Waco Mammoth Site • Special Resource Study / Environmental Assessment • Texas Waco Mammoth Site Special Resource Study / Environmental Assessment
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Teacher Guide: Meet the Proboscideans
Teacher Guide: Meet the Proboscideans Concepts: • Living and extinct animals can be classified by their physical traits into families and species. • We can often infer what animals eat by the size and shape of their teeth. Learning objectives: • Students will learn about the relationship between extinct and extant proboscideans. • Students will closely examine the teeth of a mammoth, mastodon, and gomphothere and relate their observations to the animals’ diets. They will also contrast a human’s jaw and teeth to a mammoth’s. This is an excellent example of the principle of “form fits function” that occurs throughout biology. TEKS: Grade 5 § 112.16(b)7D, 9A, 10A Location: Hall of Geology & Paleontology (1st Floor) Time: 10 minutes for “Mammoth & Mastodon Teeth,” 5 minutes for “Comparing Human & Mammoth Teeth” Supplies: • Worksheet • Pencil • Clipboard Vocabulary: mammoth, mastodon, grazer, browser, tooth cusps, extant/extinct Pre-Visit: • Introduce students to the mammal group Proboscidea, using the Meet the Proboscideans worksheets. • Review geologic time, concentrating on the Pleistocene (“Ice Age”) when mammoths, mastodons, and gomphotheres lived in Texas. • Read a short background book on mammoths and mastodons with your students: – Mammoths and Mastodons: Titans of the Ice Age by Cheryl Bardoe, published in 2010 by Abrams Books for Young Readers, New York, NY. Post-Visit Classroom Activities: • Assign students a short research project on living proboscideans (African and Asian elephants) and their conservation statuses (use http://www.iucnredlist.org/). Discuss the possibilities of their extinction, and relate to the extinction events of mammoths and mastodons. Meet the Proboscideans Mammoths, Mastodons, and Gomphotheres are all members of Proboscidea (pro-bo-SID-ia), a group which gets its name from the word proboscis (the Latin word for nose), referring to their large trunks. -
Secretary Richard Benda From
To: Secretary Richard Benda From: Melissa Bump Date: 06/09/09 RE: May 2009 - 2010 Summary Accomplishing the 2010 Initiative will take the Office of Tourism, the visitor industry, and the State of South Dakota to a whole new level. Feedback and suggestions regarding this summary report are encouraged. GOAL ONE: Double Visitor Spending from $600 Million to $1.2 Billion by 2010 Tourism Office Funding Update: April 2008 April 2009 % Change Deadwood Gaming Tax $ 260,945 $ 244,384 -6.3% Tourism Promotion Tax $ 228,602 $ 252,709 10.5% Total Monthly Deposits $ 489,547 $ 497,093 1.5% FY 2008 vs. 2009 $8,345,367 $8,443,677 1.2% 1A. Change the way we market South Dakota. • Tour Operators: Hosted From the Prairies to the Mountains familiarization tour for 10 domestic tour operators: two from W. Bloomfield, Michigan; two from Chippewa Falls, Wisconsin; one from Mountain Home, Arkansas; two from Woodville, Mississippi; two from Winston-Salem, North Carolina; and one from Indianapolis, Indiana; plus three tour representatives from Suriname. 1C. greater use of partnerships and cooperative efforts. • Million Dollar Challenge: New projects for FY2010 include Cow-Spring Creek Peninsula Recreation Area for Tony Dean Festival, August 7-9; and Watertown CVB’s City Monopoly and Geocaching promotion. • MultiMedia Press Release Co-op: Fort Sisseton had an open rate of 31.84%; Mount Rushmore Facelift had an open rate of 39.45%; Mt. Rushmore Black Hills Gold Jewelry Co. had an open rate of 29.80%; and Reptile Gardens had an open rate of 36.31%. 1E. Capitalize on the existing outdoors opportunities in our state. -
Expedition Black Hills Option B1
