history. Each essay is available in full below. Each includes samples of historical documentation from newspapers and local archives as well as photographs of buildings and spaces relevant to each topic that still exist in Rapid City. The Ridgeline and the Creek: Landscape and Memory in Rapid City The Black Hills formed when a large, oblong section of igneous rock lifted through the earth’s mantle some 65 million years ago, breaking through the limestone crust to expose the large, stone center of the Hills. In and around this central ring, forests thick with ponderosa pines, blue spruce, and cedar trees cropped up. They intersperse in meadows with prairie grasses and shrubs and are home to an array of animals including deer, elk, beavers, squirrels, raccoons, skunks, rabbits, and more. Bison, grizzly bears, wolves, mountain lions, and coyote once inhabited the vast prairies surrounding the Black Hills. Most of the large predators and most of the bison were killed off or pushed out as Euro-Americans displaced early Indigenous inhabitants. Rapid City grew up at the vertex of water and stone. A long, narrow ridgeline juts from south to north. Residents can look up at the ridge from any side of town or peer down over the vast distance visible from Skyline Drive or Highway 16. The ridge forms the backbone of the Rapid City landscape and includes two main parts from south the north: Hangman’s Hill, which is traversed by Skyline Drive, and Cowboy Hill, which begins immediately north of Rapid Creek. -
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The Journal of Weather Modification 2002 Texas Weather Modification Scientific Management Seeded Control Simple Ratio Increase Prec. Mass 1439.3 kton 667.4 kton 2.16 (1.89) 116 (89) After modeling the increase dropped to 89 % Volume 35 April 2003 WEATHER MODIFICATION ASSOCIATION North American Weather Our weather modification Consultants (NAWC) is the services span the full spectrum, world’s longest-standing from a) feasibility studies to b) private weather modification turn-key design, conduct, and company. evaluation of projects to c) total A recognized leader since technology transfer. By 1950, many consider us the combining practical technical world’s premier company in this advances with field-proven dynamic field. We are proud of methods and operational our sterling record and long list of expertise, we provide expert satisfied customers. assistance to water managers and users in the agricultural, governmental, and hydroelectric communities worldwide. together the best-suited We offer ground-based and/or methods, materials, equipment airborne, summer and winter systems and talent to provide operational and research you with the greatest project programs. Additional specialties value. in extreme storm studies, climatic When you put it all together, surveys, air quality, NAWC is the logical choice meteorological observing for high value weather systems, forensic meteorology modification services. Visit our and weather forecasting, broaden website at www.nawcinc.com for our meteorological perspective. more information, and call us at Whatever your weather (801) 942-9005 to discuss your modification needs, we can help. needs. You can also reach us We will tailor a project to your by email: [email protected]. -
The Stratobowl Flights of the 1930'S
The Stratobowl Flights of the 1930’s Teaching Tip Wind Study: For a Lifetime Wind Study: For a Lifetime During this activity your students will learn about two 1930s balloon flights launched near Rapid City that provided invaluable scientific data about the nature of the Earth's atmosphere at the edge of space, also setting an altitude record that would stand for 21 years. The students will then participate in a qualitative wind speed study. Both aircrafts were assembled and sent aloft from an unusual bowl-shaped gorge in the Black Hills. A flat patch of land surrounded by high, steep cliffs provided shelter from wind and the best-possible conditions for inflating and launching large, lighter-than-air craft. The formation is now known as the Stratobowl. According to the USDA Forest service, “The Stratobowl, a natural depression in the terrain of the Black Courtesy: EPOD (Mike Barondeau), “The Stratobowl pictured Hills, has 300-to-500-foot sides combined of tree-lined banks above is located about 1.5 miles (2.4 km) off Highway 16 and jagged limestone cliffs while the bottom is a flat plain of between Rapid City, South Dakota and Mt. Rushmore.” about 35 acres.” The Explorer I flight launched July 28, 1934, reached a height of 60,616 feet (11.5 miles) before a rip in the balloon's fabric allowed an uncontrolled release of hydrogen. Explorer II was launched from the Stratobowl in frigid weather on November 11, 1935 with Captains Stevens and Anderson on board. It's estimated that between 35,000 to 40,000 people witnessed the launch. -
