The Paleontology Synthesis Project and Establishing a Framework for Managing National Park Service Paleontological Resource Archives and Data
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Illinois Fossils Doc 2005
State of Illinois Illinois Department of Natural Resources Illinois Fossils Illinois Department of Natural Resources he Illinois Fossils activity book from the Illinois Department of Natural Resources’ (IDNR) Division of Education is designed to supplement your curriculum in a vari- ety of ways. The information and activities contained in this publication are targeted toT grades four through eight. The Illinois Fossils resources trunk and lessons can help you T teach about fossils, too. You will find these and other supplemental items through the Web page at https://www2.illinois.gov/dnr/education/Pages/default.aspx. Contact the IDNR Division of Education at 217-524-4126 or [email protected] for more information. Collinson, Charles. 2002. Guide for beginning fossil hunters. Illinois State Geological Survey, Champaign, Illinois. Geoscience Education Series 15. 49 pp. Frankie, Wayne. 2004. Guide to rocks and minerals of Illinois. Illinois State Geological Survey, Champaign, Illinois. Geoscience Education Series 16. 71 pp. Killey, Myrna M. 1998. Illinois’ ice age legacy. Illinois State Geological Survey, Champaign, Illinois. Geoscience Education Series 14. 67 pp. Much of the material in this book is adapted from the Illinois State Geological Survey’s (ISGS) Guide for Beginning Fossil Hunters. Special thanks are given to Charles Collinson, former ISGS geologist, for the use of his fossil illustrations. Equal opportunity to participate in programs of the Illinois Department of Natural Resources (IDNR) and those funded by the U.S. Fish and Wildlife Service and other agencies is available to all individuals regardless of race, sex, national origin, disability, age, reli-gion or other non-merit factors. -
FACT SHEET OVERVIEW Lower Cliff Dwelling Construction Sequence
southwestlearning.org TONTO Lower Cliff Dwelling FACTOVERVIEW SHEET Construction Sequence ARCHIVES SERVICE PARK NATIONAL Tonto National Monument, established in 1907, protects several cliff dwelling sites and numerous smaller archeo- logical sites scattered throughout the highlands and allu- vial plains within the Tonto Basin, Arizona. The Lower Cliff Dwelling is one of two large sites accessible to the public, and is the primary site visited in the Monument throughout the year. Background The Lower Cliff Dwelling consists of an approximately 20- room masonry and adobe village built within a natural al- cove above a side drainage of the Salt River called Cholla Canyon and overlooking Cave Canyon, where there is now an active spring. The site itself has been known since at The Lower Cliff Dwelling at Tonto National Monument, ca. 1905. least the late 1800s, and unfortunately, was subject to exces- sive looting and associated damage long before becoming a lage was not built all at once, however, and instead started Monument in 1907 and later coming under the protection of with only one or two rooms, to which additional rooms the National Park Service (NPS) in 1933. However, histor- were added over a period of perhaps 30 years (Nordby et ic photographs, excavation and stabilization records (e.g., al. 2012). New rooms were built on bedrock, artificially Duffen 1937; Pierson 1952), and recent research provide leveled floors, and accumulated trash. While the rocks and some indication of when and how the Lower Cliff Dwelling clay for the adobe were readily available (Nordby et al. was constructed, and to some extent, by whom. -
Fossil Collecting Areas in Iowa
FOSSIL COLLECTING AREAS IN IOWA The following list, although far from compete, includes a few of the better fossil collecting areas in Iowa. 1. Rockford, Floyd County (¼ mile south and ¼ mile west of the Rockford Brick and Tile Company pit, on county road “D”). Well preserved brachiopods, gastropods, and corals are most abundant in the yellowish shales that overlie the blue-gray beds. The fossils occurring here are known as the Hackberry fauna and have been described by C.L. and M.A. Fenton in a book entitled, “The Hackberry State of the Upper Devonian,” published by the MacMillan Company in 1924. 