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"southwardly" Definitions
  1. in a southern direction
"southwardly" Antonyms

51 Sentences With "southwardly"

How to use southwardly in a sentence? Find typical usage patterns (collocations)/phrases/context for "southwardly" and check conjugation/comparative form for "southwardly". Mastering all the usages of "southwardly" from sentence examples published by news publications.

After millennia spent stewing about timing his southwardly invasion, he's finally showing some follow-through.
It prefers open and dry habitats on southwardly directed slopes, margins of light spruce forest with interspersed rocks, margins of forest and scrubs in mountainous areas, as well as in elfin woodland. It has also been found in sub-alpine dwarf scrub. The adults feed on some shrubs, including Pinus mugo.
The National Map , accessed May 26, 2011 and drains an area of . Via the Des Moines River, it is part of the watershed of the Mississippi River. The Boone River rises near Britt in western Hancock County and flows generally southwardly through Wright, Hamilton and Webster counties, past Goldfield and Webster City.DeLorme (1998).
115Stickney, 1926: p. 46 Intense fighting occurred in the region of Cepo, north of Gjirokastër, where Albanian gendarmerie units tried unsuccessfully to infiltrate southwardly, facing resistance from the Northern Epirote forces.Miller, 1966, p. 519 On the other hand, the Epirotes managed to advance and gain control of Erseka and further advanced on Frashër and Korçë.
After Jurriaen Boekholt died in April 1599, Pomp was given command of the Blijde Boodschap ("Good Tiding" or "Gospel").This vessel, a jacht, was also known as Vliegende Hert("Flying Deer"). Strong and adverse winds dispersed the fleet when it left the Straits of Magellan. The Blijde Boodschap was blown off her course southwardly.
Wakatomika Creek rises in western Coshocton County and flows westwardly into Knox County; then southwardly into northeastern Licking and southwestern Coshocton Counties; and eastwardly through northwestern Muskingum County, past the southern edge of the village of Frazeysburg. It joins the Muskingum River from the west at the village of Dresden.DeLorme (1991). Ohio Atlas & Gazetteer.
Lewis Run begins in southeastern Ross Township. It flows south- southeast for a few hundred feet before turning southwest. The stream then turns west and enters a valley. It then gradually turns south and flows in a generally southwardly direction for a few miles, flowing in its valley alongside State Route 4029 and entering Hunlock Township.
Via the Ohio River, it is part of the watershed of the Mississippi River, draining an area of .Map of Ohio watersheds The Little Scioto River rises in western Jackson County and flows generally southwardly into Scioto County, near Minford. It flows into the Ohio River in the eastern part of the city of Portsmouth,DeLorme (1991). Ohio Atlas & Gazetteer.
Map of Ohio watersheds According to the Geographic Names Information System, it has also been known historically as "Brush Creek," "Elk Creek," and "Little Scioto River". Ohio Brush Creek rises in southeastern Highland County, and flows generally southwardly into Adams County, past the Serpent Mound, to its confluence at the Ohio River, about west of Rome.DeLorme (1991). Ohio Atlas & Gazetteer.
Rush River (Wisconsin), below STH 29 The Rush River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map, accessed October 5, 2012 tributary of the Mississippi River in western Wisconsin in the United States. It rises just north of Interstate 94 in St. Croix County near Baldwin and flows generally southwardly through Pierce County.
Duck Creek is formed in the hill country of northern Washington County at the community of Warner, just west of Lower Salem and approximately 15 mi (24 km) north of Marietta, by the confluence of East Fork Duck Creek and West Fork Duck Creek. The East Fork, approximately 20 mi (30 km) long, rises in western Monroe County and flows generally southwardly through eastern Noble and northern Washington Counties. The West Fork, approximately 30 mi (50 km) long, rises in southeastern Guernsey County and flows generally south-southeastwardly through central Noble and northern Washington Counties, past the towns of Belle Valley, Caldwell, Dexter City and Macksburg; it is the larger of the two headwaters streams. From Warner, Duck Creek flows generally southwardly in a highly meandering course and joins the Ohio River at Marietta, about 3 mi (5 km) east of its downtown.
The Anderson rises in western Crawford County in the Hoosier National Forest and flows generally southwardly through southeastern Dubois County and along the common boundary of Perry and Spencer counties, east of the town of Saint Meinrad. It joins the Ohio River just downstream of the town of Troy. Near its mouth it collects the Middle Fork Anderson River, which flows for its entire length in Perry County.
