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"westwardly" Definitions
  1. in a westward direction
"westwardly" Antonyms

48 Sentences With "westwardly"

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

Looking straight into the ocean doesn't usually mean looking in a perfect eastwardly or westwardly direction.
In the southern part a railway road is crossing from East to Westwardly from Tiruchendur to Tirunelveli.
The Middle and South branches merge in Mckeever, New York and become just Moose River. It flows generally westwardly through Herkimer County into Lewis County, reaching its confluence with the Black River in Lyons Falls.
Near Kimbolton it turns westwardly and flows through southeastern Coshocton and northeastern Muskingum Counties, past Plainfield, to its mouth at the Muskingum River,DeLorme (1991). Ohio Atlas & Gazetteer. Yarmouth, Maine: DeLorme. 8 mi (13 km) south of the city of Coshocton.
Late in 1928 Colonial extended westwardly from Syracuse to Rochester, then early in 1929 eastwardly from Albany to Boston (in Massachusetts) and westwardly again from Rochester to Buffalo. In 1928 Colonial began acquiring the intrastate rights between Syracuse and Buffalo, by buying existing firms; that process continued until 1930, after it had become a member of the Greyhound family. In 1929 the Motor Transit Corporation (MTC) bought the Colonial Motor Coach Corporation, and (in a separate transaction) the MTC became renamed as The Greyhound Corporation. Colonial became renamed as the Eastern Greyhound Lines (EGL) of New York.
From Satires of Circumstance, Thomas Hardy's 1914 book of poems about Emma. :I found her out there :On a slope few see, :That falls westwardly :To the salt-edged air, :Where the ocean breaks :On the purple strand, :And the hurricane shakes :The solid land.
Gabrielle formed out of a low pressure system that quickly developed. It begin to move south east and soon weakened into a tropical low. It slowly tracked south and south westwardly, it slowly reintensified and gained tropical cyclone status. As an anticyclone possibly forming to the south of the system.
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.
The Little Sandy River, also known historically as "Hueys Creek" and "Prices Fork", flows for its entire length in southern Chester County, rising about 5 mi (8 km) south of the town of Chester and flowing westwardly to the Sandy River about 4 mi (7 km) northeast of the Sandy's mouth at the Broad River.
The Wild Rice River's largest tributaries are the White Earth River, which joins it near Mahnomen, and the South Branch Wild Rice River, which joins it in its lower course in Norman County; the South Branch rises near Ogema in northwestern Becker County and flows generally westwardly through Clay and Norman counties, past the town of Ulen.
Via the Bark and Rock rivers, it is part of the watershed of the Mississippi River. It rises in southwestern Waukesha County and flows generally westwardly into Jefferson County, past the village of Palmyra. It joins the Bark River in Jefferson County, north of Whitewater. The U.S. Board on Geographic Names settled on "Scuppernong River" as the stream's name in 1906.
The Mulberry River flows for most of its length through the Ozark National Forest in the Ozarks. It rises in southwestern Newton County and initially flows generally westwardly through Johnson and Franklin counties. In Franklin County it turns southward into the valley of the Arkansas River and flows past the town of Mulberry. It joins the Arkansas about south of Mulberry, on the common boundary of Franklin and Crawford counties.
The Mustinka River rises about south- southwest of Fergus Falls in southwestern Otter Tail County and initially flows generally southward into Grant County, passing through Stony Brook Lake and Lightning Lake. The river turns westwardly in southern Grant County and flows past Norcross into Traverse County, where it turns southwestward past Wheaton. It flows into the northern end of Lake Traverse from the east, about southwest of Wheaton.DeLorme (1994).
The reserve contains an artificial floating walkway, which provides a direct route to the lighthouse over lagoon R7. This lagoon is part of a series of a total of three lagoons spanning the coastal path (east to west). The most eastward lagoon (R9) is overlooked by a bird hide in addition to being viewable from a fenced overpass, and the most westwardly lagoon (R4) is viewable from a fenced overpass.
Hardwicke Parish is defined in the Territorial Division Act as being bounded: :Southwest by Glenelg Parish; north by Miramichi Bay; and southeast by the County line and the shore of the Gulf of St. Lawrence from Point Escuminac; westwardly to the intersection of the County line between Kent and Northumberland, near the entrance of Escuminac River, including all the islands in front, which are south of the principal entrance to Miramichi Bay.
The Salem River is a tributary of the Delaware River in southwestern New Jersey in the United States. The course and watershed of the Salem River are entirely within Salem County. Tributaries of the Salem include Game Creek, Mannington Creek, and Fenwick Creek. The river rises in Upper Pittsgrove Township and flows initially westwardly, through Pilesgrove Township and the borough of Woodstown and along the boundaries of Carneys Point and Mannington Townships.
