1. INTRODUCTION STRF: 50m reflection line with dx=1.0m
STRL: 150m reflection line with dx=3.0m

2. DATA ACQUISITION
50m long reflection line, with 48 geophone groups spaced with dx=1.0m.
10, 15lb sledgehammer hits were stacked at every other source point.
Relative to the 150m line, line extends from x=60m to x=110m.
150m long reflection line. 48 geophone groups are evenly space with dx=3.0m.
There are six geophones per group.
10, 15lb sledgehammer hits were stacked at each channel.

3. PROCESSING Constant NMO velocity of 1200 m/s.
Only one strong reflector observed in the constant velocity stacks.
Stolt Migration is a form of time migration, which relocates seismic events to their true subsurface locations.
Migration techniques allow for more accurate images of subsurface geology.

4. CONCLUSIONS
Reflection and refraction data indicates 30-60m wide fault zone.
Reflection images show a normal fault dipping at approximately 75o E.
Many diffractions observed in the 1m line, showing the broken and fractured fault zone.
Depth to bedrock is approximately 40m.