The White River fault is a subsurface split in the region’s bedrock that runs west-east across northern Fayetteville and southern Springdale.
No seismic activity has been experienced on the White River fault in recorded history.
The White River fault is a subsurface split in the region’s bedrock that runs west-east across northern Fayetteville and southern Springdale.
No seismic activity has been experienced on the White River fault in recorded history.