Western Highland Rim Forests Conservation Opportunity Area
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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 -
General Index
GENERAL INDEX See also separate Stratigraphic Index and Chestnut Ridge anticline, 144 Authors' Index Chimney (Candle Stick) rocks, PIs. LXVII, LXVIII Agawam Station section, 29 Chinn calcite mine, 390 Allegheny-Cumberland structural front, 137 Cincinnati arch, 34, 97,132, 137,155, PIs. II, Allegheny peneplain, 156, 183 VIII, XXXI, XXXIII, XXXVI . Alluvium-filled valleys of western Ken- Claxton Station section (Caldwell Co.), 151 tucky, 161,164,203, PI. LUI Clay, 396, PI. CXVI, (tests and analyses), Barite, 388, 389, PI. XXXIV 404 Barrens (Pennyroyal), 187; (Purchase), 205 Cloverport salt industry, 429 Between the Rivers, 205 Coal, 250. See under mineral resources. Big Black Mountain, 180, PI. XXIV Conglomerate uplift, 355. See Paint Creek Big Bone Lick, 241,425, PI. LXX uplift. Big Bottoms (Purchase), 205 Creek Bottom Settlements (Eastern Coal Big Sandy River, 161, 162, 258, PI. LXXVI Field),175 Blue Grass, 166,167, 170, 231, 237, 389, CreelsboroNatural Bridge, 221, PI. LX 391, PIs. XXXV, XXXVII, Cryptovolcanic structures, 151, 393 XXXVIII, XXXIX, XL, XLIX, LI Cumberland arch, 152 Blue Lick, 245, 429, 431 Cumberland Falls, 238, PI. LXIX Boone's Cave, 231 Cumberland Gap, 143, 216, PIs. XLIII, LIX Bowling Green Is., 409, 412 Cumberland Gap topographic sheet, PI. Breaks of the Sandy, 182, 238, PIs. XLIV, XLIII LXIX Cumberland Mountain, 141,180, PIs. II, Breaks of the Tennessee, 205, 207, PI. II XXXVI, XLIII, LIX, LXIX Brines, 425, 430 "Cumberland Mountains," 175, 180 Brush Creek Hills, 189, 201 Cumberland overthrust (Pine Mountain Building Stone, 408, 409 fault, Cumberland thrust block, etc.), Burdett Knob, 135, 149, 174, 197, 390, 395, 140, 141, 142, 155, 347, PIs. -
East and Central Farming and Forest Region and Atlantic Basin Diversified Farming Region: 12 Lrrs N and S
East and Central Farming and Forest Region and Atlantic Basin Diversified Farming Region: 12 LRRs N and S Brad D. Lee and John M. Kabrick 12.1 Introduction snowfall occurs annually in the Ozark Highlands, the Springfield Plateau, and the St. Francois Knobs and Basins The central, unglaciated US east of the Great Plains to the MLRAs. In the southern half of the region, snowfall is Atlantic coast corresponds to the area covered by LRR N uncommon. (East and Central Farming and Forest Region) and S (Atlantic Basin Diversified Farming Region). These regions roughly correspond to the Interior Highlands, Interior Plains, 12.2.2 Physiography Appalachian Highlands, and the Northern Coastal Plains. The topography of this region ranges from broad, gently rolling plains to steep mountains. In the northern portion of 12.2 The Interior Highlands this region, much of the Springfield Plateau and the Ozark Highlands is a dissected plateau that includes gently rolling The Interior Highlands occur within the western portion of plains to steeply sloping hills with narrow valleys. Karst LRR N and includes seven MLRAs including the Ozark topography is common and the region has numerous sink- Highlands (116A), the Springfield Plateau (116B), the St. holes, caves, dry stream valleys, and springs. The region also Francois Knobs and Basins (116C), the Boston Mountains includes many scenic spring-fed rivers and streams con- (117), Arkansas Valley and Ridges (118A and 118B), and taining clear, cold water (Fig. 12.2). The elevation ranges the Ouachita Mountains (119). This region comprises from 90 m in the southeastern side of the region and rises to 176,000 km2 in southern Missouri, northern and western over 520 m on the Springfield Plateau in the western portion Arkansas, and eastern Oklahoma (Fig. -
Description of a Land Classification System and Its Application to the Management of Tennessee’S State Forests
DESCRIPTION OF A LAND CLASSIFICATION SYSTEM AND ITS APPLICATION TO THE MANAGEMENT OF TENNESSEE’S STATE FORESTS Glendon W. Smalley, S. David Todd, and K. Ward Tarkington III1 Abstract—The Tennessee Division of Forestry has adopted a land classification system developed by the senior author as the basic theme of information for the management of its 15 state forests (162,371 acres) with at least 1 in each of 8 physio- graphic provinces. This paper summarizes the application of the system to six forests on the Cumberland Plateau. Landtypes are the most detailed level in the hierarchical system and represent distinct units of the landscape (mapped at a scale of 1:24,000) as defined by physiography, climate, geology, soils, topography, and vegetation. Each of the 39 landtypes are described in terms of geographic setting, dominant soils, parent material, depth to bedrock, soil texture, soil drainage, relative soil water supply, relative fertility, and forest type. Additional information includes species suitable, site productivity, and operability for management activities. The