2. Bird Hill, Cerro Gordo County This is near the center of the north line of section 24, T 95N, R.19W, about 3½ miles west and ¼ mile south of the Rockford Brick and Tile Company Plant. The Hackberry fauna can be collected here also. 3. Elgin-Clermont area, Fayette County In the Elgin Member of the Maquoketa Formation large trilobites and both straight and coiled cephalopods are found. Fragments of trilobites are common, but whole specimens are rare. Road cuts along the new highway between Clermont and Elgin, the dry stream bed along county road “Y” east of Clermont, and the high-road cuts along the Turkey River southeast of Elgin are all good collecting sites. References for this area are: (1) Slocum, A.W., “Trilobites from the Maquoketa Beds of Fayette County, Iowa,” Iowa Geological Survey Annual Report, Volume 25; (2) Walter, O.T., “Trilobites of Iowa and some Related Paleozoic Forms,” Iowa Geological Survey Annual Report, Volume 31; (3) Ladd, H.S., “Stratigraphy and Paleontology of the Maquoketa Shale of Iowa,” Iowa Geological Survey Annual Report, Volume 34. -
Tonto National Monument News Release
National Park Service Tonto National Monument U.S. Department of the Interior 26260 N. AZ Hwy. 188, Lot 2 Roosevelt, AZ 85545 928-467-2241 phone www.nps.gov/tont Tonto National Monument News Release Release date: Immediate Contact: Hilary Clark Phone number: (928) 467-2241 Email: [email protected] Date: April 28, 2017 Tourism to Tonto National Monument Creates 3, 155,800 in Economic Benefits Report shows visitor spending supports 33 jobs in local economy Roosevelt, AZ – A new National Park Service (NPS) report shows that in 2016, 38,048 visitors to Tonto National Monument spent $2, 224,600 in communities near the park. This visitor spending supported 33 jobs in the local area and had a cumulative benefit to the local economy of $3,155,800. “Tonto National Monument welcomes our local visitors and others from around the world,” said Superintendent Duane Hubbard. “We are delighted to share the story of Salado cliff dwellings and prehistoric artifacts that have been preserved for over 700 years. National park tourism is a significant driver in the national economy, returning more than $10 for every $1 invested in the National Park Service, and it’s a big factor in the Gila County economy as well. We appreciate the partnership and support of our neighbors and are glad to be able to give back by helping to sustain local communities.” The peer-reviewed visitor spending analysis was conducted by economists Catherine Cullinane Thomas of the U.S. Geological Survey and Lynne Koontz of the National Park Service. The report shows $18.4 billion of direct spending by 331 million park visitors in communities within 60 miles of a national park. -
417 US National Parks, Historical Sites, Preserves, Seashores and More!
417 US National Parks, Historical Sites, Preserves, Seashores and more! Alabama o Birmingham Civil Rights National Monument o Freedom Riders National Monument o Horseshoe Bend National Military Park o Little River Canyon National Preserve o Russell Cave National Monument o Tuskegee Airmen National Historic Site o Tuskegee Institute National Historic Site Alaska o Alagnak Wild River o Aniakchak National Monument o Aniakchak National Preserve o Bering Land Bridge National Preserve o Cape Krusenstern National Monument o Denali National Park o Denali National Preserve o Gates of the Arctic National Park o Gates of the Arctic National Preserve o Glacier Bay National Park o Glacier Bay National Preserve o Katmai National Park o Katmai National Preserve o Kenai Fjords National Park o Klondike Gold Rush National Historical Park (also Washington) o Kobuk Valley National Park o Lake Clark National Park o Lake Clark National Preserve o Noatak National Preserve o Sitka National Historical Park o World War II Valor in the Pacific National Monument (also California, Hawaii) o Wrangell-St. Elias National Park o Wrangell-St. Elias National Preserve o Yukon-Charley Rivers National Preserve Courtesy of ParkRangerJohn.com Arizona o Canyon De Chelly National Monument o Casa Grande Ruins National Monument o Chiricahua National Monument o Coronado National Memorial o Fort Bowie National Historic Site o Glen Canyon National Recreation Area (also Utah) o Grand Canyon National Park o Hohokam Pima National Monument o Hubbel Trading Post National Historic Site -