Medicine Mountain Scout Ranch 24201 Bobcat Road Custer, South Dakota 57730 Expedition: Black Hills Option B1 - 3 Day Program Destinations Include: • Mammoth Site • Black Elk Peak (Formerly Harney Peak) • Wind Cave National Park • Sylvan Lake • Mount Rushmore • Crazy Horse Memorial & Laser Light Show • 1880 Train • The Alpine Inn If after reading this overview, you have any questions, please contact our friendly team at 605-342-2824 or send an email to [email protected]. EXPEDITION: BLACK HILLS Key Info: Option Number B1 Tour Length Monday - Wednesday or Wednesday - Friday (3 days) Cost Per Person $380.00 (estimated - Call for exact pricing) Day 1 Destinations in this Option 6:45AM Breakfast in Campsite 8:00AM Depart Camp Mammoth Site 9:30AM Mammoth Site For centuries the bones lay buried, until 12:00PM Sack Lunch at Mammoth Site discovered by chance in 1974 during excavating 1:00PM Wind Cave National Park for a housing development, when earth moving 5:00PM Dinner in Campsite equipment exposed South Dakota’s greatest 7:00PM - 9:00PM Open Program at Camp fossil treasure. Fortunately, through the work of Day 2 local citizens, the Mammoth Site was preserved. 6:45AM Breakfast in Campsite Today it is the world’s largest Columbian 8:00AM Depart Camp mammoth exhibit, and a world-renown 9:00AM Mount Rushmore research center for Pleistocene. 12:00PM Sack Lunch at Mount Rushmore 1:15PM 1880 Train Wind Cave National Park 5:00PM Dinner in Campsite A hidden world beneath the prairie… 7:00PM - 9:00PM Open Program at Camp Bison, elk, and other wildlife roam the rolling Day 3 prairie grasslands and forested hillsides of one 6:45AM Breakfast in Campsite of America’s oldest national parks. -
NRC-086-00-BD01 Identified: 8/19/2014 Admitted: 8/19/2014 Withdrawn: Rejected: Stricken: Other: in Eve L
NRC-086 Submitted: June 20, 2014 Hydrology, Hazards, and Geomorphic Development of Gypsum Karst in the Northern Black Hills, South Dakota and Wyoming By JACK B. EPSTEIN U.S. Geological Survey, National Center, MS 926a, Reston, VA 20192 Abstract Dissolution of gypsum and anhydrite in four stratigraphic units in the Black Hills, South Dakota and Wyoming, has resulted in development of sinkholes and has affected formational hydrologic characteristics. Subsidence has caused damage to houses and water and sewage retention sites. Substratal anhydrite dissolution in the Minnelusa Formation (Pennsylvanian and Permian) has produced breccia pipes and pinnacles, a regional collapse breccia, sinkholes, and extensive disruption of bedding. Anhydrite removal in the Minnelusa probably dates back to the early Tertiary when the Black Hills was uplifted and continues today. Evidence of recent collapse includes fresh scarps surrounding shallow depressions, sinkholes more than 60 feet deep, and sediment disruption and contamination in water wells and springs. Proof of sinkhole development to 26,000 years ago includes the Vore Buffalo Jump, near Sundance, WY, and the Mammoth Site in Hot Springs, SD. Several sinkholes in the Spearfish Formation west of Spearfish, SD, which support fish hatcheries and are used for local agricultural water supply, probably originated 500 feet below in the Minnelusa Formation. As the anhydrite dissolution front in the subsurface Minnelusa moves down dip and radially away from the center of the Black Hills uplift, these resurgent springs will dry up and new ones will form as the geomorphology of the Black Hills evolves. Abandoned sinkholes and breccia pipes, preserved in cross section on canyon walls, attest to the former position of the dissolution front. -
La Brea and Beyond: the Paleontology of Asphalt-Preserved Biotas
La Brea and Beyond: The Paleontology of Asphalt-Preserved Biotas Edited by John M. Harris Natural History Museum of Los Angeles County Science Series 42 September 15, 2015 Cover Illustration: Pit 91 in 1915 An asphaltic bone mass in Pit 91 was discovered and exposed by the Los Angeles County Museum of History, Science and Art in the summer of 1915. The Los Angeles County Museum of Natural History resumed excavation at this site in 1969. Retrieval of the “microfossils” from the asphaltic matrix has yielded a wealth of insect, mollusk, and plant remains, more than doubling the number of species recovered by earlier excavations. Today, the current excavation site is 900 square feet in extent, yielding fossils that range in age from about 15,000 to about 42,000 radiocarbon years. Natural History Museum of Los Angeles County Archives, RLB 347. LA BREA AND BEYOND: THE PALEONTOLOGY OF ASPHALT-PRESERVED BIOTAS Edited By John M. Harris NO. 42 SCIENCE SERIES NATURAL HISTORY MUSEUM OF LOS ANGELES COUNTY SCIENTIFIC PUBLICATIONS COMMITTEE Luis M. Chiappe, Vice President for