First Oil Well Kentucky

Total Page:16

File Type:pdf, Size:1020Kb

First Oil Well Kentucky THE FIRST OIL WELL IN KENTUCKY By WiUavd Rouse JiUson 1952 THE FIRST OIL WELL IN KENTUCKY By Willard Rouse Jillson 1952 THE FIRST OIL WELL IN KENTUCKY Notes on The History, Geology, Production and Present Status of the Beatty Oil Well, Drilled in Wayne, now McCreary County, Kentucky, in the year 1818 By WILLARD ROUSE JILLSON, Sc. D. OeoIogUt and Engineer ROBERTS PRINTING CO. FRANKFORT, KY. 1952 First Printing SEPTEMBER 3, 1952 FOBEWOBD America traditionally accords honor and dis­ tinction to those who are the first to achieve success in any field of important national endeavor. Retro­ spectively one recalls the great acclaim that attended Robert Fulton's demonstration of the practicality of the steamboat, Eli Whitney's tremendous success with the cotton gin, and Wilbur Wright's short but epochal flight o'er the sands of Kitty Hawk. To these the names of a good many others who have won for themselves a kind of immortality might be added—^Lewis and Clark as explorers, McCormick with the reaper, Bell with the telephone, Westing- house with the air brake, Erickson with the mono- tored gunboat and Hoe with the straightline press— to name only a few 1 In the dynamic, industrial field of PETROL­ EUM, the middle years of the nineteenth century witnessed the miracle-like emergence and recognition of Edwin L. Drake as the first practical oil producer,. and of John D. Rockefeller as the first national oil refiner and distributor. Though upwards of a hun­ dred and fifty years have passed since the event took place, it now seems but tardy justice to add to these great names topping the scroll of the petroleum pioneers, a third, that of Marcus Huling of Penn­ sylvania, who in the year 1818 brought in the Martin Beatty No. 1 on the South Pork of the Cumberland River, the first oil well in Kentucky and the iirst flowing well of importance in America! 7?ie^ Frankfort, Kentucky June 10,1952. HRST OIL WELL IN KENTUCKY SALT WATER During the first decade of the nineteenth cen­ tury, the rapid growth of population in the middle Ohio Valley created an insatiable demand for those essentials of life which are derived, more or less directly, from the earth. Iron for nails, implements and wagons; coal for forges and grates; and salt for the kitchens, tables and preserving processes of the pioneers, like meat and bread, were in the very fore­ front of domestic requirements. In Kentucky, mar­ velously expanding spear head of Anglo-American civilization in the West, the demand for salt exceeded the supply produced at "the Licks" for upwards of half a century after the building of the first forts and stations. During these early years it became not only an eagerly sought staple of merchandising, but in lieu of hard currency which was generally and provocably scarce, was frequently used in trade and barter as a commodity of monetary exchange. Time and again, when available, coarse, granulated salt was held at a value of $25.00 and $30.00 a barrel, and frequently at town and crossroad stores it was retailed at prices double and treble this amount. In an effort to meet the steady demand for in­ creasing volumes of salt, pits of considerable size and depth, were dug at all of the "improved" salt licks in Kentucky to increase the flow and volume of the natural brines. Outstanding among the "salt works" operated in this manner within or bordering the Bluegrass country were those at Lower Blue Licks, Big Bone Lick, Drennon's Lick, Mann's Lick, Bullitt's Lick, and Flat Lick. When it became ap­ parent that the limit of productivity had been reached by this method at these and a few other salt springs, it was but a natural step to change over from the shallow pit or "dug well" to a drilled well, which at somewhat greater depths might, and as it shortly developed, did penetrate the beds that ac­ tually contained the salt water. As it chanced the ex- peiriment began in a small way in 1806 at one of the salt licks in the Kanawha River in what was then Vir­ ginia, Within two years hard rock drilling had be­ come recognized as a successful brine producing practice and by the time the War of 1812 began to raise the prices of many eatables in the West, par­ ticularly preserved meats, men of enterprise and in­ genuity were "kicking down" salt wells with hand made "spring pole rigs" in southeastern Ohio and southern Kentucky. Though it was but remotely anticipated, if at all, by these pioneer operators at the time of this initial sweep of drilling exploration, in the light of present day geological knowledge, it was a certainty and only a matter of time and location before one or more salt