The Gale River flows for its entire length in Grafton County. It rises in the White Mountains in the town of Franconia as two short, northward-flowing streams: its North Branch and its South Branch. The two streams join in Bethlehem, and the Gale River flows thence generally westwardly. Returning to Franconia, the river collects the Ham Branch, its most significant tributary, then passes through Sugar Hill to Lisbon, where it joins the Ammonoosuc River.
In 1515, Valerius Cordus was born either in the city of Erfurt in Thuringia, or somewhere in the westwardly adjacent state of Hesse. His father, Euricius Cordus (born Heinrich Ritze, 1486–1535), was an educated physician and an ardent Lutheran convert. Valerius began his higher education in 1527, at the young age of 12, studying botany and pharmacy under the tutelage of his father. In the same year he also enrolled at the University of Marburg.
Recife has a tropical monsoon climate (Am) bordering on a tropical wet and dry climate (As) under the Köppen climate classification, with warm to hot temperatures and high relative humidity throughout the year. However, these conditions are relieved by pleasant westwardly trade winds blowing in from the ocean. January and February are the warmest months, with mean temperatures ranging from to , with sun. July is the cloudiest month and experiences the coolest temperatures, with mean temperatures ranging from to .
Via the Kettle and St. Croix rivers, it is part of the watershed of the Mississippi River. The Willow River flows for its entire length in northern Pine County. It rises in the Nemadji State Forest in Nickerson Township and flows generally westwardly through Kerrick, Windemere, Norman and Kettle River townships, past Duquette. In Windemere Township it collects the Little Willow River, which rises at the town of Kerrick and flows through Bruno and Norman townships.
The coarser material was probably sourced by a nearby delta that was temporarily flooded during storm events. The dominance of those coarse sandstones towards the top of the eastern flat- pebble facies association might indicate delta progradation. The iron-oxide cements are interpreted as ferricretes, that either formed autochthonous or derived from adjacent reworked ferricrete crusts. An early uplift of the eastern hinterland might be indicated by coarse, westwardly prograding deltaic deposits of the upper Huab Formation in the eastern Huab area.
The river is 240 km long and its basin covers around 20,600 km². Thirty percent of the basin is located in the Andean range. It is born in Laguna del Maule in Talca Province, at an altitude of 2,200 mt in the vicinity of the border with Argentina. From that point the rivers flows westwardly and is soon joined on its left bank by one of its main tributaries, the Melado River, which is born in Laguna Dial, in Linares Province.
The Wild Rice flows from Mud Lake in Clearwater County and follows a generally westwardly course through Mahnomen and Norman counties, through the White Earth Indian Reservation and past the towns of Mahnomen, Twin Valley and Hendrum, and just south of Ada, where the nearby headwaters of the Marsh River sometimes act as a distributary to the Red River during periods of high water. In its lower reaches through the Red River Valley, portions of its course have been straightened and channelized.
At 18:00 UTC on September 28, the Japan Meteorological Agency (JMA) assessed the formation of a tropical depression near Palau. At 06:00 UTC the next day, the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert on the westwardly tracking disturbance, designating it as Tropical Depression 21W. Upon development, the storm showed signs of improving organization. Consolidation continued as the storm approached the Philippines at the eve of October, though intensification was tempered by increasing wind shear and interaction with the archipelago.
It rises near the town of Middle River and flows generally westwardly past the towns of Newfolden and Argyle. At Old Mill State Park the river crosses an old beach of glacial Lake Agassiz. Much of the Middle River's lower course through the Red River Valley has been straightened and channelized; for approximately its final , the Middle has been routed to flow due west in a straight line. It joins the Snake River not far upstream of that river's confluence with the Red River of the North.
The Bad Axe River flows for its entire length in western Vernon County, and for most of its length as two streams, the North Fork Bad Axe River and the South Fork Bad Axe River. The North Fork rises at the town of Westby and flows generally southwestwardly for . The South Fork rises about south of Viroqua and flows westwardly for . The main stem of the Bad Axe flows for less than westward from the convergence of the two forks to its confluence with the Mississippi, about south of Genoa.
According to the Geographic Names Information System, the river's name has also been historically spelled Togatatic and Totogatic. Its name is derived from the Ojibwe language Dootoogaatigo-ziibi meaning "River of Boggy Riverway" (or literally, "River of spongy-ground river-course"), due to its course through wetlands. The Totagatic is formed by the confluence of its short east and west forks in southwestern Bayfield County, and flows generally westwardly through Sawyer, Washburn, Douglas and Burnett counties, passing through several lakes. It joins the Namekagon River in Burnett County, south of the city of Superior.