Research and Collections John M. Harris, Committee Chairman Joel W. Martin Gregory Pauly Christine Thacker Xiaoming Wang K. Victoria Brown, Managing Editor Go Online to www.nhm.org/scholarlypublications for open access to volumes of Science Series and Contributions in Science. Natural History Museum of Los Angeles County Los Angeles, California 90007 ISSN 1-891276-27-1 Published on September 15, 2015 Printed at Allen Press, Inc., Lawrence, Kansas PREFACE Rancho La Brea was a Mexican land grant Basin during the Late Pleistocene—sagebrush located to the west of El Pueblo de Nuestra scrub dotted with groves of oak and juniper with Sen˜ora la Reina de los A´ ngeles del Rı´ode riparian woodland along the major stream courses Porciu´ncula, now better known as downtown and with chaparral vegetation on the surrounding Los Angeles. -
Educator Guide Presented by the Field Museum
at the San Diego Natural History Museum July 4-November 11, 2013 Educator Guide Presented by The Field Museum INSIDE: Exhibition Introduction • Planning Your Visit Gallery Overviews and Guiding Questions • Focused Field Trip Activities Correlations to California State Content Standards • Additional Resources Mammoths and Mastodons: Titans of the Ice Age at the San Diego Natural History Museum is supported by: City of San Diego Commission for Arts and Culture County of San Diego Board of Supervisors, Community Enhancement Program Walter J. and Betty C. Zable Foundation Qualcomm Foundation The Kenneth T. and Eileen L. Norris Foundation VWR Charitable Foundation Education Sponsor: The Field Museum gratefully acknowledges the collaboration and assistance of the Shemanovskii Regional Museum and Exhibition Complex and the International Mammoth Committee. Walking Map The Field Museum • Mammoths and Mastodons Educator Guide • fieldmuseum.org/mammoths Page 2 www.sdnhm.org/mammoths-mastodons Exhibition Introduction Mammoths and Mastodons: Titans of the Ice Age July 4–November 11, 2013 Millions of years ago, colossal mammals roamed Europe, Asia, and North America. From the gigantic mammoth to the massive mastodon, these creatures have captured the world’s fascination. Meet “Lyuba,” the best-preserved baby mammoth in the world, and discover all that we’ve learned from her. Journey back to the Ice Age through monumental video installations, roam among saber-toothed cats and giant bears, and wonder over some of the oldest human artifacts in existence. Hands-on exciting interactive displays reveal the difference between a mammoth and a mastodon, This sketch shows a Columbian mammoth, an offer what may have caused their extinction, and show African elephant, and an American mastodon how today’s scientists excavate, analyze, and learn more (from back to front). -
Columbian Mammoths: Giants of the Ice Age
Name: __________________________________________________ Date: ______________ Columbian Mammoths: Giants of the Ice Age Did you know not all mammoths were woolly mammoths? The woolly mammoth was just one of nearly a dozen different species of mammoths. Another species was the Columbian (pronounced “cuh-LUM-be-un”) mammoth. Columbian mammoths lived during the Pleistocene Epoch (“PLY-stuh-SEEN EP-uck”), sometimes called the Ice Age. The Pleistocene Epoch started 2.5 million years ago and ended about 10,000 years ago. Even though people call it the Ice Age, not all the world was covered in ice. Sheets of ice called glaciers (“GLAY-shurs”) covered most of what is now Canada and the northern United States, but the lands that became the southern United States and Mexico were not under ice. Columbian mammoths were grazers, or animals that eat mostly grass. To make sure they had enough to eat, they lived in savannas (“suh-VAN-uhs”). Savannas are warm grasslands with scattered trees, and they were away from the glaciers. This was different from the woolly mammoths, which lived closer to the glaciers in lands called steppes (“STEPS”), cool plains with shrubs, herbs, and a little grass. How big was a Columbian mammoth? Huge! They were about 14 feet tall, or 4.3 meters. They also weighed as much as 10 tons, the same as a school bus. This made them much bigger than woolly mammoths, which were about 10 feet tall (3 meters) and weighed 6 tons. So why were they called Columbian mammoths? Scientists use New Latin to name animals. In New Latin, “Columbia” means “land of Columbus”, or North America. -
