Abstract:
Niyendigala landslide is a ‘skewed’ debris flow (width, 10-50 m) of more than 1.6
km in length which originated ~1260 m above MSL on 3rd May 2016 in
Paraviyangala Mountain, Belihuloya. Although landslides are most common in
mountainous areas, geology beneath is deterministic. In this report, we present the
geology of the Niyendigala landslide. Spatial analysis and mapping of the landslide
were done using Google Earth and the ArcGISTM 10.3 software. Field investigations
were carried out to confirm the spatial distribution and mapping of the landslide.
Representative rock samples were collected at seventeen locations from different
layers of the newly exposed bedrock on the slip surface. Dip and strike of foliation
and joint planes were measured using geological compass at these locations. ‘Geo
rose’ was used to plot the attitude of foliations and joints. A Fracture lineament (FL)
map of the area was prepared based on the field data and aerial photo
interpretation. Slopes along the entire landslide path vary between 7° - 33°
. Slope at
the crown is 25° - 27°
. The bedrock along the landslide consists of interbanded
quartzite, pelitic gneiss, garnet- biotite gneiss, garnet bearing charnockitic gneiss,
metagranitoid and gabbroic gneiss dipping mainly NW with a strike variable
between N75°W to N40°E. Landslide axis can vary between S25°E to S30°W. Bedrock
at the crown is weathered and highly fractured. Many joint planes are highly
inclined while some are parallel to the slip surface. It shows at least five joint sets
(090°/65°S, 45°/90° 115°/67°SW, 180°/70° E and 040°/63°SE) with joint intensities
of 3-6/m. Fracture lineaments in Panniloya catchment where the landslide occurred
are mainly oriented from NNW to NNE. The catchment shows ~5 km/km2 of FL
density while that of adjacent catchments are ~3-6 km/km2. Soil profiles along the
slide show gradual weathering or sharp contacts towards the bedrock. The slope of
the main scarp before initiation of the landslide is within the optimum angle of
repose for unconsolidated materials, 25° - 40°
. The landslide falls along a scarp slope
that consists of a folded package of inter-banded rock layers with high joint
intensity. Its axis is oblique to the strike of the foliation. Fractured and weathered
bed rock at crown helped initiation while many joint planes at the body of the
landslide contributed to the failure. However, FL density is not the highest among
adjacent catchments. Debris flow took place along a slip surface developed between
partially decomposed bedrock and overlying soil overburden at places and soil
overburden and the bedrock at other places.
