[timeout:300][out:json];
(
node(around:1000,40.22500,-109.54200)[landuse=basin][name];
way(around:1000,40.22500,-109.54200)[landuse=basin][name];
rel(around:1000,40.22500,-109.54200)[landuse=basin][name];
);
out center tags;
The Uinta Basin (also known as the Uintah Basin) is a physiographic section of the larger Colorado Plateaus province, which in turn is part of the larger Intermontane Plateaus physiographic division. It is also a geologic structural basin in eastern Utah, east of the Wasatch Mountains and south of the Uinta Mountains. The Uinta Basin is fed by creeks and rivers flowing south from the Uinta Mountains. Many of the principal rivers (Strawberry River, Currant Creek, Rock Creek, Lake Fork River, and Uintah River) flow into the Duchesne River which feeds the Green River—a tributary of the Colorado River. The Uinta Mountains form the northern border of the Uinta Basin. They contain the highest point in Utah, Kings Peak, with a summit 13,528 feet (4,123 metres) above sea level. The climate of the Uinta Basin is semi-arid, with occasionally severe winter cold.
no matches found
| basin (Q813672) | landuse=basin |
| Sedimentary basins of North America | landuse=basin |
| Structural basins of the United States | landuse=basin |