well drillers would strike oil. Accordingly it is not at all surprising to find in the folk lore of southern Kentucky the tale of a salt well drilled two 10 mUes south of MonticeUo in 1815 which "at a depth of 283 feet was abandoned because petroleum was found in such quantities as to ruin ... it as a salt well." In the midsummer of 1865, fifty years later, the bare essentials of this epoch marking discovery of oil in the southern part of this Commonwealth, already vague and legendary, fortunately found per­ manent record in the news columns of the daily Ob­ server and Reporter, of Lexington, Kentucky. It is stated that Micajah Phillips possessed the land during the sixties on which this remarkable well was drilled, but it appears that the name of the driller and the land owner, at the time the strike was made, have been irretrievably lost. Evidently the amount of oil found in this salt well in 1815 was rather small, insufficient to cause more than a local ripple of inter­ est, recollection of which has been all but obliterated in the lengthening flight of the years. OIL WELL Late in December, 1817, Martin Beatty, whose surname is frequently written Beaty—purchased of John Francis of Wayne County, Kentucky, 1000 acres of land lying on the Big South Fork of the Cumberland River at a point about two to three miles above or south of Bear Creek. Beatty was originally from Abingdon, southwestern Virginia, but at the time of this transaction was operating an iron fur­ nace near the great spring at Cumberland Gap, Ten­ nessee. He had somewhat previously purchased an appreciable undivided interest in another 1000 acre tract located on the west side of the South Fork at and about the mouth of Bear Creek upon which nat- 11 ural brines had already been produced in a drilled well and where salt was later manufactured in con­ siderable quantity. This establishment seated in Wayne County opposite the mouth of Bear Creek later came to be known as Saltville. It was operated with variable success down to the year 1840, when due to heavy and continued losses sustained in at­ tempting to ship the product out on occasional high tides and thus override the navigatory perils of the "jumps" and the "shoals" of the river, the opera­ tion was closed down and permanently abandoned. In acquiring the upper or second 1000 acre tract, money apparently being not readily at hand, Beatty issued as consideration the notes of the Saltville partnership which besides his own, embraced the interests held by Lilburn L. Henderson and Stephen T. Conn, both of whom were also from Abingdon. Francis had entered and surveyed the tract on De­ cember 24, 1817 as may be noted in Wayne County, Kentucky, Surveyors Book No. 1, page 370, under the Act of the Q-eneral Assembly passed February 2, 1813 to encourage the manufacturing of salt. This statute provided that any individual or group, after "improving" a tract of previously unoccupied land and producing 1000 bushels of salt, could acquire fee simple title to the land by paying to the Treasurer of Kentucky $10 per 100 acres for the land on which the salt was produced. Finally, after considering the matter at some length, Beatty determined to take only 727 acres of the 1000 acre entry and this boun­ dary was then surveyed and patented by him on December 28, 1821. In the meantime, however, Martin Beatty acting for the Saltville co-partnership, leased the 727 acre 12 . tract to one Marcus Huling and his associate, An­ drew Zimmerman, both of whom desiring to drill for salt brines, had come into the country from Lee County, Virginia, but were originally from north­ western Pennsylvania. A well was located in the bottoms of the South Fork just above the mouth of a sizable south flowing tributary of the Cumberland. This stream is today known as Oil Well Branch. Its debouchure and the adjacent drilling site are about one mile below the mouth of Troublesome Creek. Operations with a "spring pole rig" were begun in the Spring of 1818. Some time late in the Fall, probably the latter part of November, at a depth of "about two hundred feet" a heavy black oil was en­ countered, which rose rapidly in the hole, over­ flowed the hollow log conductor and ran in consid­ erable volume over the bank into the Cumberland River and on dowli stream for a good many, perhaps 30 or 40 miles. From such records as are now available it ap­ pears that this drilling—^widely heralded in its time and since as the Beatty Oil Well—^flowed upwards of 100 barrels per day under a gas head for several days immediately after it was "brought in as a producer." Its flow then gradually declined and fimaUy ceased, due probably to the reduction of the gas and rock pressure.
