aayjaber
Structural
- Feb 16, 2008
- 47
I am developing a property where part is sloping up by 40% with rock outcroppings showing; the rest is flat and is a small part of the property, on the surface it is a mixture of dark soil and stones of all sizes. On the published California maps of liquefaction hazard the flat area is labeled as liquefaction risk.
I dug a couple of trenches in the area and in both I encountered very dense soil mixed with stones, the soil is dark kind. As I reached the 2 ft depth it was very hard to dug much even by the sharp ax pick I am using. As I went deeper the stones started to get bigger and bigger. The stones I am digging out of the trench as of many sizes. Overnight I thought may be I should fill the trench with water to help me go deeper, when I went to work in the morning I found almost all the water I poured in the trench sitting there nice and clear.
What can be read from the observation? Is the liquefaction hazard just speculative and the real data will confirm or reject the hazard assumption?
I dug a couple of trenches in the area and in both I encountered very dense soil mixed with stones, the soil is dark kind. As I reached the 2 ft depth it was very hard to dug much even by the sharp ax pick I am using. As I went deeper the stones started to get bigger and bigger. The stones I am digging out of the trench as of many sizes. Overnight I thought may be I should fill the trench with water to help me go deeper, when I went to work in the morning I found almost all the water I poured in the trench sitting there nice and clear.
What can be read from the observation? Is the liquefaction hazard just speculative and the real data will confirm or reject the hazard assumption?