Papers of the Dakota Conference a National Conference on the Northern Plains
Papers of the Dakota Conference A National Conference on the Northern Plains Index: 1990-2010 Compiled by: Amanda Jenson Team The Center for Western Studies Preface The Center for Western Studies (CWS) of Augustana College is pleased to make available this index to the Papers of the Dakota Conference on Northern Plains History, Literature, Art, and Archaeology for the years 1990 to 2010. Over the years, many individuals have contributed to this index. This update, for 2008 to 2010, was done by Collections Assistant Amanda Jenson. In 1989, following the Twenty-second Annual Dakota History Conference, Dakota State University, the home of the conference since its founding in February 1969, invited South Dakota institutions to consider sponsoring the conference, since the academic program at Dakota State no longer accommodated a history conference. The Center for Western Studies agreed to administer the conference beginning in 1990, with the promise of financial support consideration from the South Dakota Humanities Council. The Humanities Council provided grant support for the conference annually from 1990 to 2008, in response to competitive proposals submitted by CWS. Over the years, significant additional financial support has been received from several individuals and organizations. For twenty-one years, the Center for Western Studies has not only administered the conference but has also expanded its scope to include the northern Great Plains and welcomed papers on literature, art, and archaeology as well as history. Dedicated to examining regional issues in their historical and cultural contexts, the Dakota Conference is now a signature event of CWS, which provides programming in Northern Plains studies at Augustana College. -
SBCC-Report Revised
I. EXECUTIVE SUMMARY 1. The 730-acre property at Sitting Bull Crystal Caverns (SBCC) is of great significance to the geological history of the Black Hills, as well as the histories of South Dakota tourism and, most importantly, of the Oceti Sakowin (“Great Sioux Nation”). Located about ten miles south of downtown Rapid City on Highway 16, the property sits in the heart of the sacred Black Hills (Paha Sapa), which are the creation place of the Lakota people. The Sitting Bull Cave system—named after the famed Hunkpapa leader, who is said to have camped on the property in the late 1800s—is located in the “Pahasapa limestone,” a ring of sedimentary rock on the inner edges of the “Racetrack” described in Lakota oral traditions. There are three caves in the system. The deepest, “Sitting Bull Cave,” boasts some of the largest pyramid-shaped “dog tooth spar” calcite crystals anywhere in the world. The cave opened to tourists after significant excavation in 1934 and operated almost continuously until 2015. It was among the most successful early tourist attractions in the Black Hills, due to the cave’s stunning beauty and the property’s prime location on the highway that connects Rapid City to Mount Rushmore. 2. The Duhamel Sioux Indian Pageant was created by Oglala Holy Man Nicholas Black Elk and held on the SBCC grounds from 1934 to 1957. Black Elk was a well-known Oglala Lakota whose prolific life extended from his experience at the Battle of the Little Bighorn in 1876 to the publication of Black Elk Speaks in 1932 and beyond. -
Subject File 1000: Organization and Management
