Lawas Sandstone (2)
Another borehole was drilled about 20m away from the first borehole and it reached 23.5m before encountering bedrock.
But this bed rock is mainly fresh as compared to highly to moderately weathered generally at the first borehole. It colour is mainly grey which applies to most bedrocks not stained by the surface ground water.
Friday, 27 May 2016
Thursday, 26 May 2016
Lawas Sandstone (1)
At the Lawas town near the market, this slightly orangey brown fractured sandstone core was extracted from about 12m below ground level.
The light orange-brown colour is due to the stain apparently from reddish brown clayey silt deposited at the joints, probably due to water percolation.
Lawas is at the northern region of Sarawak, close to Sabah. It lies on a younger geological formation compared to the Western or Central Sarawak.
At the Lawas town near the market, this slightly orangey brown fractured sandstone core was extracted from about 12m below ground level.
The light orange-brown colour is due to the stain apparently from reddish brown clayey silt deposited at the joints, probably due to water percolation.
Lawas is at the northern region of Sarawak, close to Sabah. It lies on a younger geological formation compared to the Western or Central Sarawak.
Saturday, 21 May 2016
Uniaxial Compression Tests and Deformation
Measurements of A Sarawak Sedimentary Rock
We often lack of basic data to solve engineering
problems such as foundation design on local rocks. We often assume data and
properties obtained from foreign publications based on foreign rocks which
often are greatly varied from local conditions, and blindly apply in the
analysis. Perhaps, we are lucky because
we always apply large safety factors, but problems occasionally did arise,
which resulted in great disputes and costs.
This research paper attempts to obtain some basic
properties of a local sedimentary rock, Salak South Sandstone, so as to
understand the behaviour of the local rock under uniaxial loading conditions.
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