The Whitewater River rises in southern Marion County (southeast of Peabody) and flows southwardly into Butler County, past the towns of Potwin and Towanda, then joins the Walnut River at Augusta. In Butler County, the river collects the West Branch Whitewater River, which rises in Harvey County and flows southeastwardly past Whitewater; and the East Branch Whitewater River, which rises near Burns in Marion County and flows southwestwardly.
Trimbelle River, at Trimbelle, WI The Trimbelle River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map, accessed October 5, 2012 tributary of the Mississippi River in western Wisconsin in the United States. It flows for its entire length in western Pierce County, rising in the town of Martell and flowing generally southwardly through the towns of River Falls, Trimbelle, Trenton and Diamond Bluff.
The Paint Rock River is a tributary of the Tennessee River in northern Alabama in the United States. Its tributaries also drain a portion of south- central Tennessee. The river is formed in northeastern Jackson County by the confluence of Estill Fork and Hurricane Creek, and flows generally southwardly, past the town of Paint Rock. In its upper course, the river flows through a deep valley cut into the Cumberland Plateau.
A map of Japan Japanese archipelago with outlined islands The Japanese archipelago is over long in a north-to-southwardly direction from the Sea of Okhotsk to the Philippine Sea in the Pacific Ocean. It is narrow, and no point in Japan is more than from the sea. There are 6,852 islands in total. The five main islands are (from north to south) Hokkaido, Honshu, Shikoku, Kyushu and Okinawa.
The Ottawa Islands and the southwardly Belcher Islands are a breeding ground for "the Hudson Bay subspecies of the Common Eider"."National Marine Conservation Areas of Canada: Canada's National Marine Conservation Areas System Plan: James Bay: The Wildlife". Parks Canada , Last Updated: 2006-11-17, Accessed 01-26-2007. In 1765 commercial whaling of bowheads was started by Churchill-based sloops of the Hudson's Bay Company with some whales being harvested in the Ottawa Islands.
It was the curse of heaven on the states where it prevailed. Compare the free regions of the Middle States, where a rich & noble cultivation marks the prosperity & happiness of the people, with the misery & poverty which overspread the barren wastes of Va. Maryd. & the other States having slaves. ... Proceed southwardly, and every step you take, through the great regions of slaves, presents a desert increasing with the increasing proportion of these wretched beings.
According to the Hydrographic Center of the Brazilian Navy, on December 9, 2017, a subtropical storm formed over the southeastern tip of a South Atlantic Convergence Zone, being located close to the state border between Espírito Santo and Bahia, moving southeastwards away from land. On early December 11, as it moved more southwardly, Guará attained its peak intensity while transitioning to an extratropical cyclone. Shortly thereafter, Guará became fully extratropical, later on the same day.
The Platte River rises near Creston in Union County, Iowa, and flows generally southwardly through Adams, Ringgold and Taylor Counties in Iowa; and Worth, Nodaway, Andrew, Buchanan and Platte Counties in Missouri. Along its course it passes the Iowa towns of Maloy, Blockton and Athelstan; and the Missouri towns of Sheridan, Parnell, Ravenwood, Conception Junction, Guilford, Tracy, Platte City and Farley. The Platte flows into the Missouri River near Farley, downstream of Leavenworth, Kansas.DeLorme (1998).
The East Branch is 10.4 miles (16.7 km) long and flows through Louisville; the Middle Branch is 16.6 miles (26.6 km) long. Shortly downstream of this confluence, the stream collects the West Branch Nimishillen Creek, which is nine miles (14.5 km) long and flows through North Canton and Canton. From Canton, Nimishillen Creek flows generally southwardly, past East Sparta, into northern Tuscarawas County, where it flows into Sandy Creek from the north.
The Headingly cum Burley Inclosure Award (1834) refers to various intakes when describing the roads and paths set out. for example: > 'Oates Road:- One other private occupation of the width and in the direction > that it is now branching from Holling Lane between two Intakes called Stoney > Close and Harris Close belonging to the Curate of Headingly and leading in a > Southwardly direction to and into an allotment on Headingly Moor set out for > Edward Oates Esquire.