From the convergence of its headwaters' forks, the Eau Claire River flows generally westwardly through northern Eau Claire County for about 40 mi (64 km), past the city of Altoona to its confluence with the Chippewa River in downtown Eau Claire. Two dams along its course in Eau Claire County cause the river to form two reservoirs: Lake Eau Claire and Lake Altoona. Upstream from Altoona, just north of the village of Fall Creek, the river passes over a waterfall known as Big Falls, which is the site of a county park.
The Sandusky River begins at the juncture of Paramour Creek and Allen Run at the unincorporated community of Leesville in Crawford County west of Crestline, and initially flows westwardly, passing through the town of Bucyrus. In Wyandot County, the river turns northward for the remainder of its course, flowing through Seneca and Sandusky counties and passing the towns of Upper Sandusky, Tiffin and Fremont before entering Sandusky Bay. In 1970, the river's course between Upper Sandusky and Fremont was designated as a State Scenic River by the government of Ohio.
The Buffalo River flows from Tamarac Lake in the Tamarac National Wildlife Refuge in central Becker County and flows generally westwardly into Clay County, past the towns of Hawley and Georgetown and through Buffalo River State Park. It flows into the Red River about west of Georgetown. The river's largest tributary is the South Branch Buffalo River, which rises in western Otter Tail County and flows initially westward into northern Wilkin County, then northward into Clay County. It joins the main stem of the river near Glyndon, Minnesota.
One branch of the river is the outlet of the Lakes of the Clouds in the saddle between Mount Washington and Mount Monroe. Leaving the vicinity of the Presidential Range, the river flows westwardly into Grafton County, where it turns southwestwardly. Along its course the Ammonoosuc passes through Chandler's Purchase, Bean's Grant, and Crawford's Purchase; and the towns of Carroll, Bethlehem, Littleton, Lisbon, Landaff, Bath, and Haverhill to the village of Woodsville, where it flows into the Connecticut River. It collects the Gale River in Lisbon, and the Wild Ammonoosuc River in Bath.
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.
The Buffalo River is formed at Osseo in northeastern Trempealeau County by the confluence of its North and South Forks, both of which are about long and rise in northwestern Jackson County; the North Fork has at times been considered the main stem of the river. From Osseo, the Buffalo flows westwardly into Buffalo County, past Strum, Eleva and Mondovi. At Mondovi the river turns southwestward for the remainder of its course; it flows into the Mississippi River northwest of Alma. For the last of the Buffalo's course, it is surrounded by marshland, before emptying into Rieck's Lake, a migratory stopover for thousands of tundra swans and other waterfowl.
The National Map , accessed October 5, 2012 and sometimes known as the main stem of the river, rises in northwestern Winnebago County, Iowa, approximately east of Rake, and flows westwardly into Kossuth County, Iowa, then northwardly into Faribault County. The West Branch, long, rises near Swea City, Iowa, in northern Kossuth County and flows northeastwardly into Faribault County. Both headwaters tributaries have been channelized for much of their courses. From their confluence the Blue Earth River flows northwardly in a winding course through eastern Faribault County into Blue Earth County, past the cities of Blue Earth, Winnebago, and Vernon Center, to Mankato, where it enters the Minnesota River from the south.
Just above Valley Green, Wise's Mill Road meets Forbidden Drive, connecting it to Henry Avenue in Roxborough. Wise's Mill Road may be the same as that described in Edgar Allan Poe's 1844 story "Morning on the Wissahiccon": "I would advise the adventurer who would behold its finest points to take the Ridge Road, running westwardly from the city, and, having reached the second lane beyond the sixth mile-stone, to follow this lane to its termination. He will thus strike the Wissahiccon, at one of its best reaches ...". Forbidden Drive ends at Northwestern Avenue (which is the county line) after crossing Bell's Mill Road.
Lone Mountain on the left Wartburg is located at (36.104244, -84.591817). The city is situated amidst the Crab Orchard Mountains, a sub-range of the Cumberland Mountains, near the eastern edge of the Cumberland Plateau. Bird Mountain dominates the area east of Wartburg, rising from its base at the edge of the city and stretching for some to its summit at Frozen Head State Park. The Emory River, its source near the summit of Bird, flows westwardly along the mountain's northern base, passing just north of Wartburg, and turning south before dropping off the plateau and emptying into the Watts Bar Lake impoundment of the Tennessee River.
