65Th Annual Tri-State Geological Field Conference 2-3 October 2004
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Interpretation of Cumberland Escarpment and Highland Rim, South-Central Tennessee and Northeast Alabama
Interpretation of Cumberland Escarpment and Highland Rim, South-Central Tennessee and Northeast Alabama GEOLOGICAL SURVEY PROFESSIONAL PAPER 524-C Interpretation of Cumberland Escarpment and Highland Rim, South-Central Tennessee and Northeast Alabama By JOHN T. HACK SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 524-C Theories of landscape origin are compared using as an example an area of gently dipping rocks that differ in their resistance to erosion UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1966 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract___________________________________________ C1 Cumberland Plateau and Highland Rim as a system in Introduction_______________________________________ 1 equilibrium______________________________________ C7 General description of area___________________________ 1 Valleys and coves of the Cumberland Escarpment___ 7 Cumberland Plateau and Highland Rim as dissected and Surficial deposits of the Highland Rim____________ 10 deformed peneplains _____________________ ,... _ _ _ _ _ _ _ _ 4 Elk River profile_______________________________ 12 Objections to the peneplain theory____________________ 5 Paint Rock Creek profile________________________ 14 Eastern Highland Rim Plateau as a modern peneplain__ 6 Conclusions________________________________________ 14 Equilibrium concept -
When the Mountain Became the Escarpment.FH11
Looking back... with Alun Hughes WHEN THE MOUNTAIN BECAME THE ESCARPMENT The Niagara Escarpment hasnt always been But Coronelli was not the first to put Niagara known by that name. Early in the 19th century it on the map. That distinction belongs to Father Louis was often referred to as the Mountain, and of course Hennepin, the Recollect priest who was the first it is still called that in Hamilton and Grimsby today. European to describe Niagara Falls from personal We in eastern Niagara have largely forgotten the observation. In his Description de la Louisiane, name, though it survives in the City of Thorolds published in 1683, five years after his visit, he speaks motto Where the Ships Climb the Mountain. of le grand Sault de Niagara, and labels it thus on the accompanying map. This is the form that So when did the name Niagara Escarpment first prevails thereafter, and it is the spelling used for Fort come into use? And what about the areas other de Niagara, established by the French at the mouth Niagara names, like Niagara Falls, Niagara River of the river in 1726. The English followed suit, and Niagara Peninsula? When did these first appear? though on many early maps (e.g. Moll 1715, I dont pretend to have definitive answers there Mitchell 1782) they use the name Great Fall of are too many sources I have not seen but I can Niagara rather than Niagara Falls. suggest some preliminary conclusions. In his Description Hennepin also refers to la The name Niagara is definitely of native origin, belle Riviere de Niagara, so the name Niagara though there is no agreement about its meaning. -
Post-Carboniferous Stratigraphy, Northeastern Alaska by R
Post-Carboniferous Stratigraphy, Northeastern Alaska By R. L. DETTERMAN, H. N. REISER, W. P. BROSGE,and]. T. DUTRO,JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 886 Sedirnentary rocks of Permian to Quaternary age are named, described, and correlated with standard stratigraphic sequences UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Detterman, Robert L. Post-Carboniferous stratigraphy, northeastern Alaska. (Geological Survey Professional Paper 886) Bibliography: p. 45-46. Supt. of Docs. No.: I 19.16:886 1. Geology-Alaska. I. Detterman, Robert L. II. Series: United States. Geological Survey. Professional Paper 886. QE84.N74P67 551.7'6'09798 74-28084 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02687-2 CONTENTS Page Page Abstract __ _ _ _ _ __ __ _ _ _ _ _ _ _ _ _ _ _ _ __ __ _ _ _ _ _ _ __ __ _ _ __ __ __ _ _ _ _ __ 1 Stratigraphy__:_Continued Introduction __________ ----------____ ----------------____ __ 1 Kingak Shale ---------------------------------------- 18 Purpose and scope ----------------------~------------- 1 Ignek Formation (abandoned) -------------------------- 20 Geographic setting ------------------------------------ 1 Okpikruak Formation (geographically restricted) ________ 21 Previous work and acknowledgments ------------------ 1 Kongakut Formation ---------------------------------- -
Vegetation and Fire at the Last Glacial Maximum in Tropical South America