Black Hills National Forest Historical Collection, 2016 Accession - Custer Office Series III. Manuscript Materials FS File Estimated Location Description Known Dates Code Dates 2016A FC42.D2.F1 1200 BHNF Personnel 1906-1954 1962 Annual Review / U.S. Department of 2016A FC42.D2.F2 1600 1962 Agriculture, Forest Service Dedication Ceremony: BHNF Headquarters, Custer, 2016A FC42.D2.F3 1600 1980 SD: Invitation and Program 2016A FC42.D2.F4 1600 BHNF FY1994 Facts and Statistical Information 1994 2016A FC42.D2.F5 1600 BHNF Annual Reports FY1999, FY2000, FY2003 1999-2003 2016A FC42.D2.F6 1630 Place Names & Their Locations List 1955 Newspapers: Custer County Chronicle, v. 135 issue 5 2016A FC42.D2.F7 1630 (Feb. 4, 2015): "Forest Service to Consolidate 2015 Locations" 2016A FC42.D2.F8 1680 Misc Historical Papers: CCC, Timber 1905-2004 CCC Documentation for Bowles (Boles?) Canyon 2016A FC42.D2.F9 1680 1935-1938 Truck Trail Bits and Pieces: Your Own Western History 2016A FC42.D2.F10 1680 1977 Magazine, v. 11, no. 4 Forest Service History Series: The Wilderness 2016A FC42.D2.F11 1680 1988 Movement and the National Forests: 1980-1984 TPIA "Adopt-a-Creek" Program, Knotty Pines 4-H 2016A FC42.D2.F12 1830 1988-1991 Club Ecology, Silviculture, and Management of Black Hills 2016A FC42.D2.F17 2070 2002 Ponderosa Pine / Shepperd and Battaglia Improving Range Conditions for Wartime Livestock 2016A FC42.D2.F18 2240 1942 Production Forest Landscape Management vol. 1: Ecological 2016A FC42.D2.F13 2380 Land Unit Visual Resource Evaluations / Reetz & 1977 Williams; Folder 1 of 4 Forest Landscape Management vol. -
G E O L O G Y This Interpretive Site Is Located Near a Significant Geologic Boundary
G E O L O G Y This interpretive site is located near a significant geologic boundary. • You are standing approximately 450 feet west of a geologic contact called the “Great Unconformity” that By the beginning of the Paleozoic era, approximately 540 million years ago, the Precambrian‐age rocks had separates older Precambrian‐age rocks from younger Paleozoic‐age rocks. been eroded down to a nearly level surface. A seaway encroached from the west about 525 million years ago, • To the west (left) are metamorphic rocks of Precambrian age. As you drive toward Mount Rushmore, resulting in the accumulation of sedimentary rocks. The erosional surface between the Precambrian rocks and Precambrian‐age rocks include schist, amphibolite, quartzite, and granite. A large road cut in schist is 1.7 the younger, overlying Paleozoic rocks represents a break in time of approximately 1 billion years where rocks miles to the southwest. were not preserved. This break in time is called the “Great Unconformity.” It is marked below in the aerial • To the east are gently‐dipping younger sedimentary rocks of Paleozoic age. The road cut 0.2 miles to the east photo and is located on the hillside about 450 feet to the east‐northeast of this location. is in the Pahasapa Limestone. An outcrop of Pahasapa Limestone is also visible as a distant ridgeline N Stratobowl approximately 4 miles to the north. The Paleozoic and Tertiary sedimentary rocks deposited near this interpretive site include, from youngest to oldest: West Pahasapa Limestone Gravel deposit Minnelusa Formation -
Papers of the Dakota Conference Index: 1990-2015
Papers of the Dakota Conference A National Conference on the Northern Plains Index: 1990-2015 Compiled by Matthew Housiaux Team The Center for Western Studies Preface The Center for Western Studies (CWS) of Augustana is pleased to make available this index to the Papers of the Dakota Conference on Northern Plains History, Literature, Art, and Archaeology for the period 1990 to 2015. Over the years, many individuals have contributed to this index. This update, for 2011 to 2015, was compiled by CWS Intern Matthew Housiaux. In 1989, following the Twenty-second Annual Dakota History Conference, Dakota State University, the home of the conference since its founding in February 1969, invited South Dakota institutions to consider sponsoring the conference, since the academic program at Dakota State no longer accommodated a history conference. The Center for Western Studies agreed to administer the conference beginning in 1990, with the promise of financial support consideration from the South Dakota Humanities Council. The Humanities Council provided grant support for the conference annually from 1990 to 2008, in response to competitive proposals submitted by CWS. Over the years, significant additional financial support has been received from several individuals and organizations. For twenty-six years, the Center for Western Studies has not only administered the conference but has also expanded its scope to include the northern Great Plains and welcomed papers on literature, art, and archaeology as well as history. Dedicated to examining regional issues in their historical and cultural contexts, the Dakota Conference is a signature event of CWS, which provides programming in Northern Plains studies at Augustana College.