Big Bone | |
---|---|
Coordinates: 38°53′19″N84°45′7″W / 38.88861°N 84.75194°W | |
Country | United States |
State | Kentucky |
County | Boone |
Time zone | UTC-5 (Eastern (EST)) |
• Summer (DST) | UTC-4 (EDT) |
GNIS feature ID | 487080 [1] |
Big Bone is an unincorporated community in southern Boone County, Kentucky, United States. It is bounded on the west by the Ohio River, and Rabbit Hash, on the south by Big Bone Creek, which empties into the river at Big Bone Landing. The northern extent is along Hathaway Road, and the eastern portion extends not further than U.S. 42, and is approached from that direction by Beaver Road (Route 338) coming from either Richwood or Walton. Big Bone took its name from a nearby prehistoric mineral lick of the same name. [2] Geographical features of interest include Big Bone Lick State Park and the now disappeared Big Bone Island.
Big Bone Lick, now the site of Big Bone Lick State Park, is a well-known landmark in the immediate area of Big Bone. [3] The salt lick, or lick, as it is more generally known locally, was long known to the original inhabitants of the area. The fossil deposits were a well-known feature in the geographical region. [4] The area was named after the extraordinarily large bones, including those of mammoths and mastodons, found in the swamps around the salt lick frequented by animals, who need salt in their diets. [4] The mineral springs are created by water flowing through the underlying formations of limestone and shale, where the trapped salts are dissolved and carried, in solution, to the surface, creating brine. [5] : 6–7
In 1809, a salt furnace featuring two large furnaces with mounted kettles was built to extract salt from the brackish water. It was soon discovered that, due to the relatively low salinity of the springs, 500 to 600 gallons of water were required to produce a single bushel of salt. By 1812 the venture had failed. [5] : 10–11
The Clay House, a resort hotel, opened nearby in 1815, offering visitors an opportunity to bathe in the supposedly medicinal salt mineral springs. It quickly became popular among naturalists, who came to find bones for museums or private collections. [6] The Clay House closed in 1830, [7] : 88 but the salt springs remained a popular spa until 1847. A second hotel was built in 1870. [5] : 11
A post office called Bigbone was established in 1890, and remained in operation until 1941. [8]
Big Bone Creek enters the Ohio River at mile 516.8 below Pittsburgh. The mouth is at the division of Boone and Gallatin Counties, Kentucky, near the site of Big Bone Island. [9] It is navigable for several miles, and flows through Big Bone Lick State Park. [10]
Big Bone Island was a small, natural island composed of sand and gravel in the Ohio River near the mouth of Big Bone Creek at Big Bone. [9] [11] It is just south of the Boone County line in Gallatin County, Kentucky. [9] Of note is that the county line "runs down the center of the creek". [9] It plays a part in local lore and history of the area and was a popular fishing and camping location. [11] The island has disappeared due mostly to the rise of the river caused by the construction of the Markland Dam, [9] but also due to slabs of floating river ice which destroyed much of the vegetation and carried away most of the soil during the flooding of 1978. [11] [12]
In January 1978, the Ohio River rapidly rose from 29.6 feet on January 25 to 53.9 feet on January 30, during what has been described as "one of the most severe winter months in southwestern Ohio history." [13] This caused an enormous ice jam, which eventually broke, sending "a wall of ice and water" downstream. [13] It has been stated that the decisions and actions of the U.S. Army Corps of Engineers on January 27, 1978, at the Markland Dam, caused the ice jam to break. [13] This was characterized as being perhaps the worst disaster in modernity on the Ohio River, [14] and caused significant damage, with entire docks, barges and boats crammed against or forced through the Markland dam. [15] : 89–94 A towboat and seven barges sank at the dam, three barges were swept over the dam, six barges were unaccounted for, and 11 barges lodged against the dam producing a major pollution and explosion potential. [16] [13] The ice literally "shaved off" Big Bone Island at the time. [13]
The Ohio River is a 981-mile-long (1,579 km) river in the United States. It is located at the boundary of the Midwestern and Southern United States, flowing in a southwesterly direction from western Pennsylvania to its mouth on the Mississippi River at the southern tip of Illinois. It is the third largest river by discharge volume in the United States and the largest tributary by volume of the north-south flowing Mississippi River, which divides the eastern from western United States. It is also the 6th oldest river on the North American continent. The river flows through or along the border of six states, and its drainage basin includes parts of 14 states. Through its largest tributary, the Tennessee River, the basin includes several states of the southeastern U.S. It is the source of drinking water for five million people.
Boone County is a county located on the Ohio River in the northernmost part of the Commonwealth of Kentucky. As of the 2020 census, the population was 135,968, making it the fourth-most populous county in Kentucky. Its county seat is Burlington. The county was formed in 1798 from a portion of Campbell County and was named for frontiersman Daniel Boone. Boone County, with Kenton and Campbell Counties, is of the Northern Kentucky metro area, and the Cincinnati-Middletown, OH-KY-IN Metropolitan Statistical Area. It is the location of the Cincinnati/Northern Kentucky International Airport, which serves Cincinnati and the tri-state area.
The Monongahela River, sometimes referred to locally as the Mon, is a 130-mile-long (210 km) river on the Allegheny Plateau in north-central West Virginia and Southwestern Pennsylvania. The river flows from the confluence of its west and east forks in north-central West Virginia northeasterly into southwestern Pennsylvania, then northerly to Pittsburgh and its confluence with the Allegheny River to form the Ohio River. The river includes a series of locks and dams that makes it navigable.
