The map below is a part of Elizondo's thesis paper.

About 500 feet of Tertiary sediments is exposed in the general vicinity of the old St. Frances Dam Reservoir, in San Francisquito Canyon, Los Angeles County, California. The area where these sediments occur is located in the easternmost part of the Ventura Basin.

At least 500 feet of well bedded red siltstones, shales, sandstones and conglomerates of continental origin is overlain by 2700 feet of piedmont deposits made up of coarse conglomerates, fanglomerates, and associated finer grained clastic rocks. No specific age can be assigned to these deposits, but to the north they are unconformably underlain by marine strata of Eocene age. These are thick bedded to massive arkoses. To the west, south and southwest the piedmont deposits are unconformably overlain by non-marine conglomerates and massive sandstones of the Upper Miocene Mint Canyon formation. The evidence prevails that the sediments in the area studied become progressively younger to the south and to the west, as happens everywhere else in the easternmost part of the Ventura Basin. Fossiliferous beds of the uppermost Miocene Modelo formation unconformably overlie the Mint Canyon beds to the south and to the west.

Pre-Cretaceous rocks composed of gray, quartz-muscovite, schist crop out in the northeasternmost part of the area. Metaquartzites and quartz veins are minor parts of this terrane. This group of rocks is known as Pelona Schists.

Pre- and post-Mint Canyon dip slip reverse faulting seems to form the dominant structural feature of the area. A possibility of normal faulting exists in the northwestern part of the area, between Eocene(?)-Miocene(?) rocks and the Mint Canyon formation, and is fully considered in the text.

The sedimentary formations are folded, and the axes follow a northwest-southeast direction in the northern part of the area, and are probalby related to a first stage deformation in pre-Mint Canyon times; to the south, the fold axes trend north-south, and seem to be related to a second stage of deformation that probably took place in post-late Miocene time.

The area is in its late youth to early mature state of topographic development. The stream along San Francisquito Canyon cuts across the structure of the Pelona schists indiscriminately for at least one mile, reflecting inheritance of a drainage system established under different conditions. Cavernous weathering is largely confined to many beds of hard, massive, conglomeratic sandstone of Eocene(?)-Miocene(?) age, in the north central part of the area.