The investigation of toppling slope failures in welded ash flow tuff at Glennies Creek Dam, New South Wales
The investigation of toppling slope failures in welded ash flow tuff at Glennies Creek Dam, New South Wales
The Quarterly Journal of Engineering Geology (1988) 21 (4): 289-298
- Australasia
- Australia
- boreholes
- Carboniferous
- dams
- excavations
- failures
- fractures
- friction angles
- geologic hazards
- igneous rocks
- joints
- mass movements
- mechanical properties
- New South Wales Australia
- Paleozoic
- pyroclastics
- rock masses
- rock mechanics
- rockfalls
- rockfill dams
- shear strength
- site exploration
- slope stability
- style
- volcanic rocks
- welded tuff
- Singleton Australia
- Glennies Creek Dam
The Glennies Creek Dam spillway was designed as an unlined rock cutting in welded tuff 700 m long with a bedwidth of 37 m, a maximum cut height of 40 m and right-and left-hand side slopes of 3 in 1 and 2 in 1, respectively. Toppling failures in the 3 in 1 right-hand spillway batter occurred during construction. In order to maintain rockfill production, that part of the right-hand batter affected by the failures was battered back from 3 in 1 to a slope of 1 in 1; involving 33 000 m (super 3) of additional excavation. Geological investigations concluded that toppling became possible due to the removal of the column toe support due to plane sliding movements on joints dipping towards the cut at 24 degrees . These sliding movements were caused by immediately adjacent heavy quarry blasting which reduced the available joint friction angle from the peak value of 38 degrees to the residual value of 25 degrees . An essential step in the analysis of slope stability is the identification of slopes susceptible to toppling. The application of standard methods of toppling analysis to slopes which are not susceptible to toppling even though it may be kinematically possible will result in unnecessarily conservative slope designs.