Past Climate Variability in South America and Surrounding Regions Developments in Paleoenvironmental Research VOLUME 14 Aims and Scope: Paleoenvironmental research continues to enjoy tremendous interest and progress in the scientific community. The overall aims and scope of the Developments in Paleoenvironmental Research book series is to capture this excitement and doc- ument these developments. Volumes related to any aspect of paleoenvironmental research, encompassing any time period, are within the scope of the series. For example, relevant topics include studies focused on terrestrial, peatland, lacustrine, riverine, estuarine, and marine systems, ice cores, cave deposits, palynology, iso- topes, geochemistry, sedimentology, paleontology, etc. Methodological and taxo- nomic volumes relevant to paleoenvironmental research are also encouraged. The series will include edited volumes on a particular subject, geographic region, or time period, conference and workshop proceedings, as well as monographs. Prospective authors and/or editors should consult the series editor for more details. The series editor also welcomes any comments or suggestions for future volumes. EDITOR AND BOARD OF ADVISORS Series Editor: John P. Smol, Queen’s University, Canada Advisory Board: Keith Alverson, Intergovernmental Oceanographic Commission (IOC), UNESCO, France H. John B. Birks, University of Bergen and Bjerknes Centre for Climate Research, Norway Raymond S. Bradley, University of Massachusetts, USA Glen M. MacDonald, University of California, USA For futher -
Triassic- Jurassic Stratigraphy Of
Triassic- Jurassic Stratigraphy of the <JF C7 JL / Culpfeper and B arbour sville Basins, VirginiaC7 and Maryland/ ll.S. PAPER Triassic-Jurassic Stratigraphy of the Culpeper and Barboursville Basins, Virginia and Maryland By K.Y. LEE and AJ. FROELICH U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1472 A clarification of the Triassic--Jurassic stratigraphic sequences, sedimentation, and depositional environments UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1989 DEPARTMENT OF THE INTERIOR MANUEL LUJAN, Jr., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging in Publication Data Lee, K.Y. Triassic-Jurassic stratigraphy of the Culpeper and Barboursville basins, Virginia and Maryland. (U.S. Geological Survey professional paper ; 1472) Bibliography: p. Supt. of Docs. no. : I 19.16:1472 1. Geology, Stratigraphic Triassic. 2. Geology, Stratigraphic Jurassic. 3. Geology Culpeper Basin (Va. and Md.) 4. Geology Virginia Barboursville Basin. I. Froelich, A.J. (Albert Joseph), 1929- II. Title. III. Series. QE676.L44 1989 551.7'62'09755 87-600318 For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 CONTENTS Page Page Abstract.......................................................................................................... 1 Stratigraphy Continued Introduction... .......................................................................................... -
For: the City of Verona, Wisconsin
RESOURCE ASSESSMENT AND DEVELOPMENT ANALYSIS FOR THE THE UPPER SUGAR RIVER AND BADGER MILL CREEK SOUTHWEST OF VERONA, WI JUNE 2008 PROJECT NO. 1297 FOR: THE CITY OF VERONA, WISCONSIN TABLE OF CONTENTS 1. INTRODUCTION .................................................................................................1 1.1 Purpose of Study.............................................................................................................. 1 1.2 Study Area Description .................................................................................................. 1 1.3 Background to key water resource issues .................................................................... 2 1.4 Study Approach............................................................................................................... 3 1.5 Study Participants............................................................................................................ 4 2 EXISTING DATA REVIEW ..................................................................................5 2.1 Fisheries ............................................................................................................................ 5 2.2 Macroinvertebrates.......................................................................................................... 9 2.3 Water Quality................................................................................................................. 12 2.4 Streamflow......................................................................................................................14 -
Living on the Edge