Mammoths' - National Park Service MAMMOTH SITE
^ \ . I I ^ I !* A 5,^' ; WACO 'The nation's first and only recorded discovery of a nursery herd of Pleistocene mammoths' - National Park Service MAMMOTH SITE WACO MAMMOTH SITE OVERVIEW • The Waco AAommoth Site sits In more than 100 acres of wooded parkland and is the result of a collabo ration between the City of Waco, Baylor University, and the Waco AAommoth Foundation. The City of Waco manages the site, while Baylor University's AAayborn AAuseum Complex curates the excavated mate rial and oversees scientific research. • Congressional legislation is currently pending to create the Waco Mammoth National Monument and to include the site as a unit of the Notional Park Service. • The Waco Mammoth Site was first discovered in 1978. The site is the only known discovery of a nursery herd (female mammoths and their offspring) in North America. This is also North America's largest known collection of Columbian mammoths that died in a single event. • Research indicates the Waco mammoths perished in a series of flood-related events spread across thou sands of years. One of the earliest events took place approximately 68,000 years ago and included 19 of the mammoths. • To date, 24 mammoths have been discovered, and the likelihood of additional fossils exists. A large por tion of the mammoth remains were discovered in the ravine outside of the dig shelter. COLUMBIAN MAMMOTH FACTS • Columbian Mammoths (Mommuthus columbi) lived during the Pleisto cene Epoch (2.5 million years to 10,000 yeors ago). • The Columbian mammoth was one of the largest mammals to have lived during the Pleistocene Epoch. -
Black Hills, Badlands & Mount Rushmore
COMPLIMENTARY $3.95 2019/2020 YOUR COMPLETE GUIDE TO THE PARKS BLACK HILLS, BADLANDS & MOUNT RUSHMORE ACTIVITIES • SIGHTSEEING • PRESERVATION EVENTS • TRAILS • HISTORY • MAPS • MORE OFFICIAL PARTNERS T:5.375” S:4.75” WELCOME S:7.375” SO TASTY EVERYONE WILL WANT A BITE. T:8.375” Welcome to the Black Hills and Badlands of South Dakota! As you explore our fine state, I’m confident you’ll find some of the best scenery, most unique attractions and friendliest people in the country. Our scenic drives, such as Spearfish Canyon and the 70-mile Peter Norbeck Scenic Byway, will surprise you with amazing views around every corner. Just 50 miles east, you’ll find a moon-like landscape in Badlands National Park. If you need to stretch your legs, you’ll find more than 400 miles of nature walks and hikes. South Dakota is also home to two of the world’s largest Chad Coppess/South Dakota Dept. of Tourism mountain carvings: patriotic Mount Rushmore National Me- Governor Dennis Daugaard & First Lady Linda Daugaard morial and Crazy Horse Memorial, a tribute to Native Ameri- cans. I encourage you to visit both and learn the history and story behind each of these magnificent sculptures. I also encourage you to take a drive through Custer State Park, the country’s second largest state park, where wildlife abounds. Along Wildlife Loop Road, you’ll have a chance to see antelope, deer, prairie dogs, “beg- ging” burros and the park’s 1,300-member bison herd. In fact, Austin-Lehman Adventures named Custer State Park one of the world’s Top 10 Wildlife Destinations. -
Karst Features in the Black Hills, Wyoming and South Dakota- Prepared for the Karst Interest Group Workshop, September 2005
193 INTRODUCTION TO THREE FIELD TRIP GUIDES: Karst Features in the Black Hills, Wyoming and South Dakota- Prepared for the Karst Interest Group Workshop, September 2005 By Jack B. Epstein1 and Larry D. Putnam2 1U.S. Geological Survey, National Center, MS 926A, Reston, VA 20192 2Hydrologist, U.S. Geological Survey, 1608 Mountain View Road, Rapid City, SD 57702. This years Karst Interest Group (KIG) field trips will demonstrate the varieties of karst to be seen in the semi-arid Black Hills of South Dakota and Wyoming, and will offer comparisons to karst seen in the two previous KIG trips in Florida (Tihansky and Knochenmus, 2001) and Virginia (Orndorff and Harlow, 2002) in the more humid eastern United States. The Black Hills comprise an irregularly shaped uplift, elongated