Maybe between 20 an 50 ft OLDER ALLUVIUM (Holocene) Unconsolidated deposits consisting of locally derived clay-, silt-, sand-, and rarely gravel-sized sedimentary material; represent slightly older terrace deposits than those formed in modern flood plains; predominantly found adjacent to, and 5-10 ft. above, modern alluvial deposits of major drainage systems. Areas rarely subject to flooding. Thickness: unknown, possibly as much as 50 ft (15 meters). REMNANTS OF OLDER ALLUVIUM (Holocene and/or Pleistocene?) Unconsolidated deposits consisting of locally derived clay-, silt-, sand-, and rarely gravel-sized sedimentary material; found as small, isolated remnants about 5-10 ft. above Qao deposits. Areas probably never subject to flooding. Thickness: unknown, possibly as much as 20 ft (6 meters).
Very cool that you showed your boys moving dirt when they were little.🤗
How far down is rock?
Maybe between 20 an 50 ft
OLDER ALLUVIUM (Holocene) Unconsolidated deposits consisting of locally derived clay-, silt-,
sand-, and rarely gravel-sized sedimentary material; represent slightly older terrace deposits than
those formed in modern flood plains; predominantly found adjacent to, and 5-10 ft. above, modern
alluvial deposits of major drainage systems. Areas rarely subject to flooding. Thickness: unknown,
possibly as much as 50 ft (15 meters).
REMNANTS OF OLDER ALLUVIUM (Holocene and/or Pleistocene?) Unconsolidated deposits
consisting of locally derived clay-, silt-, sand-, and rarely gravel-sized sedimentary material; found as
small, isolated remnants about 5-10 ft. above Qao deposits. Areas probably never subject to flooding.
Thickness: unknown, possibly as much as 20 ft (6 meters).
@@TonyGaeddert towards the end of the video it seemed like the bulldozer was driving on bed rock when it was in the water?