The Rock River starts in Pipestone County, Minnesota, approximately northeast of the town of Pipestone, and flows initially southwardly through Rock County, Minnesota, and Lyon County, Iowa, where it turns southwestward into Sioux County, Iowa. It flows into the Big Sioux River in Sioux County, north of Hawarden. Along its course the Rock River passes the towns of Holland, Edgerton, Luverne and Ash Creek in Minnesota; and the towns of Rock Rapids, Doon and Rock Valley in Iowa.
It flows for its entire length in southern Saint Louis County. Its name in the Ojibwe language is askibwaanikaa-ziibi (river full of Jerusalem artichokes), having the identical name in Ojibwe as the nearby Us-kab-wan-ka River. The river flows from Artichoke Lake in New Independence Township and flows generally southwardly through Alborn and Culver Townships. It flows into the Saint Louis River from the north in Culver Township, opposite the town of Brookston.
The Boyer River rises near Storm Lake in southwestern Buena Vista County and initially flows southwardly into Sac County. In southern Sac County it turns southwestward and flows through Crawford, Harrison and Pottawattamie Counties, past the towns of Deloit, Denison, Arion, Dow City, Dunlap, Woodbine, Logan and Missouri Valley. It enters the Missouri River in northwestern Pottawattamie County, north of Council Bluffs. At Denison, the Boyer collects the East Boyer River, which rises in northwestern Carroll County and flows southwestwardly past Vail.
The Hay River begins at the city of Cumberland in Barron County, where it flows from Beaver Dam Lake. It flows generally southwardly through western Barron and northern Dunn Counties, past the villages of Prairie Farm and Wheeler. It joins the Red Cedar River in Dunn County as part of Tainter Lake at a settlement of the same name. Upstream of Wheeler, the river collects the South Fork Hay River, which rises in southeastern Polk County and flows south-southeastwardly, past the community of Connorsville.
During the construction, the weight of the water had to be included in the tension of the tower, which is why it stood southwardly inclined before the completion. The tower stands on a base construction which includes three basements which accommodate company / technical equipment. Because the location of the tower lies in the seismic zone of Basel – Erdbebengebiet in the Upper Rhine district, this has been built especially securely about the base. The tower should remain stable in an earthquake up to 8 on the Richter scale.
In 1792 he became and remained the Clerk of the County Court of that new county in whose minutes his beautiful penmanship appears. He, and General Joseph McDowell and Mussendine Matthews as North Carolina commissioners superintended in 1799 the running of the line between North Carolina and Tennessee from the southern border of Virginia southwardly across Big Pigeon River. In consequence of some conversation when engaged in that work he wrote recollections of the Battle of Kings Mountain published many years after his death. He was a colonel of militia.
Dongpo Park is located in the east part of downtown of Changzhou city, and its original name is Dongjiao Park. It covers 2.667 hectares, and is a typical Jiangnan Garden composed of cultural sites and natural landscape. During the time of south Song dynasty, the civilians of Changzhou established Yizhou Pavilion to commemorate, Su Dongpo, who was the great literature master and used to come to Changzhou. During the time of Qing dynasty, Kangxi and Qianlong, two emperors southwardly visited, they ordered to build up the temporary palace here and reconstructed this pavilion.
Significant portions of the Yellow River's course have been straightened and channelized; the river's present-day course is considered to begin at a confluence of agricultural ditches in southeastern St. Joseph County, approximately north of the town of Bremen. The river initially flows southwardly into Marshall County, past Bremen; then generally southwestwardly, returning to its naturally winding riverbed and flowing through the city of Plymouth; and westwardly in a substantially straightened course through Starke County, past the city of Knox. It flows into the Kankakee River in southwestern Starke County, approximately west of Knox near the town of English Lake.
After the summer monsoon recedes (Oct-Nov): During this period, the southwest monsoon winds continually weaken, so the Northward Somali Current (extension flow of the EACC) no longer crosses the equator, turning instead to the east at around 3°N. However, the Great Whirl still remains. Southwestward current (Dec-Feb, Winter Monsoon): During the fall (Sep-Nov), with the strengthening northeast monsoon influencing it, the Somali Current gradually becomes weaker and slower. Finally, in early December, beginning south of 5°N and expanding rapidly to 10°N by January, the current reverses its direction, now flowing southwardly (velocities of 0.7 – 1.0 m/s).
