From its origin in the Canelo Hills of
Santa Cruz County at , Ciénega Creek flows northwesterly through the upper Ciénega basin, a wide
alluvial valley separating the northern
Santa Rita and Empire Mountains to the west and the
Whetstone Mountains to the east. A bedrock high, called "the Narrows," serves as a hydrologic barrier dividing the upper and lower basins, and is characterized by riparian vegetation and perennial flow. Ciénega Creek continues northward through the lower alluvial basin until it bends west/northwest in the vicinity of Anderson and Wakefield Canyons. After crossing
Interstate 10 near the town of
Vail, Ciénega Creek again crosses a bedrock high, and once more the flow becomes perennial. In these stretches, groundwater is forced upward through faults in the bedrock from aquifers near the surface. Just north of Vail, Ciénega Creek becomes known as Pantano Wash, which continues northwest through Tucson and links up with the Rillito River. ==Flora and fauna==