J. C. Dohrenwend 1982 <p>Patterns of Late Cenozoic Faulting</p> <p>The Walker Lake 1^o x 2^o quadrangle lies athwart the transitional boundary between the Sierra Nevade and Basin and Range physiographic provinces. Six distinct topographic domains are identified with the quadrangle (fig. 1). Theses domains are clearly defined by contrasting orientations, densities, and styles of lake Neogene faulting as follows:</p> application/pdf 10.3133/mf1382D en U.S. Geological Survey Map showing late Cenozoic faults in the Walker Lake 1 degree by 2 degrees Quadrangle, Nevada-California reports