Recommended publications
  • The Cumberland Settlement
    The Cumberland Settlement Essential Question: Why was the Cumberland Settlement created and what problems did the early settlers encounter? In 1775, Richard Henderson purchased 20 million acres of land from the Cherokee in a land deal known as the Transylvania Purchase. The lands lay in what is now middle Tennessee and Kentucky. While Henderson was not able to convince Virginia and North Carolina to recognize his entire claim, he was able to claim the region near the Cumberland River in Middle Tennessee. In 1779, Henderson planned a settlement in order to take advantage of the region’s rich natural resources including fertile soil and abundant animal life. Henderson’s settlement was named the Cumberland Settlement for the Cumberland River which served as main transportation route in the region. Henderson gave the difficult task of establishing the settlement to James Robertson and John Donelson. Donelson was an experienced land surveyor and veteran of the Cherokee War. James Robertson was one of first Watauga settlers and had served as one of the five magistrates established under the Watauga Compact. Robertson had also served as commander of Watuaga Fort during the Cherokee War. Henderson had a two part plan for settling the Cumberland region. First, Robertson and a small group of Wataugans traveled overland in the spring of 1779 to select a site for the settlement near French Lick. French Lick was a natural salt lick along the Cumberland River that had been the location of a French trading post. In December of 1779, Robertson and the men returned and built cabins and Fort Nashborough in preparation for the arrival of Donelson’s party in the spring of 1780.
    [Show full text]
  • Comprehensive Annual Financial Report 2008
    CITY OF HENDERSON, KENTUCKY COMPREHENSIVE ANNUAL FINANCIAL REPORT FOR THE FISCAL YEAR ENDED JUNE 30, 2008 Betty Smithhart, Photographer CITY OF HENDERSON, KENTUCKY COMPREHENSIVE ANNUAL FINANCIAL REPORT For the Fiscal Year Ended June 30, 2008 Prepared by the City of Henderson Finance Department CITY OF HENDERSON, KENTUCKY COMPREHENSIVE ANNUAL FINANCIAL REPORT For the Fiscal Year Ended June 30, 2008 TABLE OF CONTENTS Page INTRODUCTORY SECTION Letter of Transmittal ...........................................................................................1 GFOA Certificate of Achievement .....................................................................9 Organizational Chart ...........................................................................................10 List of Elected and Appointed Officials .............................................................11 FINANCIAL SECTION Independent Auditors’ Report .............................................................................12 Management’s Discussion and Analysis ............................................................14 Basic Financial Statements: Government-wide Financial Statements: Statement of Net Assets ................................................................................25 Statement of Activities .................................................................................26 Fund Financial Statements: Balance Sheet – Governmental Funds ..........................................................27 Reconciliation of the Balance Sheet of Governmental
    [Show full text]
  • 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......................................
    [Show full text]
  • Lake Cumberland
    Lake or Pond LAKE INSET National River, Stream MAP Wildlife or Creek Reserve State Capitol BOAT RAMP See LAKE Creek LAKE or Rive or LAKE r County Seat Wildlife POND FRANKFORT ACCESS SITE 33 InsetInset Management NWR Area Inez State Road WMA 89 U.S. Highway U.S. Military 420 TROUT 3D Base Licking Big U.S. Interstate STREAM Lower River Sandy 64 Parkway KY p.38+39 & Salt PKWY River River Little State State p.22+23 Nature Forest National p.18+19 Sandy Preserve Park State SF Rivers Lock & Dam Park SNP NP SP Lower Upper p.42+43 State USFS Resort SRP Green KY Proclamation Park Area SNA River River State SHS Upper County or Natural p.8+9 p.26+27 State Line Area Green State Tennessee, Upper Historic Site Lower Cumberland, River Cumberland p.12+13 Tradewater & Mississippi p.30+31 Fort Boonesborough Rivers p.2+3 SP 0 50 100 Approx. Scale in Miles: LOCK & DAM #10 S t o n 75 e 627 y LOCK & DAM #9 Run White Hall TUCKY EN SHS K 169 388 RIVER 1156 r MADI e v i R 27 LOCK & 25 DAM #8 LAKE REBA Richmond k 876 e x HERRINGTON LAKE e Di r C r a g u S TAYLOR \FORK GARRARD 595 LAKE P ai nt L re ic ilver C ek 1295 k S C re e k 421 39 75 Lancaster 595 Big South Fork of the Cumberland River 1016 590 25 Upper areas of this river are within the Big South Fork National River and Recreation Area which is in both Kentucky and Tennessee.
