Geoarchaeological Summary of the Balcones Escarpment
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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. -
Geophysical Mapping of Mount Bonnell Fault of Balcones Fault Zone
Geophysical mapping of Mount Bonnell fault of Balcones fault zone and its implications on Trinity-Edwards Aquifer interconnection, central Texas, USA Mustafa Saribudak1 Abstract There are up to 1200 ft (365 m) of total displacement across the Geophysical surveys (resistivity, natural potential [self-po- BFZ. Faults generally dip steeply (45–85°), varying primarily tential], conductivity, magnetic, and ground penetrating radar) due to specific rock properties and local stress fields (Ferrill and were conducted at three locations across the Mount Bonnell fault Morris, 2008). in the Balcones fault zone of central Texas. The normal fault has The BFZ includes the Edwards and Trinity aquifers, which hundreds of meters of throw and is the primary boundary between are primary sources of water for south-central Texas communities, two major aquifers in Texas, the Trinity and Edwards aquifers. including the city of San Antonio. The Trinity Aquifer underlies In the near surface, the fault juxtaposes the Upper Glen Rose the Edwards Aquifer through the Balcones fault zone. Formation on the Edwards Plateau, consisting of interbedded The BFZ’s most prominent fault is the Mount Bonnell, with limestone and marly limestone, against the Edwards Group, which a vertical throw of up to 600 ft (183 m) (Figure 1). The fault is mostly limestone, on the eastern down-thrown side (coastal hydrogeologically juxtaposes these Cretaceous carbonate aquifers plain). The Upper Glen Rose member is considered to be the during the Miocene tectonic deformation associated with the Upper Trinity Aquifer and also a confining zone underlying the Balcones fault zone, where the younger Edwards Group limestone Edwards Aquifer. -
The Abyssal Giant Pockmarks of the Black Bahama Escarpment: Relations Between Structures, fluids and Carbonate Physiography” by Thibault Cavailhes Et Al
Solid Earth Discuss., https://doi.org/10.5194/se-2020-11-RC2, 2020 SED © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Interactive comment Interactive comment on “The abyssal giant pockmarks of the Black Bahama Escarpment: Relations between structures, fluids and carbonate physiography” by Thibault Cavailhes et al. Charles Paull (Referee) [email protected] Received and published: 10 April 2020 The manuscript describes a series of ∼circular depressions at the base of the Bahama Escarpment. These are curious features and their discovery may ultimately merit pub- lication. However, the manuscript more closely resembles a first draft, rather than a Printer-friendly version polished work. As is, the existing draft is too poorly written to fully follow many of the arguments in detail. Part of may be attributed to the challenge of writing in a second Discussion paper language. I have made some suggestions as to how to begin to sharpen the word- ing, but it is an incomplete effort. There are also a number of science related points C1 (also indicate below) that need to be considered before this could be recommended for publication. SED Why are these depressions called pockmarks from the outset? What is actually ob- served are approximately circular depressions. The term ‘pockmark’ has evolved to Interactive imply that the depression was somehow physically excavated by seepage, not phys- comment ical collapse. Moreover, it is not commonly been used in carbonate settings. The manuscript also refers to other similar depressions that have been previously been called plunge pools. This is yet another mechanism for surface erosion. -
1 a Film by Roger J. Kuhns What Was It Like in Door County Wisconsin 425 Million Years Ago? What