Living on the Ledge Life in Eastern Wisconsin Outline • Location of Niagara Escarpment Eastern U.S. • General geology • Locations of the escarpment in Wisconsin • Neda Iron mine and early geologists • Silurian Dolostone of Waukesha Co.- Lannon Stone , past and present quarries • The Great Lakes Watershed Niagara Falls NY – Rock falls caused by undercutting: notice the pile of broken rock at base of American falls. Top Layer is equivalent to Waukesha/ Lannon Stone You may have see Niagara Falls locally if you visited the Hudson River painters exhibit at MAM. Fredrick Church 1867 Fredrick Church 1857 Or you can see a bit of the Ledge as a table top while meditating with a bottle of Silurian Stout in my yard Fr. Louis Hennepin sketch of Niagara Falls 1698 Niagara Falls - the equivalent stratigraphic section in N.Y. from which the correlation of the Neda to the Clinton Iron was incorrectly made Waterfalls associated with the Niagara Escarpment all follow this pattern- resistant cap rock and soft shale underneath The “Ledge” of Western NY The Niagara Escarpment Erie Canal locks at Lockport NY The Erie Canal that followed the lowland until it reached the Niagara Escarpment The names of Silurian rocks in the Midwestern states change with location and sometimes with authors! 417mya Stratigraphic column for rocks of Eastern Wisconsin. 443mya Note the Niagara Escarpment rocks at the top. The Escarpment is the result of resistant dolostone 495mya cap rock and soft shale rock below The Michigan Basin- Showing outcrops of Silurian rocks Location of major Silurian Outcrops in Eastern Wisconsin Peninsula Park from both top and bottom Ephraim Sven’s Overlook Door County – Fish Creek Niagara Escarpment in the background Door Co Shoreline Cave Point near Jacksonport - Door Co Cave Point - 2013 Cave Point - Door Co - 2013 during low lake levels Jean Nicolet 1634 overlooking Green Bay WI while standing on the Ledge Wequiock Falls near Green Bay WI. -
Stratigraphy and Correlation of Glacial Deposits of the Rocky Mountains, the Colorado Plateau and the Ranges of the Great Basin
STRATIGRAPHY AND CORRELATION OF GLACIAL DEPOSITS OF THE ROCKY MOUNTAINS, THE COLORADO PLATEAU AND THE RANGES OF THE GREAT BASIN Gerald M. Richmond u.s. Geological Survey, Box 25046, Federal Center, MS 913, Denver, Colorado 80225, U.S.A. INTRODUCTION glaciations (Charts lA, 1B) see Fullerton and Rich- mond, Comparison of the marine oxygen isotope The Rocky Mountains, Colorado Plateau, and Basin record, the eustatic sea level record, and the chronology and Range Provinces (Fig. 1) together occupy much of of glaciation in the United States of America (this the western interior United States. These regions volume). include approximately 140 mountain ranges that were glaciated during the Pleistocene. Most of the glaciers Historical Perspective were valley glaciers, but ice caps formed on uplands Following early recognition of deposits of two alpine locally. Discussion of the deposits of all of these ranges glaciations (Gilbert, 1890; Ball, 1908; Capps, 1909; would require monographic analysis. To avoid this, Atwood, 1909), deposits of three glaciations gradually representative ranges in each province are reviewed. became widely recognized (Alden, 1912, 1932, 1953; Atwood and Mather, 1912, 1932; Alden and Stebinger, Purpose and Scope 1913; Blackwelder, 1915; Atwood, 1915; Fryxell, 1930; This report summarizes the evidence for correlation Bradley, 1936). Subsequently drift of the intermediate of the Quaternary glacial deposits in 26 broadly glaciation was shown to represent two glacial advances distributed mountain ranges selected on the basis of (Fryxell, 1930; Horberg, 1938; Richmond, 1948, 1962a; availability of detailed information and length of glacial Moss, 1951a; Nelson, 1954; Holmes and Moss, 1955), record. and the older drift was shown to include deposits of Because the glacial deposits rarely are traceable from three glaciations (Richmond, 1957, 1962a, 1964a). -
Wisconsin Wisconsin
LAKE WINNEBAGO WATERSHED (WI) HUC:04030103 Wisconsin Wisconsin Rapid Watershed Assessment Lake Winnebago Watershed Rapid watershed assessments provide initial estimates of where conservation investments would best address the concerns of landowners, conservation districts, and other community organizations and stakeholders. These assessments help landowners and local leaders set priorities and determine the best actions to achieve their goals. Wisconsin October 2007 The United States Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, sex, religion, age, disability, political beliefs, sexual orientation, and marital or family status. (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 fi le a complaint of discrimination, write USDA, Director, Offi ce of Civil Rights, Room 326W, Whitten Building, 14th and Independence Avenue, SW, Washington DC 20250-9410, or call (202) 720-5964 (voice and TDD). USDA is an equal opportunity provider and employer. 1 LAKE WINNEBAGO WATERSHED (WI) HUC:04030103 CONTENTS o g a b e n n i W e k a L INTRODUCTION 3 COMMON RESOURCE AREA DESCRIPTION 4 ELEVATION MAP 5 LAND USE AND ANNUAL PRECIPITATION MAPS 6 ASSESSMENT OF WATERS 7 SOILS 9 DRAINAGE CLASSIFICATION 10 FARMLAND CLASSIFICATION 11 HYDRIC SOILS 12 LAND CAPABILITY CLASSIFICATION 13 PRS AND OTHER DATA 14 CENSUS AND SOCIAL DATA (RELEVANT) 15 ECOLOGICAL LANDSCAPE 16 RESOURCE CONCERNS 17 WATERSHED PROJECTS, 17 STUDIES, MONITORING, ETC WATERSHED ASSESSMENT 17 PARTNER GROUPS 18 FOOTNOTES/BIBLIOGRAPHY 19 2 LAKE WINNEBAGO WATERSHED (WI) HUC:04030103 1 INTRODUCTION The Lake Winnebago watershed is located in east central Wisconsin and surrounds the largest lake in the state, Lake Winnebago, which covers 137,708 acres. -
