The Honey Lake Fault Zone is a right lateral-moving (dextral) geologic fault extending through northwestern Nevada and northeastern California.
It is considered an integral part of the Walker Lane.
A 50 km (31 mi) zone of disturbed landforms reveals the fault's presence on the surface.
The geological evidence shows at least four surface-faulting earthquakes have occurred in the late Holocene era.
This article about a specific United States geological feature is a stub.