a film by Roger J. Kuhns www.rogerjameskuhns.com What was it like in Door County Wisconsin 425 million years ago? What has gone on in the geologic and biologic past beneath our feet? What are the changes we’re experiencing now? What might the future hold for our land, water, environment and communities? “Escarpment” is the natural history story of Eastern Wisconsin and the Niagara Escarpment region of the Great Lakes. The film was shot on location along the entire length of the Niagara Escarpment, with a Door County focus. It is a fast-paced fun voyage through billions of years of Eastern Wisconsin geologic and biologic past. The film reconstructs ecosystems that existed when the dolomitic rocks of the Niagara Escarpment were formed, considers if dinosaurs ever walked in what is now Door County, follows the path of glaciers, and many other major events in our rich geologic past. Locations around the world are featured to show what Eastern Wisconsin was like in the past. Animated sequences are used to illustrate parts of the story. The film helps to inform, enlighten, and guide us towards being better stewards of the land, and takes a glimpse of what a sustainable future might look like. In the spirit of Discovery Channel and National Geographic films, geologist and sustainologist Roger Kuhns produced this film for all ages. Kuhns has worked on the Niagara Escarpment and Great Lakes geology and ecology during the course of his career. FILM: Escarpment GENRE: Science / Nature / Travel PRODUCED BY: Roger J. Kuhns RUN TIME: 1 hour 33 minutes PRODUCTION: musicTOears Press CONTACT INFO: [email protected] / 860-910-8525 AVAILABLE AT: www.rogerjameskuhns.com MOVIE TRAILER: https://www.youtube.com/watch?v=YAyRp7VYFWs 1 2017-2018 Reviews from viewers of a film by Roger J. -
Historic Overview
Updated Reconnaissance Level Survey of Historic Resources Town of Amherst HISTORIC OVERVIEW LOCATION The Town of Amherst lies in northern Erie County, New York. It is bordered by Niagara County to the north, the Erie County towns of Clarence to the east, Cheektowaga to the south, and Tonawanda to the west. The total area of Amherst is approximately 53 square miles. ENVIRONMENTAL SETTING The natural environmental setting influenced prehistoric and historic settlement patterns in the Town of Amherst. The town lies within the Erie‐Ontario Lake Plain physiographic province, described as a nearly level lowland plain with few prominent topographic features. The area is underlain by Onondaga limestone dating to the Late Devonian period. Later glaciations shaped much of the western New York topography, including that of Amherst. One of the most prominent topographic features in the relatively featureless province is the Onondaga Escarpment, an east‐west trending hard limestone bedrock formation that lies in the southern portion of the Town of Amherst. The Onondaga Escarpment proved resistant to the effects of glacial scouring and it forms the southern boundary of a large basin once occupied by the shallow glacial Lake Tonawanda. Lake Tonawanda eventually receded leaving behind wetlands and deposits of clay and sand throughout much of northern Amherst (Owens et al. 1986:2). The most important drainages in the Town of Amherst are Tonawanda Creek, Ransom Creek, and Ellicott Creek. Tonawanda Creek forms the northern boundary between Amherst and Niagara County. It flows in a western direction and drains much of the eastern and Northern portions of Amherst. -
A RECREATIONAL USE SURVEY of the SAN MARCOS RIVER Thesis
A RECREATIONAL USE SURVEY OF THE SAN MARCOS RIVER Thesis Presented to the Graduate Council of Southwest Texas State University in Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE By David D Bradsby San Marcos, Texas May 1994 - A RECREATIONAL USE SURVEY OF THE SAN MARCOS RIVER Approved: B. G. Whiteside, Chairman Approved: TABLE OF CONTENTS List of Figures . i v List of Tables . vi Acknowledgements . vi i Introduction . 1 Recreational Literature Review . 2 San Marcos River . 6 Threatened and Endangered Species . 2 4 Methods . 27 Results.................................... 35 Discussion . 5 4 Conclusions . 6 9 Literature Cited . 7 2 iii LIST OF FIGURES Figure Page 1 . Map of the upper San Marcos River from Spring Lake to the Blanco River confluence ................ 