The larger and more angular fragments would not have traveled as far as some of the busted up smaller more rounded ones. These counts were done at Montezuma Pass, Huachuca Mtns., and roadcut at Bisbee Roundabout. Along with these counts, two sections of ground were measured for bedding sequences, fossils, and thickness. One at the Huachuca Mtns. Section two was done at a roadcut through the Mule Mtns extending from the Morita Formation to the Mural Limestone.
Strike is a direction taken by a bedding plane as it intersects the horizontal.
The dip is the angle that any planar feature makes with the horizontal, measured perpendicular to the strike. This is the northwestern end of the Bisbee Basin, and the following stations will be going in the general direction of the Southeast. There was lots of sandstone and some limestone, shale, bedded chert, and stromatolites. Although there were a lot of individual fossils the variety was at a minimal. Ooids and other coated grains were found, as well as cross-stratification showing an inconsistent flow direction.