National Park Service Mission 66 Era Resources B
NPS Form 10-900-b (Rev. 01/2009) 0MB No. 1024-0018 (Expires 5/31/2012) UNITED STATES DEPARTMENT OF THE INTERIOR National Park Service National Register of Historic Places Multiple Property Documentation Form This form Is used for documenting property groups relating to one or several historic contexts. See instructil'.r!§ ~ ~ tloDpl lj~~r Bulletin How to Complete the Mulliple Property Doc11mentatlon Form (formerly 16B). Complete each item by entering the req lBtEa\oJcttti~ll/~ a@i~8CPace, use continuation sheets (Form 10-900-a). Use a typewriter, word processor, or computer to complete all items X New Submission Amended Submission AUG 1 4 2015 ---- ----- Nat Register of Historie Places A. Name of Multiple Property Listing NatioAal Park Service National Park Service Mission 66 Era Resources B. Associated Historic Contexts (Name each associated historic context, identifying theme, geographical area, and chronological period for each.) Pre-Mission 66 era, 1945-1955; Mission 66 program, 1956-1966; Parkscape USA program, 1967-1972, National Park Service, nation-wide C. Form Prepared by name/title Ethan Carr (Historical Landscape Architect); Elaine Jackson-Retondo, Ph.D., (Historian, Architectural); Len Warner (Historian). The Collaborative Inc.'s 2012-2013 team comprised Rodd L. Wheaton (Architectural Historian and Supportive Research), Editor and Contributing Author; John D. Feinberg, Editor and Contributing Author; and Carly M. Piccarello, Editor. organization the Collaborative, inc. date March 2015 street & number ---------------------2080 Pearl Street telephone 303-442-3601 city or town _B_o_ul_d_er___________ __________st_a_te __ C_O _____ zi~p_c_o_d_e_8_0_30_2 __ _ e-mail [email protected] organization National Park Service Intermountain Regional Office date August 2015 street & number 1100 Old Santa Fe Trail telephone 505-988-6847 city or town Santa Fe state NM zip code 87505 e-mail sam [email protected] D. -
Lithostratigraphic Mapping Through Saprolitic Regolith Using Soil Geochemistry and High-Resolution Aeromagnetic Surveys
EGU2020-20242 https://doi.org/10.5194/egusphere-egu2020-20242 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Lithostratigraphic Mapping Through Saprolitic Regolith Using Soil Geochemistry and High-Resolution Aeromagnetic Surveys. Helen Twigg and Murray Hitzman iCRAG, School of Earth Sciences, University College Dublin, Belfield, Dublin, Ireland The Neoproterozoic Central African Copperbelt located in southern Democratic Republic of Congo (DRC) and the northwestern Zambia and contains 48% of the world’s cobalt reserves and significant resources of copper, zinc, nickel and gold. A good understanding of the geology is critical for successful mineral exploration. However, geological mapping is hindered by low topographic relief, limited outcrop, and a generally deep (10-100m) weathering profile developed since the Late Miocene. Multielement soil geochemistry provides a means for conducting geological mapping. Areas with outcrop or containing drill holes and/or trenches were utilized to relate known geological lithologies with soil geochemical results using major element and trace element ratios. The lithostratigraphy within a study area along the DRC-Zambia border can be geochemically sub- divided into three units. Mixed carbonate and siliciclastic lithologies of the lower portion of the local stratigraphy are typically characterised by elevated V, Ti, and Nb. Mudstones and siltstones are dominated by elevated Al, Fe and Ba. The upper portion of the local stratigraphy is geochemically neutral with regards to trace elements. Lithological discrimination through analysis of soil geochemical data is limited in some areas by intense weathering. A A-CNK-FM diagram exhibits how complete weathering of carbonate rocks and carbonate-rich breccias (after evaporites) results in the somewhat counter intuitive outcome that residual soils above carbonate rocks are amongst the most aluminum rich in the study area with >80% Al2O3 (mol%) or >80% combined Al2O3 (mol%) and FeO + MgO (mol%). -
Some Philosophical Questions About Paleontology and Their Practica1 Consequences