7 2. Detailed map of the upper San Marcos River showing study areas ...... .... ..... ..... .. ... .. ....... ... .. ..... ......... ...... ... 9 3. Pepper's study area on the San Marcos River looking upstream .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. ... .. .. .. .. .. 1 1 4. Sewell Park study area on the San Marcos River looking downstream............................................................... 1 3 5. City Park study area on the San Marcos River ............ 1 5 6. Rio Vista Annex study area on the San Marcos River ........... ......... .... .... .... ......... ........ .... ......... ....... 1 7 7. Rio Vista Park study area on the San Marcos River ................ ......... ....... ..... .... ........ .... ........ -
April 2014 Midden
The Midden League City Rain Garden by Chris LaChance Galveston Bay Area Chapter - Texas Master Naturalists April 2014 Table of Contents President’s Corner by Maureen Nolan-Wilde, President 2014 Prairie Ponderings 2 Wetland Wanderings 2 In mid-January, current and former board members took part in a planning day at Julie Receives Award 4 Galveston Island State Park. The purpose of the day was to build on the Chapter’s accomplishments, identify opportunities and help plan for the future. 2014 Plant of the Yr. 4 Early People of Texas 6 We developed a “roadmap” that can be used to set goals and focus our efforts for 2014 and beyond. We identified the following areas where we can make immediate Heritage Book Study - 6 improvements: Review Membership 7 Succession planning for key roles (learning exactly what board members and Outreach Survey committee chairs do so that, in the future, this knowledge isn’t lost), Coastal Mammals AT 7 Pelican AT 8 Leveraging current technologies (for example, making better use of the website, social media and tools for sending messages to our members), Diurnal Raptors AT 9 GBA Clan 10 Growing our outreach efforts (such as stewardship and education in schools). WaterSmart Award 12 Since that meeting, we have launched an image database that contains over 1,000 GBAC 1st Camp Out 12 pictures and has been viewed more than 10,200 times. This database, which is easily 2014 Class Fun 14 accessible and can be viewed 24/7, is a great example of using technology to make us more efficient and effective. -
MEXICO Las Moras Seco Creek K Er LAVACA MEDINA US HWY 77 Springs Uvalde LEGEND Medina River
Cedar Creek Reservoir NAVARRO HENDERSON HILL BOSQUE BROWN ERATH 281 RUNNELS COLEMAN Y ANDERSON S HW COMANCHE U MIDLAND GLASSCOCK STERLING COKE Colorado River 3 7 7 HAMILTON LIMESTONE 2 Y 16 Y W FREESTONE US HW W THE HIDDEN HEART OF TEXAS H H S S U Y 87 U Waco Lake Waco McLENNAN San Angelo San Angelo Lake Concho River MILLS O.H. Ivie Reservoir UPTON Colorado River Horseshoe Park at San Felipe Springs. Popular swimming hole providing relief from hot Texas summers. REAGAN CONCHO U S HW Photo courtesy of Gregg Eckhardt. Y 183 Twin Buttes McCULLOCH CORYELL L IRION Reservoir 190 am US HWY LAMPASAS US HWY 87 pasas R FALLS US HWY 377 Belton U S HW TOM GREEN Lake B Y 67 Brady iver razos R iver LEON Temple ROBERTSON Lampasas Stillhouse BELL SAN SABA Hollow Lake Salado MILAM MADISON San Saba River Nava BURNET US HWY 183 US HWY 190 Salado sota River Lake TX HWY 71 TX HWY 29 MASON Buchanan N. San G Springs abriel Couple enjoying the historic mill at Barton Springs in 1902. R Mason Burnet iver Photo courtesy of Center for American History, University of Texas. SCHLEICHER MENARD Y 29 TX HW WILLIAMSON BRAZOS US HWY 83 377 Llano S. S an PECOS Gabriel R US HWY iver Georgetown US HWY 163 Llano River Longhorn Cavern Y 79 Sonora LLANO Inner Space Caverns US HW Eckert James River Bat Cave US HWY 95 Lake Lyndon Lake Caverns B. Johnson Junction Travis CROCKETT of Sonora BURLESON 281 GILLESPIE BLANCO Y KIMBLE W TRAVIS SUTTON H GRIMES TERRELL S U US HWY 290 US HWY 16 US HWY P Austin edernales R Fredericksburg Barton Springs 21 LEE Somerville Lake AUSTIN Pecos -
Geological Society of America Bulletin