in a northwest direction, and about 130 miles long and 60 miles wide (figure 1). Erosion, following tectonic uplift in the late Cretaceous, has exposed a core of Precambrian metamorphic and igneous rocks which are in turn rimmed by a series of sed- iments of Paleozoic and Mesozoic age which generally dip away from the center of the uplift. The homocli- nal dips are locally interrupted by monoclines, structural terraces, low-amplitude folds, faults, and igneous intrusions. These rocks are overlapped by Tertiary and Quaternary sediments and have been intruded by scattered Tertiary igneous rocks. The depositional environments of the Paleozoic and Mesozoic sedimen- tary rocks ranged from shallow marine to near shore-terrestrial. Study of the various sandstones, shales, siltstones, dolomites and limestones indicate that these rocks were deposited in shallow marine environ- ments, tidal flats, sand dunes, carbonate platforms, and by rivers. -
Children's Catalog 2020-2021
CHILDREN’S CATALOG | 2020-2021 CONTENTS 01 New Titles 15 Juvenile Fiction 22 Juvenile Non Fiction 165 Sales Representatives 167 Title Index pages 174 Author Index pages 175 Order Info from Graham Nash OUR HOUSE BY GRAHAM NASH, ILLUSTRATED BY HUGH SYME, FOREWORD BY CAROLE KING more information on page 11! NEW TITLES The Generous Fish BY JACQUELINE JULES, ILLUSTRATED BY FRANCES TYRRELL Inspired by Jewish folklore, The Generous Fish is the story of a young boy named Reuven who takes a verse from scripture to “cast your bread upon the waters” (Ecclesiastes 11:1) quite literally. The result of his daily act is a giant talking fish with golden scales! Boy and fish spend idyllic days together until the villagers realize those scales are real gold. Every villager has good reason to ask for one. Devorah needs clothes for her children. Old Joseph needs money for a cane. The fish says he has plenty to share. But he grows weak from giving away too much, too fast. Can Reuven stand up to the village and save his friend? Jacqueline Jules is the author of forty books for young readers, including the award-winning Zapato Power series, Never Say a Mean Word Again: A Tale from Medieval Spain, and Feathers for Peacock. A former school librarian and teacher, Jacqueline enjoys visiting schools to share her passion for reading and writing. She is a word person, who loves rearranging words on the page, the same way people have fun fitting the pieces of a jigsaw puzzle together. Jacqueline lives in Arlington, Virginia. -
Black Hills – Mammoths, Monuments, Wagons and Wars
Black Hills – Mammoths, Monuments, Wagons and Wars July 7-11, 2021 Colorado School of Mines 2 graduate credits Cost: $420. With tuition. $325 without tuition. (Does not include lodging.) Day 1: Meet at Scotts Bluff, Nebraska at the Oregon Trail Museum and Visitors Center, at 8:00 a.m. Hike Oregon Trail Pathway along deep wagon wheel ruts along the Oregon Trail, while viewing replicates of many covered wagons that made the trek westward. Drive the historic Summit Road, which is the oldest paved road in Nebraska. Tour the Museum and Visitors Center to learn more about the people, the passions and the trials of the Oregon Trail. Scotts Bluff is the second most written about landmark in the numerous journals of the pioneer who followed the trail between 1841 and 1869. Continue our journey on the Oregon Trail to Chimney Rock, Jailhouse Rock and Courthouse Rock, which were all welcomed pinnacle landmarks along the trail through the wilderness of Nebraska. Travel back in time to the Miocene Geologic Epoch to Agate Fossils National Monument. Tour the fascinating visitor’s center to see dramatic displays of the ancient gigantic mammals that roamed the plains 23 to 5.3 million years ago. The Miocene is when two major ecosystems first appeared on Planet Earth, the kelp forest and the rolling grasslands. Hike a one mile Daemonelix Trail through ancient sand dunes to view fascinating petrified spiral burrows. What are the ”Devils Corkscrews” that so baffled early paleontologists? Were they created by spiraling tree roots or the shape claws of an extinct mammal? The visitor’s center also contains an extensive collection of Oglala Lakota Sioux artifacts, especially articles owned by Red Cloud, one of the major Sioux chiefs.