It meanders in a generally north-westwardly direction, past Hamry nad Sázavou, Havlíčkův Brod, Sázava, Přibyslav, Nové Dvory, Pohled, Havlíčkův Brod, Světlá nad Sázavou, Ledeč nad Sázavou, Chřenovice, across the Vysočina-Central Bohemian border to Vlastějovice, Horka II , Zruč nad Sázavou, where it is joined by its right tributary Želivka, Kácov, Soběšín, Český Šternberk, Rataje nad Sázavou, Ledečko and Sázava-Černé Budy (Sázava Monastery). From here it flows generally westward, past Stříbrná Skalice, Chocerady, Hvězdonice, Senohraby (Zlenice castle), Čtyřkoly, Čerčany, Poříčí nad Sázavou, Nespeky, Týnec nad Sázavou, Krhanice, Kamenný Přívoz, reaching its confluence with the Vlatva (at the latter's 78.3 km mark) at the boundary between Hradištko and Davle, just south of the municipal border of Prague.
The Trempealeau River rises in western Jackson County as two streams, its North and South Branches; the South Branch has at times been known as the main stem of the river, and the North Branch has at times been known as "Bovee Creek". The two streams join just east of Hixton, and the Trempealeau initially flows generally westwardly into Trempealeau County, past Hixton, Taylor, Blair, Whitehall and Independence. Near Independence, the river turns to the southwest and flows past Arcadia; in its lower course, it is used to define the boundary between Trempealeau and Buffalo counties. The Trempealeau flows into the Mississippi River just downstream of Winona, Minnesota at Perrot State Park.
The Le Sueur River rises in Hartland Township in northwestern Freeborn County and flows initially northwardly, through the southwestern extremity of Steele County into Waseca County, then westwardly in a winding course into Blue Earth County, passing through St. Clair. It flows into the Blue Earth River southwest of Mankato, approximately three miles (5 km) upstream of the Blue Earth's mouth at the Minnesota River. Its largest tributaries are the Cobb and Maple Rivers, which it collects from the south approximately six and eight miles (10 km/13 km) upstream of its mouth, respectively. A minor tributary of the Le Sueur River in Waseca and Steele Counties is known as the Little Le Sueur River.
Principal tributaries of the Redwood River include Coon Creek, 37 miles (60 km) long, which flows from Lake Benton in Lincoln County westwardly to Russell in Lyon County; Three Mile Creek, 50 miles (81 km) long, which rises in Lincoln County and flows northeastwardly and southeastwardly through Lyon County, joining the Redwood downstream of Marshall; and Ramsey Creek, 10 miles (16 km) long, which flows over a waterfall in Ramsey City Park in Redwood Falls. Approximately 82% of the land in the Redwood River watershed is used for agriculture, primarily for the cultivation of corn and soybeans. Hundreds of miles of streams in the watershed have been converted to agricultural ditches, disrupting habitat and reducing the ability of the land to absorb flooding.
Stonecoal Creek is a tributary of the West Fork River, long, in north-central West Virginia in the United States. Via the West Fork, Monongahela and Ohio Rivers, it is part of the watershed of the Mississippi River, draining an area of on the unglaciated portion of the Allegheny Plateau. The stream is believed to have been named in the late 1760s by a group of explorers and settlers (including Jesse Hughes), who found coal in nearby hills and mixed with pebbles in the stream. Stonecoal Creek rises approximately five miles (8 km) west-northwest of Buckhannon in northwestern Upshur County and flows westwardly into northern Lewis County, where it joins the West Fork River from the east in the city of Weston.
Sailing west-to-east to circle the globe in a wind-driven craft is no small feat but rarely is the plan to go westwardly instead — the "wrong way around" — against the prevailing winds, currents and waves. This route puts immense stresses on the vessel and crew, and for solo sailors, days can pass with little or no sleep when the going is particularly hard. Few single-handers have attempted such a feat and certainly none near Saitō's age — when he finished this voyage he was 77 years and 8 months old. The voyage started with an October 2008 departure from Yokohama, and entailed a westward circumnavigation of , and expected arrival back in Yokohama in the spring of 2010, after 6 months. Instead, it took almost 3 years for him to successfully complete the circumnavigation.
Thence he went westwardly, and fell over on a stream > which he called Elk: at the mouth of this he erected a camp, and continued > to reside [there] for more than twelve months. During this time he neither > saw the Pringles nor any other human being; and at the expiration of it went > to the South Branch, where he disposed of his furs and skins and then > returned to, and continued at, his encampment at the mouth of Elk [present- > day Clarksburg], until permanent settlements were made in the > vicinity.Withers, Alexander Scott (1831), Chronicles of Border Warfare, or, > A History of the Settlement by the Whites, of north-western Virginia: and of > the Indian wars and massacres, in that section of the state; with > reflections, anecdotes, &c.;, Clarksburg, Va.: J. Israel, pg 90.