Downloaded from gsabulletin.gsapubs.org on January 11, 2012 Geological Society of America Bulletin Structural framework of the Edwards Aquifer recharge zone in south-central Texas David A. Ferrill, Darrell W. Sims, Deborah J. Waiting, Alan P. Morris, Nathan M. Franklin and Alvin L. Schultz Geological Society of America Bulletin 2004;116, no. 3-4;407-418 doi: 10.1130/B25174.1 Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Geological Society of America Bulletin Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. -
65Th Annual Tri-State Geological Field Conference 2-3 October 2004
65th Annual Tri-State Geological Field Conference 2-3 October 2004 Weis Earth Science Museum Menasha, Wisconsin The Lake & The Ledge Geological Links between the Niagara Escarpment and Lake Winnebago Joanne Kluessendorf & Donald G. Mikulic Organizers The Lake & The Ledge Geological Links between the Niagara Escarpment and Lake Winnebago 65th Annual Tri-State Geological Field Conference 2-3 October 2004 by Joanne Kluessendorf Weis Earth Science Museum, Menasha and Donald G. Mikulic Illinois State Geological Survey, Champaign With contributions by Bruce Brown, Wisconsin Geological & Natural History Survey, Stop 1 Tom Hooyer, Wisconsin Geological & Natural History Survey, Stops 2 & 5 William Mode, University of Wisconsin-Oshkosh, Stops 2 & 5 Maureen Muldoon, University of Wisconsin-Oshkosh, Stop 1 Weis Earth Science Museum University of Wisconsin-Fox Valley Menasha, Wisconsin WELCOME TO THE TH 65 ANNUAL TRI-STATE GEOLOGICAL FIELD CONFERENCE. The Tri-State Geological Field Conference was founded in 1933 as an informal geological field trip for professionals and students in Iowa, Illinois and Wisconsin. The first Tri-State examined the LaSalle Anticline in Illinois. Fifty-two geologists from the University of Chicago, University of Iowa, University of Illinois, Northwestern University, University of Wisconsin, Northern Illinois State Teachers College, Western Illinois Teachers College, and the Illinois State Geological Survey attended that trip (Anderson, 1980). The 1934 field conference was hosted by the University of Wisconsin and the 1935 by the University of Iowa, establishing the rotation between the three states. The 1947 Tri-State visited quarries at Hamilton Mound and High Cliff, two of the stops on this year’s field trip. -
San Marcos Recovery Plan
~""'.- San Marcos Recovery Plan U. • Fish & Wildlife Service Albu,querque, New Mexico .-1-934--- The San Marcos Recovery Plan FOR San Hareqs River, Endangered and Threatened Species San ,Marcos Gambusia (Gambusia georgei) Hubbs and Peden ~ountainDarter (Etheostoma fonticola) (Jordan and Gilbert) San Marcos Salamander (Eurycea nana) Bish~p Te1,Ca s Wildr ice" (Z.tzaniatexana}Hitchcock PREPARED BY THE SAN MARIDS REIDVERY TEAM Dr. Robert J. Edwards, Leader, Pan American University, Edinburg, Texas 78539 Mr. Harold E. Beaty, 3414 Forest Trail, Temple, Texas 76502 Dr. Glenn Longley, Southwest Texas State University, San Marcos, Texas 78666 Mr. David H. Riskind, Texas Parks and Wildlife Department, Austin, Texas 78744 Dr. Dianna D.Tupa, center for Research and Water Resources, Unlvers1tyof Texas Balcones Research' Center, Austin, Texas 78758 Dr. Bobby G.Whites ide, Southwes t Texas State University, San Marcos, Texas 78666 OONSULTANTS Mr. Harry Bishop, USFWS, Fish Cult. & Develop. Res. Center, San Marcos, Texas 78666 Dr. W. H. P. Emery, South~est Texas State University, San Marcos, Texas 7e666 (Member 1981-82) Mr. Russell L. Masters, Edwards Underground Water District, San AntoniO, Texas 78205 Mr. William McPherson, Soil Conservation Service, Bastrop, Texas 78602 Mr. Floyd E. Potter, Jr., Texas Parks and lHl(,ili~~ Department, Austin, Texas 78759 i;:'y' , . // i f ,It . '1 ,/.' "V- Approved: '. ~ /-, j;t Regtaff'a i or, Region 2 U.S. Fi h, .. ' 'Wildlife Service Date: '/ .f --------~~~~~--------------------- SUMMARY 1 •. GOAL: Secure the survival and eventual recovery of the San Marcos .. gambusia, f01.nltain darter, San Marcos salamander, and Texas wildrice through protection of their natural ecosystem, the . San Marcos River.