Big Bone Lick State Park is located at Big Bone in Boone County, Kentucky. The name of the park comes from the Pleistocene megafauna fossils found there. Mammoths are believed to have been drawn to this location by a salt lick deposited around the sulfur springs. Other animals including forms of bison, caribou, deer, elk, horse, mastodon, musk ox, peccary, ground sloths, wolves, black bears, stag moose, saber-toothed cats, and possibly tapir also grazed the vegetation and salty earth around the springs that the animals relied on for their diet.
The Kentucky River is a tributary of the Ohio River in Kentucky, United States. The 260-mile (420 km) river and its tributaries drain much of eastern and central Kentucky, passing through the Eastern Coalfield, the Cumberland Mountains, and the Bluegrass region. Its watershed encompasses about 7,000 square miles (18,000 km2), and it supplies drinking water to about one-sixth of the population of the state.
The Mahoning River is a river in northeastern Ohio and a small portion of western Pennsylvania. Flowing primarily through several Ohio counties, it crosses the state line into Pennsylvania before joining with the Shenango River to form the Beaver River. The Mahoning River drops from 1,296 feet (395 m) at the headwaters near Winona to 761 feet (232 m) at the outfall near Mahoningtown, Pennsylvania. It is part of the Ohio River watershed. The name is said to derive from either the Lenape or Shawnee languages and mean "Deer Lick," as the area was once known for salt springs, but it's possible the name of the Mahoning and several other similarly named landmarks and places in western Pennsylvania could come from the Lenape, mënehokink (may-nuh-ho-keeng), meaning "place to get water."
Yatesville Lake is a reservoir in Lawrence County, Kentucky in the far eastern part of the state, close to the town of Louisa.
The Salt River is a 150-mile-long (240 km) river in the U.S. state of Kentucky that drains 2,920 square miles (7,600 km2). It begins near Parksville, Kentucky, rising from the north slope of Persimmon Knob south of KY 300 between Alum Springs and Wilsonville, and ends at the Ohio River near West Point. Taylorsville Lake is formed from the Salt River, and Guist Creek Lake is also in its drainage basin.
The Markland Locks and Dam is a concrete dam bridge and locks that span the Ohio River. It is 1395 feet long, and connects Gallatin County, Kentucky, and Switzerland County, Indiana.
Mary Draper Ingles, also known in records as Mary Inglis or Mary English, was an American pioneer and early settler of western Virginia. In the summer of 1755, she and her two young sons were among several captives taken by Shawnee after the Draper's Meadow Massacre during the French and Indian War. They were taken to Lower Shawneetown at the Ohio and Scioto rivers. Ingles escaped with another woman after two and a half months and trekked 500 to 600 miles, crossing numerous rivers, creeks, and the Appalachian Mountains to return home.
The Carroll Lee Cropper Bridge is a continuous steel arch-shaped truss bridge over the Ohio River between Indiana and Kentucky. Built between 1968 and 1977, the four-lane arched truss span provides a western Ohio River crossing for the Interstate 275 beltway around the Cincinnati area. The section of Interstate 275 on the Cropper bridge is the only Interstate highway in the Cincinnati, Ohio area that goes between Indiana and Kentucky.
The Licking River is a partly navigable, 303-mile-long (488 km) tributary of the Ohio River in northeastern Kentucky. The river and its tributaries drain much of the region of northeastern Kentucky between the watersheds of the Kentucky River to the west and the Big Sandy River to the east. The North Fork Licking River, in Pendleton County, Kentucky, is one of its tributaries. The South Fork Licking River, in counties including Harrison County, Kentucky, is another.
Hamilton is an unincorporated community in Boone County, Kentucky, United States. It is situated at Latitude 38.88333, Longitude -84.78167, in the southern part of the county on the Ohio River; it is about a mile north of the mouth of Big Bone Creek. It was established in 1835, being incorporated by the Kentucky Legislature as the Town of Landing. The plat laid out by Joel Hamilton and George McGlasson. The original trustees were: William Winston Jr., George McGlasson, Joel Hamilton, Henry L. Rose, James Dukan. The same year the Legislature provided a Constable for the town.
Bullitt's Lick is a historic salt lick 3 miles (4.8 km) west of Shepherdsville in Bullitt County, Kentucky. It was the first commercial supplier of salt in Kentucky, and the first industry in Kentucky as well, supplying jobs for many residents but also using slaves.
The following outline is provided as an overview of and topical guide to the United States Commonwealth of Kentucky:
Alum Creek State Park is a 4,630-acre (1,870 ha) Ohio state park in Delaware County, Ohio, in the United States. Alum Creek Lake was constructed from 1970 to 1974 as part of the Flood Control Act of 1962. Alum Creek Dam was constructed on Alum Creek, a tributary of Big Walnut Creek, which drains into the Scioto River. Alum Creek Reservoir holds 3,387 acres (1,371 ha) of water and is open to fishing, boating, ice fishing, ice boating, and swimming. The park is just north of the state capital of Columbus and contains the remnants of a settlement by freed slaves that arrived in Ohio from North Carolina.
Paleontology in Kentucky refers to paleontological research occurring within or conducted by people from the U.S. state of Kentucky.
Clendenin Magisterial District is one of ten magisterial districts in Mason County, West Virginia, United States. The district was originally established as a civil township in 1863, and converted into a magisterial district in 1872. In 2020, Clendenin District was home to 3,435 people.
{{cite book}}
: CS1 maint: postscript (link)