In places along the volcano's base, lava flows can be seen spilling out into the surrounding plains, forming broad aprons, and burying the basal escarpment.

Through the cul-de-sac between Baydağlari and Tahtalidağlari, the Alakir Çay (" Alakir River "), the ancient Limyra, flows to the south trickling from the broad valley under superhighway D400 near downtown Kumluca across a barrier beach into the Mediterranean.

From Northampton, the river flows along a broad valley, formed by the enormous amount of water released by the melting ice during the Ice Age, towards the east coast.

The river Weser flows westward along the south of the Wiehengebirge through a broad valley and the town of Rinteln.

Located north of the city, it consists of a broad area of scattered quaternary pyroclastic cones and associated basaltic lava flows.

Over long periods of time, the gradual buildup of thousands of these flows slowly constructs the characteristically low, broad profile of a mature shield volcano.

The Mangfall River, a short but broad affluent of the Inn River, flows northward with the district's municipalities on either bank.

Below the two source streams Dunajec flows through a broad valley called Nowotarska Basin.

It lies some 80 km to the west of the city centre, at the foot of the Rock and Pillar Range of hills in the broad Strath-Taieri valley, through which flows the middle reaches of the Taieri River.

The Gomal River, which has a varied flow depending on season, runs from its origin in the mountains of the Sar Hawza District and flows south, before turning southeast to the Pakistani border, forming the broad river valley that defines the topography of the Gomal District, before flowing east through Pakistan and eventually running to the powerful Indus River.

The low-gradient Chickahominy sluggishly flows through broad swampy lowlands for from Henrico County to eastern New Kent County.

The Green River flows through Split Mountain Canyon before leaving Dinosaur National Monument in a meandering path across a broad irrigated flood plain

It flows through one of the largest and most gorgeous gorges in Central Europe, the Rappenloch Gorge, down to Dornbirn, cuts through the town and the meanders off over a broad meadow landscape, the Lauterach Ried, finally flowing, parallel and quite close to the mouth of the Rhine, into Lake Constance.

Hawaiian volcanic eruptions are also characterised by lavas with low silica content, but the Hawaiian volcanoes are broad, shallow-sloped shield volcanoes in contrast to the steep-sided cone of Nyiragongo, and the silica content is high enough to slow most Hawaiian flows to walking pace.

It flows west, then northwest, past Meeker ( site of the White River Museum ), and across the broad valley between the Danforth Hills on the north and the Roan Plateau on the south.

At Little Ferry, it is joined by the broad Overpeck Creek, then flows southward, widening in a broad meandering tidal estuary through the Meadowlands, forming extensive side streams and wetlands.

The Missouri River Trench is the geological name applied to the broad valley of the Missouri River as it flows southward through North Dakota and South Dakota in the United States.

Below that, to the west of Lake Tapps, the White River enters a broad floodplain and flows past the city of Pacific before emptying into the Puyallup River at Sumner.

Downstream from the dam, the Osage flows freely to the northeast in broad oxbow meanders through forested bluffs, joining the Missouri approximately east and downstream of Jefferson City.

The river flows north in a slow meandering course through a broad flat valley called the Teton Basin ( formerly known as " Pierre's Hole "), flanked by the Teton Range to the east and the Big Hole Mountains to the west.

Emerging from Island Park Reservoir, the river flows through a canyon that then opens up into a broad, flat meadow located in the Island Park Caldera in central Fremont County.

It flows southwest across the plain, past St. Anthony, splitting into multiple channels into a broad inland delta north of Rexburg.

The North Fork ( 250 mi / 400 km ) rises in the Kuskokwim Mountains approximately 200 miles ( 320 km ) WSW of Fairbanks and flows southwest in a broad valley.

Escher's lithograph Waterfall depicts a watercourse that flows in a zigzag along the long sides of two elongated Penrose triangles, so that it ends up two stories higher than it began.

The river flows southeast in a zigzag course across the coastal plain through the Roanoke River National Wildlife Refuge and then briefly turns north as it enters Batchelor Bay on the western end Albemarle Sound.

It flows in a zigzag course along the southern edge of the Selkirk Mountains, forming the southern boundary of the Spokane Indian Reservation, where it is impounded by the Long Lake Dam to form Long Lake, a 15 mi ( 24 km ) reservoir.

It flows southwest to Wapakoneta, then generally north in a zigzag course, past Delphos, Fort Jennings and Oakwood.

The Lurio, rising in the Namuli Mountains, flows north-east, having a course of some.

It flows south, forming the state line for the remainder of its course.

It flows through Brazil for most of its course.

In the lower reaches, from Zhengzhou to the sea, a distance of, the river is confined to a levee-lined course as it flows to the northeast across the North China Plain before emptying into the Bohai Sea.

The Iskar River in its upper course flows near eastern Sofia.

A waterfall is a place where water flows over a vertical drop in the course of a stream or river.

The Ardèche river flows as far as the Rhône, following a course generally to the south east.

The river flows just north of Bald Eagle Mountain ( one of the northernmost ridges of the Ridge-and-valley Appalachians ) through much of its course in Lycoming County, but it passes the end of the mountain and turns south just before the borough of Muncy ( on the east bank ).

The main water course is the Neosho River, which flows through the western part of the county from north to south.

Eaton Rapids is on the northward course of the Grand River as it flows from Jackson to Lansing, where it turns westward, at its confluence with the Spring Brook.

No mills remain on the raceway that still flows in its original course from the Rancocas just above the dam.

The Keuka Lake Outlet flows between the lakes in the north part of the town and helped determine the course of the Crooked Lake Canal.

There is also the private golf course around which the original community was built, as well as a nature preserve through which Penny Creek flows.

The River Enters the Town Near the NE Corner of section 24 and flows in a WSWesterly course with a Gentle current except a few Riffles where the current becomes Rapid.

The River enters the Township near the center of its East Boundary and flows in a Southerly and South-Westerly course with a switft current and is from 1 too 3 feet deep in a low Stage of water and is adapted to the forming of a good motive power for mills.

The River Enters the Township Near the NW corner of section 1 and flows in a south westerly course with a swift current and has a good motive power for mills.

The River Enters the Township near the SE corner of Section 12 and flows a West SouthWesterly course, with a Rapid current and is from 2 too 4 feet deep, and is adapted to the forming of a good motive power for mills.

Below Uffington, the county border follows the old course of the river, first to the south to Tallington and then to the north, while the main course now flows along the Maxey Cut to Peakirk.

Parts of this course were later used for the River Lark, which flows in the reverse direction along the section below Prickwillow, after the main river was moved further to the west.

In the town of Brigg, the river splits into two, the ' Old River Ancholme ', which maintains its natural course through the centre of the town, and the man-made ' New River Ancholme ' which flows almost straight through some of the former industrial areas of the town.

The final of the river's course are quite straight, as the river flows through another artificial channel.

The river flows in a series of wide meanders in southerly direction for most of its course towards York.

Another tributary is the River Cocker, which joins the Derwent at Cockermouth, through which the Derwent flows after exiting Bassenthwaite Lake on its now westerly course.