maps aid the delineation of stands, streamside management zones, and “conservation” and other special use areas; the location of rare, threaten and endangered (RTE) species; the design of harvests; and the modeling of future forest conditions. The landtypes are an integral element in modeling wildlife habitat, in siting game food plots, and planning other wildlife management activities, particularly on forests that are dual wildlife and forest management areas. The maps are excellent training devices and extremely useful in explaining management plans to legislators and the public. INTRODUCTION The five levels of Smalley’s system proceeding from the least- The Tennessee Division of Forestry (TDF) has adopted a land detailed to the most-detailed are: physiographic province, classification system developed by the senior author (Smalley region, subregion, landtype association, and landtype. -
By Nevin M. Fenneman DEPARTMENT of GEOLOGY, UNIVERSITY of CINCINNATI Communicated by W
GEOLOGY: N. M. FENNEMAN 17 PHYSIOGRAPHIC SUBDIVISION OF THE UNITED STATES By Nevin M. Fenneman DEPARTMENT OF GEOLOGY, UNIVERSITY OF CINCINNATI Communicated by W. M. Davis, November 24, 1916 Various attempts at subdivision of the United States into physio- graphic provinces have been made, beginning with- that of Powell.' The Association of American Geographers, recognizing the fundamental importance of this problem, appointed a committee in 1915 to prepare a suitable map of physiographic divisions. The committee consists of Messrs. M. R. Campbell and F. E. Matthes of the U. S. Geological Survey and Professors Eliot Blackwelder, D. W. Johnson, and Nevin M. Fenneman (chairman). The map herewith presented and the ac- companying table of divisions constitute the report of that committee. The same map on a larger scale (120 miles to the inch) will be found in Volume VI of the Annals of the Association of American Geographers, accompanying a paper by the writer on the Physiographic Divisions of the United States. In that paper are given the nature of the bound- ary lines and those characteristics of the several units which are believed to justify their recognition as such. Though the above-named com- mittee is not directly responsible for the statements there made, many of them represent the results of the committee's conferences. The paper as a whole is believed to represent fairly well the views of the committee, though in form the greater part of it is a revision of a former publication.2 The basis of division shown on this map, here reproduced, is physio- graphic or, as might be said in Europe, morphologic. -
Ground-Water Resources in the Cumberland River Basin, I Kentucky-Tennessee
GROUND-WATER RESOURCES IN THE CUMBERLAND RIVER BASIN, I KENTUCKY-TENNESSEE I U. S. GEOLOGICAL SURVEY WATER RESOURCES INVESTIGATIONS t OPEN FILE REPORT 80- 202 1 I I I I '.m I i Prepared by the U.S. Geological Survey for the Ohio River Basin Commission's study of the Cumberland River basin. i i i i GROUND-WATER RESOURCES IN THE • CUMBERLAND RIVER BASIN • KENTUCKY-TENNESSEE I U.S. GEOLOGICAL SURVEY • WATER RESOURCES INVESTIGATIONS OPEN FILE REPORT 80-202 I I I I I I • Prepared by the U.S. Geological Survey for the Ohio River Basin Commission's study of the Cumberland River Basin I I I I I I I I UNITED STATES DEPARTMENT OF THE INTERIOR I CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY I H. William Menard, Director • I I I I I I I I Open-File Report • For additional information write to: U.S. Geological Survey | A-413 Estes Kefauver Federal Building U.S. Courthouse _ Nashville, Tennessee 37203 I I I I I I CONTENTS I Page Conclusions...................................................... 1 I Introduction..................................................... 3 Geologic setting................................................. 3 I Major aquifers and their water-bearing properties................ 4 I Aquifers in the alluvium...................................... 6 Aquifers in the Pennsylvanian rocks........................... 7 I Aquifers in the Mississippian rocks........................... 8 Aquifers in the Ordovician rocks. ............................. 9 I Potential for development........................................ 11 I Selected references.............................................. 13 I ILLUSTRATIONS I Plate 1. Map showing generalized geology of the Cumberland River basin....................................... In back I of report 2. Map showing potential availability of large I ground-water supplies in the Cumberland River basin...................................... -
At-Risk Species Assessment on Southern National Forests, Refuges, and Other Protected Areas