ACTA GEOLOGICA HISPANICA. Concept and method in Paleontology. 16 (1981) nos 1-2, pags. 7-23 Some philosophical questions about paleontology and their practica1 consequences by Miquel DE RENZI Depto. de Geología, Facultad de Ciencias Biológicas, Universidad de Valencia. Burjassot (Valencia). This papcr attempts to objectively discuss the actual state ofpaleontology. The En aquest treball s'ha intentat fer un balanc d'alguns aspectes de I'estat de la progress of this science stood still somewhat during the latter part of the last paleontologia. La historia de la paleontologia mostra un estancarnent a les century which caused it to develop apart from the biological sciences. an area to darreries del segle passac aquest estancament va Fer que la nostra ciencia s'anes which it is naturally tied. As aconsequence, this bruought a long-term stagnation, allunyant cada cop mes de I'area de les ciencies bii~logiques,amb les qualsestava because biology, dunng this century, has made great progress and paleontology lligada naturalment AixO va portar, com a conseqüencia, un important has not During the last 20 years paleontology as a science hasrecuperatedsome endarreriment, car la biologia, durant aquest segle, ha donat un gran pas of this loss, but we as scientists need to be careful in various aspects of its endavant, mentre que aquest no ha estat el cas de lapaleontologia Al nostre pais development -i possiblement a molts d'altres- la paleontologia es, fonamentalment, un estn per datar estrats. Tanmateix, un mal estri, car la datació es basadaen les especies fossils i la seva determinació es fonamenta en el ccncepte d'especie biolbgica; els fossils pero en moltes ocasions, són utilitzats mes aviat com si fossin segells o monedes. -
Mary Anning of Lyme Regis: 19Th Century Pioneer in British Palaeontology
Headwaters Volume 26 Article 14 2009 Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology Larry E. Davis College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/headwaters Part of the Geology Commons, and the Paleontology Commons Recommended Citation Davis, Larry E. (2009) "Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology," Headwaters: Vol. 26, 96-126. Available at: https://digitalcommons.csbsju.edu/headwaters/vol26/iss1/14 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in Headwaters by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. LARRY E. DAVIS Mary Anning of Lyme Regis 19th Century Pioneer in British Palaeontology Ludwig Leichhardt, a 19th century German explorer noted in a letter, “… we had the pleasure of making the acquaintance of the Princess of Palaeontology, Miss Anning. She is a strong, energetic spinster of about 28 years of age, tanned and masculine in expression …” (Aurousseau, 1968). Gideon Mantell, a 19th century British palaeontologist, made a less flattering remark when he wrote in his journal, “… sallied out in quest of Mary An- ning, the geological lioness … we found her in a little dirt shop with hundreds of specimens piled around her in the greatest disorder. She, the presiding Deity, a prim, pedantic vinegar looking female; shred, and rather satirical in her conversation” (Curwin, 1940). Who was Mary Anning, this Princess of Palaeontology and Geological Lioness (Fig. -
Historical Development and Problems Within the Pennsylvanian Nomenclature of Ohio.1
Historical Development and Problems Within the Pennsylvanian Nomenclature of Ohio.1 GLENN E. LARSEN, OHIO Department of Natural Resources, Division of Geological Survey, Fountain Sq., Bldg. B, Columbus, OH 43224 ABSTRACT. An analysis of the historical development of the Pennsylvanian stratigraphic nomenclature, as used in Ohio, has helped define and clarify problems inherent in Ohio's stratigraphic nomenclature. Resolution of such problems facilitates further development of a useful stratigraphy and philosophy for mapping. Investigations of Pennsylvanian-age rocks in Ohio began as early as 1819- From 1858 to 1893, investigations by Newberry, I. C. White, and Orton established the stratigraphic framework upon which the present-day nomenclature is based. During the 1950s, the cyclothem concept was used to classify and correlate Pennsylvanian lithologic units. This classification led to a proliferation of stratigraphic terms, as almost every lithologic type was named and designated as a member of a cyclothem. By the early 1960s, cyclothems were considered invalid as a lithostratigraphic classification. Currently, Pennsylvanian