Later on, however, the Neotropic species proved far less successful than the Nearctic. This difference in fortunes was manifested in several ways. Northwardly migrating animals often were not able to compete for resources as well as the North American species already occupying the same ecological niches; those that did become established were not able to diversify much, and in some cases did not survive for long. Southwardly migrating Nearctic species established themselves in larger numbers and diversified considerably more, and are thought to have caused the extinction of a large proportion of the South American fauna.
The Uwharrie River rises in northwestern Randolph County, just south of the city of High Point, and flows generally southwardly into northwestern Montgomery County, through the low Uwharrie Mountains and the Uwharrie National Forest. It flows into the Pee Dee River 8 mi (13 km) east of the city of Albemarle as part of the Lake Tillery reservoir, across the Pee Dee from Morrow Mountain State Park. Above the mouth of the Uwharrie, the Pee Dee is known as the Yadkin River. In its upper course, the Uwharrie collects a minor tributary named the Little Uwharrie River, which flows for a short distance through northwestern Randolph County.
In Athens County north of Glouster it collects the East Branch Sunday Creek, 15.5 miles (25 km) long, which rises in Perry County and passes through Morgan County. Tom Jenkins Dam, constructed on the East Branch in Athens County in 1950 by the U.S. Army Corps of Engineers, forms Burr Oak Lake, the site of Burr Oak State Park. In Glouster, Sunday Creek collects the West Branch Sunday Creek, 14 miles (22.5 km) long, which rises in Perry County and flows generally southwardly. Other significant Tributaries include Greens Run, Mud Fork, and Johnson Run, all perennial streams draining the area to the west of the creek.
Thetford The Ompompanoosuc River Columbia Gazetteer of North America entry is a river, about 25 mi (40 km) long, in eastern Vermont in the United States. It is a tributary of the Connecticut River, which flows to Long Island Sound. According to the Geographic Names Information System, the river has also been known by the names "Om-pom-pa-noos-uc" and "Pompanoosuc." The Ompompanoosuc River rises in eastern Orange County in the town of Vershire, and flows generally southwardly through the towns of West Fairlee and Thetford into northeastern Windsor County, where it joins the Connecticut River in the village of Pompanoosuc which is located in the town of Norwich.
The river rises in a region of granite mountains in Iron County, Missouri, and flows generally southwardly through the Ozarks and the St. Francois Mountains near Missouri's highest point Taum Sauk. It forms the Missouri-Arkansas border in the Bootheel and eventually exits the state at Missouri's lowest point in the "toe" at above sea level. It passes through Lake Wappapello, which is formed by a dam constructed in 1941. Below the dam the river meanders through cane forests and willow wetlands or forested swamp, transitioning from a clear stream into a slow and silt-laden muddy river as it enters the flat lands of the Mississippi embayment.
The Little Wabash rises in Coles County near Mattoon and flows generally southwardly through Shelby, Effingham, Clay, Richland, Wayne, Edwards and White counties, past the towns of Louisville, Golden Gate, Carmi and New Haven. It enters the Wabash River on the common boundary of White and Gallatin counties, about southeast of New Haven. In its upper course in Shelby County, the river is dammed to form Lake Mattoon and collects the short West Branch Little Wabash River, which flows for its entire length in Shelby County. Other tributaries include the Fox River, which joins it in Edwards County; the Elm River, which joins it in Wayne County; and the Skillet Fork, which joins it in White County.
SR 536 became SR 190 in the 1933 renumbering, and in October 1933 it was extended another , taking it across the North Landing River to SR 615.: "1. Be it enacted by the General Assembly of Virginia, That the location of route number one hundred and ninety of the State highway system, formerly route number five hundred and thirty-six in Princess Anne county, shall be southwardly from the Norfolk county line to a point near Blackwater river, and thence eastwardly across North Landing river to connect with Munden Point road." SR 190 was downgraded to secondary SR 726 in 1952, effective once the new Pungo Ferry Bridge (which replaced Pungo Ferry) was complete, which happened in 1954.
In Article VI the lands ceded: :Beginning at fort Clark, on the Missouri, five miles above Fire Prairie, and running thence a due south course to the river Arkansas, and down the same to the Mississippi; hereby ceding and relinquishing forever to the United States, all the lands which lie east of the said line, and north of the southwardly bank of the said river Arkansas, and all lands situated northwardly of the river Missouri. And we do further cede and relinquish to the United States forever, a tract of two leagues square, to embrace fort Clark, and to be laid off in such manner as the President of the United States shall think proper.