David Moynahan | St. Marks NWR At-Risk Species Assessment on Southern National Forests, Refuges, and Other Protected Areas National Wildlife Refuge Association Mark Sowers, Editor October 2017 1001 Connecticut Avenue NW, Suite 905, Washington, DC 20036 • 202-417-3803 • www.refugeassociation.org At-Risk Species Assessment on Southern National Forests, Refuges, and Other Protected Areas Table of Contents Introduction and Methods ................................................................................................3 Results and Discussion ......................................................................................................9 Suites of Species: Occurrences and Habitat Management ...........................................12 Progress and Next Steps .................................................................................................13 Appendix I: Suites of Species ..........................................................................................17 Florida Panhandle ............................................................................................................................18 Peninsular Florida .............................................................................................................................28 Southern Blue Ridge and Southern Ridge and Valley ...............................................................................................................................39 Interior Low Plateau and Cumberland Plateau, Central Ridge and Valley ...............................................................................................46 -
Northwest Corridor Regional Transportation Authority of Middle Tennessee Transit Study SUMMARY of FINDINGS and RECOMMENDATIONS | October 2017
Northwest Corridor Regional Transportation Authority of Middle Tennessee Transit Study SUMMARY OF FINDINGS AND RECOMMENDATIONS | October 2017 For a copy of the appendices of the Northwest Corridor Transit Study report, please contact Felix Castrodad at 615-862-5626 or [email protected]. Northwest Corridor Transit Study | FINAL REPORT | 10.2017 ACKNOWLEDGEMENTS The Regional Transportation Authority (RTA) of Middle Tennessee would RTA BOARD TENNESSEE DEPARTMENT OF TRANSPORTATION like to thank the following for their contributions to the development Chair: Mayor Kim McMillan, City of Clarksville Commissioner John Schroer of the Northwest Corridor Transit Study: Vice Chair: Mayor Randall Hutto, Wilson County Secretary: Paula Mansfield, Rutherford County GOVERNOR’S APPOINTEES ADVISORY COMMITTEE Cheatham County Cheatham County - Daryl Phillips Mayor Kim McMillan, City of Clarksville Ashland City - Mayor Rick Johnson Davidson County - Ed Cole Mayor Rick Johnson, City of Ashland City Cheatham County - Mayor David McCullough Dickson County - Scott England Mayor Megan Barry, Metropolitan Nashville and Davidson County Montgomery County - Mike Evans Davidson County Mayor Billy Paul Carneal, City of Springfield Rutherford County - Paula Mansfield Belle Meade - Mayor James Hunt Mayor Jim Durrett, Montgomery County Sumner County - Lee Zoller Davidson County/Metro Nashville - Mayor Megan Barry Mayor David McCullough, Cheatham County Williamson County - Kelly Dannenfelser Goodlettsville - Mayor John Coombs Mayor Howard Bradley, Robertson County -
Clarksville Historic Survey Final Report 2020
CLARKSVILLE HISTORIC RESOURCES SURVEY UPDATE CLARKSVILLE, MONTGOMERY COUNTY, TENNESSEE REPORT PREPARED FOR THE CITY OF CLARKSVILLE, TENNESSEE THOMASON AND ASSOCIATES, PRESERVATION PLANNERS NASHVILLE, TENNESSEE AUGUST 2020 TABLE OF CONTENTS SECTION I - INTRODUCTION & PROJECT LOCATION………………………………….2 SECTION II - METHODOLOGY……………………………………………………………....6 SECTION III - HISTORICAL OVERVIEW……………………………………………………8 SECTION IV – ARCHITECTURAL OVERVIEW…………………………………………...37 SECTION V - SUMMARY AND RECOMMENDATIONS…………………….…………...76 BIBLIOGRAPHY………………………………………….……………………………………82 SECTION I: INTRODUCTION & PROJECT LOCATION Introduction The Tennessee Historical Commission (THC) is the state’s historic preservation agency, and one of its important programs is the architectural and historical inventory of the state’s cultural resources. This inventory is a significant part of historic preservation and community planning since it provides basic data on the location, condition and architectural character of buildings and structures. Montgomery County was originally surveyed in 1981. Since that time numerous properties have been listed in the National Register of Historic Places, and mid-20th-century buildings have attained the fifty-year mark. In 2019, the THC awarded the City of Clarksville a federal historic preservation grant to fund a survey of downtown Clarksville. The inventory was conducted between May and September of 2020. This survey was completed by Thomason and Associates of Nashville, Tennessee (Contractor). The scope of the survey included updating the existing inventory from 1981 and identifying properties that have reached fifty years since their dates of construction. For this survey, the end date of 1969 reflects the fifty-year time period from 2019. To assist the Contractor with this survey, the Clarksville Planning Commission’s GIS Department provided property maps identifying pre-1970 parcels based on Montgomery County tax records. -