    [Show full text]
  • A Native History of Kentucky
    A Native History Of Kentucky by A. Gwynn Henderson and David Pollack Selections from Chapter 17: Kentucky in Native America: A State-by-State Historical Encyclopedia edited by Daniel S. Murphree Volume 1, pages 393-440 Greenwood Press, Santa Barbara, CA. 2012 1 HISTORICAL OVERVIEW As currently understood, American Indian history in Kentucky is over eleven thousand years long. Events that took place before recorded history are lost to time. With the advent of recorded history, some events played out on an international stage, as in the mid-1700s during the war between the French and English for control of the Ohio Valley region. Others took place on a national stage, as during the Removal years of the early 1800s, or during the events surrounding the looting and grave desecration at Slack Farm in Union County in the late 1980s. Over these millennia, a variety of American Indian groups have contributed their stories to Kentucky’s historical narrative. Some names are familiar ones; others are not. Some groups have deep historical roots in the state; others are relative newcomers. All have contributed and are contributing to Kentucky's American Indian history. The bulk of Kentucky’s American Indian history is written within the Commonwealth’s rich archaeological record: thousands of camps, villages, and town sites; caves and rockshelters; and earthen and stone mounds and geometric earthworks. After the mid-eighteenth century arrival of Europeans in the state, part of Kentucky’s American Indian history can be found in the newcomers’ journals, diaries, letters, and maps, although the native voices are more difficult to hear.
    [Show full text]
  • Longhunter, Southern Kentucky Genealogical Society Newsletter Volume 26, Number 2 Kentucky Library Research Collections Western Kentucky University, [email protected]
    Western Kentucky University TopSCHOLAR® Longhunter, Southern Kentucky Genealogical Kentucky Library - Serials Society Newsletter Spring 2003 Longhunter, Southern Kentucky Genealogical Society Newsletter Volume 26, Number 2 Kentucky Library Research Collections Western Kentucky University, [email protected] Follow this and additional works at: https://digitalcommons.wku.edu/longhunter_sokygsn Part of the Genealogy Commons, Public History Commons, and the United States History Commons Recommended Citation Kentucky Library Research Collections, "Longhunter, Southern Kentucky Genealogical Society Newsletter Volume 26, Number 2" (2003). Longhunter, Southern Kentucky Genealogical Society Newsletter. Paper 81. https://digitalcommons.wku.edu/longhunter_sokygsn/81 This Newsletter is brought to you for free and open access by TopSCHOLAR®. It has been accepted for inclusion in Longhunter, Southern Kentucky Genealogical Society Newsletter by an authorized administrator of TopSCHOLAR®. For more information, please contact [email protected]. HUNTER ISSN 10677348 Southern Kentucky Genealogical Society + Volume XXVI - Issue 2 Spnng, 2003 SOUTHERN KENTUCKY GENEALOGICAL SOCIETY P. O. Box 1782 Bowling Green, KY 42102-1782 2003 Officers SM President Gail Jackson Miller, CG , <[email protected]> 425 Midcrest Dr, Bowling Green, KY, 42101 Vice President Chad Regan, < [email protected]> 309 w. Villa Dr., Bowling Green, KY, 42101 Recording Secretary Ann Wyan, <[email protected] > 850 Wilkinson Trace #207, Bowling Green, KY, 42103 Corresponding Secretary Alexandra Ebling, <[email protected]> 431 Collen Bridge Road, Alvaton, KY, 42122 Treasurer Rebecca Shipley, < [email protected]> 702 Eastwood, Bowling Green, KY, 42103 Longhunter Editor Gail Jackson Miller, CGS>' Membership Membership in the Southern Kentucky Genealogical Society is open to aU persons, especiaUy those who are interested in research in Allen, Barren, Butler, Edmonson, Logan, Simpson, and Warren County, KY or their neighbors.