The Saint Francis River is a tributary of the Elk River in east-central Minnesota in the United States. Via the Elk River, it is part of the watershed of the Mississippi River, draining an area historically characterized by mixed hardwood and coniferous forests on flat to rolling till plains. The St. Francis River rises in Alberta Township in northeastern Benton County, and flows generally southwardly through eastern Benton County, passing to the east of Foley and collecting a minor tributary known as the West Branch St. Francis River. The river turns eastward in northern Sherburne County, and flows south- and southwestwardly through the Sherburne National Wildlife Refuge and Sand Dunes State Forest.
The township, the ninth in order of creation, was erected from Lemon Township by the Butler County Commissioners on May 7, 1810, following a petition by residents of the district. Its boundaries were: :Beginning on the west bank of the Miami at the southwest corner of township No. 1 of the fourth range; thence north with the western boundary line of the said fourth range to the boundary line of the said county of Butler; thence east with the said northern boundary line to the Miami; thence south and southwardly with the meanders of the Miami to the place of the meanders of the Miami to the place of beginning. The first election for township officers was on May 19, 1810.
The legislation that created Heele County declared: > That the territory comprised within the following limits, be erected into a > county to be called Heele: commencing at the south east corner of Town Range > 4, North 69 West; thence north to the north east corner of Town 69 West > Range 10 North, thence west to the summit of the Rocky Mountains; thence > southwardly to the north west corner of Jackson county; thence east to the > place of beginning. Heele County encompassed much of what is today Larimer County, Colorado. The Jefferson Territory never received federal sanction, but on February 28, 1861, U.S. President James Buchanan signed an act organizing the Territory of Colorado. On November 1, 1861, the Colorado General Assembly organized 17 counties, including Larimer County, for the new Colorado Territory.
The Pomme de Terre River issues from Stalker Lake in Tordenskjold Township, approximately three miles (5 km) northeast of Dalton in southern Otter Tail County, and flows generally southwardly through eastern Grant and Stevens Counties and western Swift County, through the cities of Barrett, Morris, and Appleton. It flows into Marsh Lake on the Minnesota River in southwestern Swift County, approximately four miles (6 km) southwest of Appleton. Marsh Lake was formed by a backup of water caused by the Pomme de Terre's delta, and is presently maintained by a manmade dam. In its upper course the river flows through a morainic region of numerous lakes, in a course characterized by meadows and wooded hills, as well as marshy stretches near areas where the river passes through lakes.
The accord was proclaimed on December 30, 1825.Oklahoma State University Library (Kappler Project: Indian Affairs: Laws and Treaties) - Treaty With The Osage, 1825 (Article I) The Great and Little Osage Tribes or Nations do, hereby cede and relinquish to the United States, all their right, title interest and claim, to lands lying within the State of Missouri and Territory of Arkansas, and to all lands lying West of the said State of Missouri and Territory of Arkansas, North and West of the Red River, South of the Kansas River, and East of a line to be drawn from the head sources of the Kansas, Southwardly through the Rock Saline, with such reservations, for such considerations, and upon such terms as are hereinafter specified, expressed, and provided for.
Sunday Creek is a tributary of the Hocking River, 27.2 miles (43.8 km) long, in southeastern Ohio in the United States. Via the Hocking and Ohio Rivers, it is part of the watershed of the Mississippi River, draining 139 square miles (360 km²) in a mainly rural area of the Allegheny Plateau region. Its name is locally said to derive from early white settlers who in 1802 reached the creek on a Sunday, and so named it after the day of their discovery. (also see nearby Monday Creek.) Sunday Creek rises in southeastern Perry County and flows generally southwardly into northern Athens County, passing through the communities of Rendville, Corning, Glouster, Trimble, Jacksonville, and Millfield (site of the 1930 Millfield Mine disaster), to Chauncey, where it flows into the Hocking River.
Columbia Gazetteer of North America entry According to the Geographic Names Information System, it has also been known historically as "Wantastiquet" and as "Waters of the Lonely Way". Its watershed covers ; land use is about 90% forested and 3% agricultural, and the upper river supports wild native brook and wild brown trout, while Atlantic salmon occur in most of the river.West River basin summary The West River rises in the Green Mountains in the town of Mount Holly in southeastern Rutland County and flows southwardly through southwestern Windsor County into Windham County, where it turns southeastwardly. Along its course it flows through or along the boundaries of the towns of Weston, Londonderry, Jamaica, Townshend, Brookline, Newfane (where it collects the Rock River), and Dummerston to Brattleboro, where it flows into the Connecticut River.