The remaining part of the line is in a > westwardly direction, crossing the Kelvin River by a noble aqueduct, and > thence to the Clyde, into which, after running parallel with it for some > distance, it locks down at Bowling's Bay, near Dalmuir Burnfoot. The canal > is in length, viz, from Grangemouth to the east end of the summit pool, is > ten miles and three quarters [], with a rise, from low water in the Forth, > of , by twenty locks. The summit level is in length, and in the remainder of > its course, there is a fall to low water, in the Clyde, at Bowling's Bay, of > , by nineteen locks. The branch to the Monkland Canal at Glasgow is two > miles and three quarters []; and there is another cut into the Carron River, > at Carron Shore, in order to communicate with the Carron Iron Works.
Tributaries of the river in its upper course include the East Branch Blue Earth River, long, which rises in southwestern Freeborn County and flows westwardly through Faribault County to the city of Blue Earth; and Elm Creek, long, which rises in northeastern Jackson County and flows eastwardly through Martin County into northeastern Faribault County, where it joins the Blue Earth River near Winnebago. The Blue Earth River flows in most of its course through till plains and the plain of a former glacial lake. The drain of the glacial lake, Union Slough, drains in two directions, south into the East Fork of the Des Moines River and north, as Union Slough, into the West Branch of the Blue Earth River. The lower (northern) part of the river's watershed was historically covered by the Big Woods, a tract of hardwoods that has since been largely converted to agricultural use; segments of the woodland extended southward along the riparian corridors of the Blue Earth River and its tributaries.
Below the dam and after returning fully to Pennsylvania, the Shenango flows south-southeastwardly into Mercer County, flowing through Jamestown and Greenville before turning westwardly into Shenango River Lake, formed in 1965 by a United States Army Corps of Engineers dam.United States Army Corps of Engineers website for Shenango River Lake Below that dam, the Shenango flows southwestwardly through the communities of Sharpsville and Sharon (near which it briefly enters Trumbull County, Ohio); then south-southeastwardly past Farrell, Wheatland and West Middlesex into Lawrence County, where it passes New Castle and Oakland. It joins the Mahoning River to form the Beaver River, 3 mi (4.8 km) southwest of New Castle. Tributaries of the Shenango include the short Little Shenango River, which flows for its entire length in Mercer County and joins the Shenango from the east at Greenville; Pymatuning Creek, which flows into Shenango River Lake; and Neshannock Creek, which joins the river at New Castle.
Hackers Creek is a tributary of the West Fork River, long, in north-central West Virginia in the United States. Via the West Fork, Monongahela and Ohio Rivers, it is part of the watershed of the Mississippi River, draining an area of on the unglaciated portion of the Allegheny Plateau. The stream is believed to have been named for a settler named John Hacker (1743-1824), who lived near the creek for over twenty years beginning around 1770, and was said to have been able to "read but not write; and yet he was a magistrate and a patriarch in the settlement." Hackers Creek rises approximately north of Buckhannon in northern Upshur County and flows westwardly into northeastern Lewis County, where it turns northwestwardly and flows through the town of Jane Lew into southern Harrison County, where it joins the West Fork River from the southeast, approximately three miles (5 km) northwest of Jane Lew.
Priestley wrote in 1831, > Besides the fine rivers above-mentioned [the Forth and Clyde, the canal], is > joined by the Edinburgh and Glasgow Union Canal, near Falkirk; with the > Monkland and Kirkintilloch Railway at its summit, near the last-mentioned > village; and with the Monkland Canal and the Garnkirk and Glasgow Railway, > at Port Dundas, near the city of Glasgow. This magnificent canal commences > in the River Forth, in Grangemouth Harbour, and near to where the Carron > empties itself into that river. Its course is parallel with the Carron, and > in nearly a westwardly direction, passing to the north of the town of > Falkirk, and thence to Red Bridge, where it quits the county of Stirling, > and enters a detached portion of the shire of Dumbarton. Hence it passes to > the south of Kilsyth, and runs along the south bank of the River Kelvin, and > over the Luggie Water, by a fine stone aqueduct, at Kirkintilloch; it then > approaches within little more than of the north-west quarter of the city of > Glasgow, to which there is a branch communicating with the Monkland Canal at > Port Dundas, near that city.

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