Quaternary faults and ne(at)otectonic features of Nevada, Exhibit C
Let's leave the single-strand faults behind and check out some nicely sliced and diced Nevada piedmonts. First, we have spectacular piedmont of Lone Mountain near Tonopah, Nevada. Long one of my favorite places to hang out in the desert. Never a soul around. The various fault traces along the piedmont have produced / enhanced an interesting array of alluvial fans. Also, note the very nice beach cusp produced by what was once a very remote desert lake in the late Pleistocene.
Next we go back up to Dixie Valley and learn that what looks like a simple fault in a previous entry is a mere hint of how things have gone in the Pleistocene.
For the final entry, down to Fish Lake Valley at the foot of the White Mountains. Luckily, Nevada shares part of this range with California. In fact, Nevada's highest peak, Boundary Peak, straddles the state line near the northern tip of the Whites.
The flight from Reno to Vegas goes right over this fan (in addition to 100s of others). Take that flight sometime. Truly a thing to behold.
There are many more examples, but I need to move on to a different pathology before my time in Nevada runs out.