West Little Owyhee River
West Little Owyhee River is a tributary of the Owyhee River in the U.S. state of Oregon.
The source of the river is at an elevation of near McDermitt, while the mouth is at an elevation of in the Owyhee Desert.
West Little Owyhee River has a watershed.
The river begins east of McDermitt and flows east by Deer Flat and into Louse Canyon.
Near Twin Buttes, it turns sharply north, still in Louse Canyon, which it follows through the Owyhee Desert all the way to the Owyhee River in Owyhee Canyon.
The entire river is protected as part of the National Wild and Scenic Rivers System.
Overseen by the Bureau of Land Management, the river offers fishing for smallmouth bass and trout, and the canyon area is scenic.
Dispersed camping is allowed, although the watershed has no developed parks or campsites.
Other forms of recreation include hiking, backpacking, hunting, picnicking, and biking.
Named tributaries from source to mouth are Lake Fork West Owyhee River, Jack Creek, Little Spring Creek, and Toppin Creek, which all enter from the right.
Further downstream, Cave Creek enters from the left.
Lower Lake Fork Valley, Colorado
The Lake Fork of the Gunnison River begins in high mountains in the western region of the U.S. state of Colorado, draining the northeastern part of the San Juan Mountains.
After passing through Lake San Cristobal, one of the larger natural lakes of Colorado, it is joined at Lake City by Henson Creek, and from there flows north.
About 22 miles( 35 km) north of Lake City, it enters the Lake Fork Canyon, and at the north end of the canyon, joins the Gunnison River just before it enters the Gunnison River canyon.
For the purposes of this discussion, we will consider the lower Lake Fork Valley to be that part of the river between Lake City and the canyon.
The area is not unlike many other areas in the west.
Early on, it was Ute Indian land and when white men began moving into the area, using places and resources of the Utes, there were conflicts.
The discovery of gold in Colorado brought numbers of prospectors into the mountains.
To deal with these problems, a treaty was signed in 1868, giving much of western Colorado to the Utes.
However, gold continued to attract prospectors to the area and troubles continued.
To deal with it, a group of Ute leaders were taken to Washington, D.C. in 1873, and under protest, they signed the Brunot treaty which opened a large portion of the San Juan Mountains to prospectors and mining.
Otto Mears, a man responsible for many of the railroads and roads in Colorado, hired Enos Hotchkiss to build a road into the Lake City area, from which it was to continue on to the west.
Hotchkiss found gold near present Lake City in 1875, and the town was started.
Thus began the era when minerals and mining defined much of the character of the Lake Fork area.
Even at these early times, though, there were people who saw the beauty of the mountains and realized that the area had great resources for raising cattle, and so ranches, although secondary to mining, began.
With more and more people in the area, there was need for mail and other services and the stagecoach became important.
One of these stagecoach routes began at Sapinero, the small town at the intersection of the Lake Fork and the Gunnison Rivers.
The route went up over Sapinero Mesa on the east side of the Lake Fork Canyon.
A small stream called Johnson Gulch( after an early squatter who built a cabin there) runs from the east to the Lake Fork river, just above the canyon.
The stage road dropped into Johnson Gulch and then down into the valley of the Lake Fork.
From there it went 2 miles( 3 km) to the south where a stage station and large barn were built at what was later called Barnum Station.
From there, it continued up the Lake Fork valley to Lake City.
Only small amounts of minerals were able to be taken from the Lake City area in wagons and so pressure for a railroad developed.
In 1881, the Denver and Rio Grande( D&RG) built a rail line into Gunnison and then continued to the west to Sapinero.
Although a branch had been planned for Lake City, the lack of money delayed it.
Finally, in 1879, it was completed.
This was the end of the stagecoach in this area.
The rail line came up the Lake Fork Canyon and at Johnson Gulch, a water tank was built to provide water for the steam engines.
This was called Madera Siding.
The rail line continued to the area below Barnum Station where holding corrals were built, and this was an important loading place for cattle which were then shipped to Sapinero and from there on east across Marshall Pass.
The major use of the rail line, however, was to carry increasing mineral wealth from the Lake City area.
Ranchers along the valley were also dependent on the train to bring mail and needed supplies.
As with so many other mining areas, the mines of Lake City began producing less and less.
Finally in 1933, the rail line was making little money and was abandoned by the D&RG.
The line was purchased and called the San Cristobal Railroad, and a galloping goose was built to run on the tracks and to take mail and other things to and from Lake City.
The galloping goose was a combination between a car and a railway car, built on a Pierce- Arrow body.
It used a gasoline engine and could be driven up the railroad tracks and carry mail and limited amounts of freight.
This was never very successful, though, and the rail line was completely abandoned in 1939.
By this time, there were automobile roads into the area, and mail was brought into the valley from Gunnison in this way.
Rainwater Creek
Rainwater Creek is a tributary stream of Lake Fork Creek.
It flows into Lake Fork Creek downstream from the Lake Fork Reservoir Dam approximately four miles west of Quitman in western Wood County, Texas.
Its primary source is a spring, augmented by stormwater runoff.
It is named for the family of William Walton Rainwater, who was among the earliest permanent settlers of the area.
Stuart River (Minnesota)
The Stuart River is a river located in Minnesota, in the United States.
Dee River (Queensland)
The Dee River is a river located in Central Queensland, Australia.
Lake Fork Gunnison River
Lake Fork Gunnison River or Lake Fork is a tributary of the Gunnison River in Colorado.
The river's source is Sloan Lake near Handies Peak in the San Juan Mountains of Hinsdale County.
Lake Fork flows through Lake San Cristobal and Lake City before a confluence with the Gunnison River in Blue Mesa Reservoir.
Lake Fork West Owyhee River
The Lake Fork West Owyhee River is a short tributary of the West Little Owyhee River in the U.S. state of Oregon.
The river begins near Cat, Bend, and Pedroli springs near the eastern boundary of the Fort McDermitt Indian Reservation in southern Malheur County.
It flows generally northeast to meet the larger river in Louse Canyon.
The Lake Fork has no named tributaries.
Don River (North Queensland)
The Don River is a river located in North Queensland, Australia.
Maskerchugg River
The Maskerchugg River is a river in the U.S. state of Rhode Island.
It flows approximately 6 km( 4 mi).
There are four dams along the river's length.
Lake Fork Creek
Lake Fork Creek is a river in Hunt, Rains, and Wood counties in Texas.
It is a major tributary of the Sabine River, and has as its major tributaries Dry Creek, Glade Creek, Caney Creek, Little Caney Creek, Rainwater Creek, and Birch Creek.
In 1980, Lake Fork Creek was impounded, resulting in the formation of Lake Fork Reservoir.

Question: Are both rivers, Maskerchugg River and Lake Fork West Owyhee River, located in the same country?
Answer: yes