Lonesome Valley is an approximately north-northwest trending valley. It is dissected in its center by an upside-down
V-shaped, double watercourse.
Granite Creek–(Granite Creek Wash) is west, and an unnamed wash is east-(a tributary to Granite Wash); both flow north to meet the Verde River, at the north of Little Black Mesa. The unnamed wash at Lonesome Valley's south end flows south from the
water divide, north of Prescott Valley, to meet the
Agua Fria River. Coyote Wash courses southwesterly just east, (see satellite photo). Lonesome Valley appears somewhat circular, but the Chino Valley townsite is on a flatland region at the northwest. Alluvial fans lie at the east with the west flank of the Black Hills. The
Granite Mountain (Arizona) region at the west-southwest, has a large dissected alluvial section at its northeast. The southwest perimeter of Lonesome Valley borders the north of
Granite Dells, where Granite Creek exits flowing north.
Watson Lake is at the south of the Dells, where Granite Creek enters. The highpoint of the valley is Black Hill, ), on the east bank of Granite Creek, and at valley center-southwest. (on satellite photo: black, at southeast of Chino Valley, northeast of the green,
Antelope Hills Golf Course-(note also black shadows; sun, from southeast))
Southwest valley region The southwest of the valley is bordered by the north of
Granite Dells. Attached at the east of the Dells is
Glassford Hill, at ). The prominent hill forms the west perimeter of the Prescott Valley townsite. Granite Creek flows north (slightly north-northeast) from the west, and the 'unnamed wash' flows northwest at the hill's east. ==Access==