This line divided Hardwick Township with its lands north of the line being ceded to create the townships of Green and Stillwater. The line also divided Walpack Township with the lands south of the line being ceded to create Pahaquarry Township in Warren County. Another line of partition, the Lawrence Line of 1743, is still extant in the boundaries of four Sussex County municipalities. This line was drawn by surveyor John Lawrence to provide final resolution after 67 years of disputes to the division of New Jersey into the two proprietary colonies of the Province of West Jersey and Province of East Jersey in accordance with the Quintipartite Deed (1676), divided the state in a straight line from "the Northernmost Branch of said Bay or River of De la Ware which is in forty-one Degrees and forty minutes of latitude...unto the most southwardly poynt of the East syde of Little Egge Harbour".
This area was also swampy, and would require much engineering effort and funds to cross with a road. On November 25, 1808, at Brownstown in Michigan Territory, the United States and five nations of Indians signed the Treaty of Brownstown. \- Text of Treaty of Brownstown Library of Congress Article II of the treaty called for the Indian Nations to cede to the United States “…also a tract of land, for a road only, of one hundred twenty feet in weadth, to run southwardly from what is called Lower Sandusky, to the boundary line established by the Treaty of Greenville, with the privilege of taking at all times, such timber and other materials, from the adjacent lands as may be necessary for making and keeping in repair the said road, with the bridges that may be required along the same.” Lower Sandusky is now called Fremont, Ohio and the boundary line of the Greenville Treaty lies in southern Marion County.
The treaty specifically cedes the following land: :And in consideration of the advantages which we derive from the stipulations contained in the foregoing articles, we, the chiefs and warriors of the Great and Little Osage, for ourselves and our nations respectively, covenant and agree with the United States, that the boundary line between our nations and the United States shall be as follows, to wit: beginning at fort Clark, on the Missouri, five miles above Fire Prairie, and running thence a due south course to the river Arkansas, and down the same to the Mississippi; hereby ceding and relinquishing forever to the United States, all the lands which lie east of the said line, and north of the southwardly bank of the said river Arkansas, and all lands situated northwardly of the river Missouri. And we do further cede and relinquish to the United States forever, a tract of two leagues square, to embrace fort Clark, and to be laid off in such manner as the President of the United States shall think proper.
The river was named after the Lakota people (Sioux Natives) which was known by them as Tehankasandata, or Thick Wooded River. The Big Sioux River rises in Roberts County, South Dakota on a low plateau known as the Coteau des Prairies and flows generally southwardly through Grant, Codington, Hamlin, Brookings, Moody, and Minnehaha counties, past the communities of Watertown, Castlewood, Bruce, Flandreau, Egan, Trent, Dell Rapids, and Baltic to Sioux Falls, where it passes over a waterfall in Falls Park, which gives that city its name. Downstream of Sioux Falls and the community of Brandon, the Big Sioux is used to define the boundary between South Dakota and Iowa, flowing along the eastern borders of Lincoln and Union counties in South Dakota, and the western borders of Lyon, Sioux and Plymouth counties in Iowa, past the communities of Canton, Fairview, Hudson, Hawarden, North Sioux City, and Dakota Dunes in South Dakota and Beloit, Hawarden and Akron in Iowa. It joins the Missouri River from the north at Sioux City, Iowa.
In the Treaty of Fort Clark in 1808, the Osage Nation, the most influential tribe in Missouri, ceded all lands west of Fort Clark near Sibley, Missouri in Jackson County, Missouri. In exchange for this, the tribe was paid merchandise worth $1,500 along with a fort to protect them and a government sanctioned trading post. Treaty of the Osage 1808 . The specific boundaries: :And in consideration of the advantages which we derive from the stipulations contained in the foregoing articles, we, the chiefs and warriors of the Great and Little Osage, for ourselves and our nations respectively, covenant and agree with the United States, that the boundary line between our nations and the United States shall be as follows, to wit: beginning at Fort Clark, on the Missouri, five miles above Fire Prairie, and running thence a due south course to the river Arkansas, and down the same to the Mississippi; hereby ceding and relinquishing forever to the United States, all the lands which lie east of the said line, and north of the southwardly bank of the said river Arkansas, and all lands situated northwardly of the river Missouri.

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