Natural Resources
Natural Heritage in the MSNHA The Highland Rim The Muscle Shoals National Heritage Area is located within the Highland Rim section of Alabama. The Highland Rim is the southernmost section of a series low plateaus that are part of the Appalachian Mountains. The Highland Rim is one of Alabama’s five physiographic regions, and is the smallest one, occupying about 7 percent of the state. The Tennessee River The Tennessee River is the largest tributary off the Ohio River. The river has been known by many names throughout its history. For example, it was known as the Cherokee River, because many Cherokee tribes had villages along the riverbank. The modern name of the river is derived from a Cherokee word tanasi, which means “river of the great bend.” The Tennessee River has many dams on it, most of them built in the 20th century by the Tennessee Valley Authority. Due to the creation of these dams, many lakes have formed off the river. One of these is Pickwick Lake, which stretches from Pickwick Landing Dam in Tennessee, to Wilson Dam in the Shoals area. Wilson Lake and Wheeler Lake are also located in the MSNHA. Additionally, Wilson Dam Bear Creek Lakes were created by four TVA constructed dams on Bear Creek and helps manage flood conditions and provides water to residents in North Alabama. Though man-made, these reservoirs have become havens for fish, birds, and plant life and have become an integral part of the natural heritage of North Alabama. The Muscle Shoals region began as port area for riverboats travelling the Tennessee River. -
A History of Tennessee.Indd
352 TENNESSEE BLUE BOOK A HISTORY OF TENNESSEE 353 SECTION VI Tennessee 354 TENNESSEE BLUE BOOK A HISTORY OF TENNESSEE 355 A HISTORY OF TENNESSEE The Land and Native People Tennessee’s great diversity in land, climate, rivers, and plant and animal life is mirrored by a rich and colorful past. For all but the last 200 years of the 12,000 years or so that this country has been inhabited, the story of Tennessee is the story of its native peoples. The fact that Tennessee and many of the places in it still carry Indian names serves as a lasting reminder of the significance of its native inhabit- ants. Since much of Tennessee’s appeal for her ancient people as well as for later pioneer settlers lay with the richness and beauty of the land, it seems fitting to begin by considering some of the state’s generous natural gifts. Tennessee divides naturally into three “grand divisions”—upland, often moun- tainous, East Tennessee, Middle Tennessee with its foothills and basin, and the low plain of West Tennessee. Travelers coming to the state from the east encounter first the lofty Unaka and Smoky Mountains, flanked on their western slope by the Great Valley of East Tennessee. Moving across the Valley floor, they next face the Cumberland Plateau, which historically attracted little settlement and presented a barrier to westward migration. West of the Plateau, one descends into the Cen- tral Basin of Middle Tennessee—a rolling, fertile countryside that drew hunters and settlers alike. The Central Basin is surrounded on all sides by the Highland Rim, the western ridge of which drops into the Tennessee River Valley. -
Classification and Evaluation of Forest Sites on the Northern Cumberland Plateau
.,;;~~~\ United States IttAc.. !)) Department of Classification and Evaluation \:..~ Agriculture Forest Service of Forest Sites on the Southern Forest Northern Cumberland Plateau Experiment Station New Orleans, Louisianfl General rechnical Report SO-60 March 1986 Glendon W. Smalley SUMMARY This paper presents a comprehensive forest site classification system for the northern Cumberland Plateau in north central Tennessee and eastern Ken tucky. The system is based on physiography, geology, soils, topography, and vegetation. Twenty-four landtypes are described and evaluated in terms of productivity and desirability of selected pines and hardwoods for timber pro duction. Also, each landtype is rated for five soil-related problems that can affect forest management operations. ACKNOWLEDGMENTS I am indebted to my colleagues, past and present, for their scientific input, reviews, and stimulating discussions. I am also grateful to the soil scientist$, silviculturists, plant ecologists, and practicing foresters who have reviewed this guide. CONTENTS Introduction ..................................................... 1 Northern Cumberland Plateau Region............................. 1 Subregions and LandtypeAssociations ..... ..... ... .. .. ... .. ...... 11 Landtypes ....................................................... 15 Forest Management Interpretations ............................... 16 Using the System ................................................ 17 Landtype Descriptions and Forest Management Interpretations . 23 Literature Cited ..............................