nomenclature of Ohio, as used by the Ohio Division of Geological Survey, consists of four groups containing 123 named beds, with no formal formations or members. In accordance with the 1983 North American Stratigraphic code, the Ohio Division of Geological Survey considers all nomenclature below group rank as informal. OHIO J. SCI. 91 (1): 69-76, 1991 INTRODUCTION DISCUSSION Understanding the historical development of Pennsyl- The Early 1800s vanian stratigraphy in Ohio is important to the Ohio The earliest known references to Pennsylvanian-age Division of Geological Survey (OGS). Such an under- rocks in Ohio are found in Atwater's (1819) report on standing of Pennsylvanian stratigraphy helps define Belmont County, and an article by Granger (1821) on plant stratigraphic nomenclatural problems in order to make fossils collected near Zanesville, Muskingum County. -
Fossil Collecting in Ohio
No. 17 OHIOGeoFacts DEPARTMENT OF NATURAL RESOURCES • DIVISION OF GEOLOGICAL SURVEY FOSSIL COLLECTING IN OHIO Hobbyists have long known about Ohio’s great abundance and WHERE FOSSILS ARE FOUND IN OHIO diversity of fossils. Many world-famous paleontologists—geologists who study fossils—began their careers as youngsters collecting fossils Ordovician rocks in Ohio are world famous for in their native Ohio. Fossils from Ohio are important constituents the abundance, variety, and excellent preserva- of museum collections throughout the United States and Europe. tion of the fossils they contain. The limestones and shales exposed in almost every road cut or WHY OHIO HAS FOSSILS stream bed in southwestern Ohio, southeastern Indiana, and north-central Kentucky provide The area that is now Ohio was not always dry land as it is today. the opportunity to collect a bonanza of fossils. Approximately 510 million years ago (m.y.a.), Ohio was south of the Among the more abundant types of fossils col- Equator. As the North American Plate moved to its current position ORDOVICIAN lected from Ordovician rocks are brachiopods, 508–438 m.y.a. through the process of plate tectonics, tropical to subtropical seas bryozoans, gastropods, and trilobites. repeatedly transgressed over the plate. It is because of those warm Silurian rocks of western Ohio are not known seas that Ohio has the abundant fossils that people collect today. for their fossils. When the limestones and shales The seas that covered Ohio during the Ordovician, Silurian, and were fi rst deposited they were quite fossilifer- most of the Devonian Periods of the Paleozoic Era were the site of ous. -
Stratigraphical Framework for the Devonian (Old Red Sandstone) Rocks of Scotland South of a Line from Fort William to Aberdeen
Stratigraphical framework for the Devonian (Old Red Sandstone) rocks of Scotland south of a line from Fort William to Aberdeen Research Report RR/01/04 NAVIGATION HOW TO NAVIGATE THIS DOCUMENT ❑ The general pagination is designed for hard copy use and does not correspond to PDF thumbnail pagination. ❑ The main elements of the table of contents are bookmarked enabling direct links to be followed to the principal section headings and sub-headings, figures, plates and tables irrespective of which part of the document the user is viewing. ❑ In addition, the report contains links: ✤ from the principal section and sub-section headings back to the contents page, ✤ from each reference to a figure, plate or table directly to the corresponding figure, plate or table, ✤ from each figure, plate or table caption to the first place that figure, plate or table is mentioned in the text and ✤ from each page number back to the contents page. Return to contents page NATURAL ENVIRONMENT RESEARCH COUNCIL BRITISH GEOLOGICAL SURVEY Research Report RR/01/04 Stratigraphical framework for the Devonian (Old Red Sandstone) rocks of Scotland south of a line from Fort William to Aberdeen Michael A E Browne, Richard A Smith and Andrew M Aitken Contributors: Hugh F Barron, Steve Carroll and Mark T Dean Cover illustration Basal contact of the lowest lava flow of the Crawton Volcanic Formation overlying the Whitehouse Conglomerate Formation, Trollochy, Kincardineshire. BGS Photograph D2459. The National Grid and other Ordnance Survey data are used with the permission of the Controller of Her Majesty’s Stationery Office. Ordnance Survey licence number GD 272191/2002.