Seismic surveys are not particularly helpful in mapping normal faults because they are [[Fault trap regime|listric]] with about 100-300 ft of [[throw]] at the surface and about 30-80 ft of throw in the Niobrara. The faults are usually not present below the Niobrara. Therefore, although the Mesa Verde provides good [[seismic marker]] beds, the underlying Mancos and Niobrara | Seismic surveys are not particularly helpful in mapping normal faults because they are [[Fault trap regime|listric]] with about 100-300 ft of [[throw]] at the surface and about 30-80 ft of throw in the Niobrara. The faults are usually not present below the Niobrara. Therefore, although the Mesa Verde provides good [[seismic marker]] beds, the underlying Mancos and Niobrara |