Exploring Wisconsin Geology
UW Green Bay Lifelong Learning Institute January 7, 2020 Exploring Wisconsin Geology With GIS Mapping Instructor: Jeff DuMez Introduction This course will teach you how to access and interact with a new online GIS map revealing Wisconsin’s fascinating past and present geology. This online map shows off the state’s famous glacial landforms in amazing detail using new datasets derived from LiDAR technology. The map breathes new life into hundreds of older geology maps that have been scanned and georeferenced as map layers in the GIS app. The GIS map also lets you Exploring Wisconsin Geology with GIS mapping find and interact with thousands of bedrock outcrop locations, many of which have attached descriptions, sketches, or photos. Tap the GIS map to view a summary of the surface and bedrock geology of the area chosen. The map integrates data from the Wisconsin Geological & Natural History Survey, the United States Geological Survey, and other sources. How to access the online map on your computer, tablet, or smart phone The Wisconsin Geology GIS map can be used with any internet web browser. It also works on tablets and on smartphones which makes it useful for field trips. You do not have to install any special software or download an app; The map functions as a web site within your existing web browser simply by going to this URL (click here) or if you need a website address to type in enter: https://tinyurl.com/WiscoGeology If you lose this web site address, go to Google or any search engine and enter a search for “Wisconsin Geology GIS Map” to find it. -
Geomorphological Studies of the Sedimentary Cuddapah Basin, Andhra Pradesh, South India
SSRG International Journal of Geoinformatics and Geological Science (SSRG-IJGGS) – Volume 7 Issue 2 – May – Aug 2020 Geomorphological studies of the Sedimentary Cuddapah Basin, Andhra Pradesh, South India Maheswararao. R1, Srinivasa Gowd. S1*, Harish Vijay. G1, Krupavathi. C1, Pradeep Kumar. B1 Dept. of Geology, Yogi Vemana University, Kadapa-516005, Andhra Pradesh, India Abstract: The crescent shaped Cuddapah basin located Annamalai Surface - at an altitude of over 8000’ (2424 mainly in the southern part of Andhra Pradesh and a m), ii. Ootacamund Surface – at 6500’-7500’ (1969- little in the Telangana State is one of the Purana 2272 m) on the west and at 3500’ (1060m) on the east basins. Extensive work was carried out on the as noticed in Tirumala hills, iii. Karnataka Surface - stratigraphy of the basin, but there is very little 2700’-3000’ (Vaidynathan, 1964). 2700-3300 reference (Vaidynathan,1964) on the geomorphology of (Subramanian, 1973) 2400-3000 (Radhakrishna, 1976), the basin. Hence, an attempt is made to present the iv. Hyderabad Surface – at 1600’ – 2000’v. Coastal geomorphology of the unique basin. The Major Surface – well developed east of the basin.vi. Fossil Geomorphic units correspond to geological units. The surface: The unconformity between the sediments of the important Physiographic units of the Cuddapah basin Cuddapah basin and the granitic basement is similar to are Palakonda hill range, Seshachalam hill range, ‘Fossil Surface’. Gandikota hill range, Velikonda hill range, Nagari hills, Pullampet valley and Kundair valley. In the Cuddapah Basin there are two major river systems Key words: Topography, Land forms, Denudational, namely, the Penna river system and the Krishna river Pediment zone, Fluvial. -
Hydrogeology of the Chinle Wash Watershed, Navajo Nation Arizona, Utah and New Mexico
Hydrogeology of the Chinle Wash Watershed, Navajo Nation Arizona, Utah and New Mexico Item Type Thesis-Reproduction (electronic); text Authors Roessel, Raymond J. Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 07/10/2021 19:50:22 Link to Item http://hdl.handle.net/10150/191379 HYDROGEOLOGY OF THE CHINLE WASH WATERSHED, NAVAJO NATION, ARIZONA, UTAH AND NEW MEXICO by Raymond J. Roessel A Thesis Submitted to the Faculty of the DEPARTMENT OF HYDROLOGY AND WATER RESOURCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE WITH A MAJOR IN HYDROLOGY In the Graduate College THE UNIVERSITY OF ARIZONA 1994 2 STATEMENT BY AUTHOR This thesis has been submitted in partial fulfillment of requirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this thesis are allowable without special permission, provided that accurate acknowledgment of source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the head of the major department or the Dean of the Graduate College when in his or her judgment the proposed use of the material is in the interests of scholarship. In all other instances, however, permission must be obtained from the author.