    [Show full text]
  • Mccreary County, KY
    McCreary County, Kentucky CASE STUDIES What I think makes it a Bright Spot is that we do see ourselves—the whole county—as a community, and that we do come together. —Kay Morrow, Director, McCreary County Public Library Creative Commons 2.0 Generic Treewoman8 / The Big South Fork of the Cumberland River in McCreary County The only Kentucky county without an incorporated city, McCreary County is a place where everyone knows everyone. As in many communities in Appalachia, residents here have seen their way of life shift dramatically as a result of the boom and bust of the coal and timber industries and declining economic opportunities. Despite living in one of the poorest counties in the state and the country, McCreary residents harbor a sense of hope for untapped potential. They embody the Kentucky commonwealth’s motto “United We Stand, Divided We Fall.” McCreary County may face many challenges, but this tight-knit community draws upon its collective strength and common goals to improve health across the county. In downtown Whitley City, the county seat, the courthouse yard sprawls across the street from the local library, both welcoming venues in a community that is striving to reinvent itself as an outdoor-activity destination. 45 CREATING A CULTURE OF McCreary County, Kentucky | HEALTH IN APPALACHIA CASE STUDIES McCreary County is home to approximately 18,000 people, and the population is predominantly white. Its poverty rate is triple the national rate, and the unemployment rate is 10.6 percent, much higher than the national average of 6.2 percent. McCreary County is among the ten percent of Appalachian counties—and one of nine counties in Appalachian Kentucky—identified as a Bright Spot, performing better than expected on 14 out of 19 different health outcome measures.
    [Show full text]
  • Cumberland Plateau Geological History
    National Park Service U.S. Department of the Interior Big South Fork National River and Recreation Area Oneida, Tennessee Geology and History of the Cumberland Plateau Geological History Rising over 1000 feet above the region around it, the Cumberland Plateau is a large, flat-topped tableland. Deceptively rugged, the Plateau has often acted as a barrier to man and nature’s attempts to overcome it. The Plateau is characterized by rugged terrain, a moderate climate, and abundant rainfall. Although the soils are typically thin and infertile, the area was once covered by a dense hardwood forest equal to that of the Appalachians less than sixty miles to the east. As a landform, this great plateau reaches from north-central Alabama through Tennessee and Kentucky and Pennsylvania to the western New York border. Geographers call this landform the Appalachian Plateau, although it is known by various names as it passes through the differ­ ent regions. In Tennessee and Kentucky, it is called the Cumberland Plateau. Within this region, the Cumberland River and its tributaries are formed. A view from any over- look quickly confirms that the area is indeed a plateau. The adjoining ridges are all the same height, presenting a flat horizon. The River Systems The Clear Fork River and the New River come together to form the Big South Fork of the Cumberland River, the third largest tributary to the Cumberland. The Big South Fork watershed drains an area of 1382 square Leatherwood Ford in the evening sun miles primarily in Scott, Fentress, and Morgan counties in Tennessee and Wayne and Overlooks McCreary counties in Kentucky.
    [Show full text]
  • Cumberland Falls Trail 11X17
    Sheltowee Trace #100 Section 27 - Moonbow: This 11-mile section of the These popular trails are located along the Cumberland River on the London Sheltowee Trace National Recreation Trail is also known as the “Moonbow Trail.” London District Ranger District. The trail runs adjacent to the Cumberland River from the Mouth of Laurel to 761 S. Laurel Road Cumberland Falls, the second largest waterfall east of the Rocky Mountains. London, KY 40744 Bark Camp Trail #413 follows the north side of Bark Camp Creek. The trail 606-864-4163 passes under rock shelters and cliffs. There is a small waterfall about a mile from From Fishing Creek to Bark Camp Creek, an alternate flood route (#100A, 3 the trailhead and a beautiful series of cascades near the trail's junction with the miles) is available for use during periods of high water. The flood route follows Open Dates Sheltowee Trace National Recreation Trail. An adirondack shelter is located on mostly ridges and Forest Service roads above the cliffline. Open all year. the Sheltowee Trace about one tenth mile south of the its junction with Bark Camp Trail. The creek is stocked with rainbow trout. The Sheltowee Trace continues by crossing a bridge over Bark Camp Creek, just Fees No fee for trail use. Directions to trailhead: From I-75, take exit 25 and travel west on US 25 W. Turn Food Storage Required above the scenic water cascades. A small camping shelter is located a few right on KY 1193 and travel several miles, merging straight ahead onto KY 1277.
    [Show full text]
  • Bank Fishing
    Bank Fishing The following bank fishing locations were compiled by 4. Fish are very sensitive to sounds and shadows and can TWRA staff to inform anglers of areas where you can fish see and hear an angler standing on the bank. It is good without a boat. The types of waters vary from small ponds to fish several feet back from the water’s edge instead and streams to large reservoirs. You might catch bluegill, of on the shoreline and move quietly, staying 20 to 30 bass, crappie, trout, catfish, or striped bass depending on feet away from the shoreline as you walk (no running) the location, time of year, and your skill or luck. from one area to the other. Point your rod towards the All waters are open to the public. Some locations are sky when walking. Wearing clothing that blends in privately owned and operated, and in these areas a fee is re- with the surroundings may also make it less likely for quired for fishing. It is recommended that you call ahead if fish to be spooked. you are interested in visiting these areas. We have included 5. Begin fishing (casting) close and parallel to the bank these fee areas, because many of them they are regularly and then work out (fan-casting) toward deeper water. stocked and are great places to take kids fishing. If you’re fishing for catfish, keep your bait near the bottom. Look around for people and obstructions Bank Fishing Tips before you cast. 1. Fish are often near the shore in the spring and fall.
    [Show full text]
  • Robertson Sumner Macon Clay Jackson Putnam Smith
    24" Numbers in green circles correspond to numbered Points of Interest throughout this guide. 1 Point of Interest RING OF FIRE TRAIL EXTRAS: PAGE Farms .......................................... 18 Visitor Information Festivals & Events ......................... 17 Food & Wine ................................ 12 SF - State Forest Land Trust for Tennessee I-65, exit 121, S bound 36" Great Outdoors ............................. 16 WMA - Wildlife Protected Property Robertson Co. (Mitchellville) Management Area 615-325-4721 Lodging ....................................... 13 Main Trail I-40, exit 267, E & W bound Off-Trail Highlight Smith Co., 615-683-6410 NASHVILLE AREA Base map SELF-GUIDED DRIVING TOUR by Richard Quin All locations on map are approximate. Map is not to scale. 8" 591 383 816 73 96 492 99 WATCH FOR THESE 848 KENTUCKY 65 Find out more at SIGNS ALONG 87 216 49 MITCHELLVILLE KENTUCKY 63RingOfFireTrail.com THE RING OF FIRE 431 163 Fairfield 174 TRAIL ROUTE. 161 32 31E Red River Rocky ORLINDA 109 259 Mound 51 17-21 52 36 37 33 ADAMS 56 52 25 34-35 261 Moss 238 52 WESTMORELAND MACON Hermitage 41 29 31W Springs 16 76 CEDAR HILL PORTLAND 52-55 56 30-31 38 Frog 161 25 Pond 53 Dale LAFAYETTE 39 10 48-51 CLAY CELINA Hollow 49 RED BOILING 45 135 57-58 Lake Port 256 Cedar Hill 28 CROSS PLAINS 109 41-42 SPRINGS Royal Swamp WMA 22-26 174 52 40 46 151 State 47 53 To Park SPRINGFIELD 27 76 52 Allons 15 ROBERTSON 141 43 44 52 Bethpage 10 Standing 136 Stone 76 North Springs State Park 59 49 WHITE 25 31E 231 292 & SF 14 262 56 56 431 41 HOUSE
    [Show full text]
  • Wolf Creek Dam (Lake Cumberland) Reconnaissance–Level Evaluation of Dissolved Oxygen Improvement Study
    Wolf Creek Dam (Lake Cumberland) Reconnaissance–Level Evaluation of Dissolved Oxygen Improvement Study Section 1. Introduction. The purpose of this evaluation is to identify, compare and assess the costs of various technologies available to improve dissolved oxygen (DO) levels in hydropower discharges from Wolf Creek Dam (WOL). In 2017, the Southeastern Power Administration (SEPA) and other hydropower stakeholders requested that the Corps consider installation of technologies, such as oxygen diffusers, to prevent hydropower revenues lost through water releases via sluice and orifice gates during seasonal periods of poor water quality. Wolf Creek Dam is located at Cumberland River mile 460.9 in south central Kentucky with a vicinity map shown in Figure 1. The dam is 258 feet (ft) high and consists of a combination earth fill and concrete structure totaling 5,736 feet long. Wolf Creek powerhouse has six 45- megawatt (MW) turbines, for a total (non-overload) capacity of 270-MW. US Highway 127 currently crosses the crest of the dam but is expected to be relocated in the near future. Lake Cumberland, created by the dam, impounds 6,089,000 acre-feet (ac-ft) at the top of the Flood Control Pool elevation of 760 ft (National Geodetic Vertical Datum of 1929). All project uses except flood control, are drawn from the power pool located between elevations 673 ft and 723 ft. Under normal operations, summer pool elevation of 723 ft and is targeted in mid-May and held until mid-June. The lake is then gradually drawn down to reach the targeted winter pool elevation of 695 ft by January.
    [Show full text]