Fig 2 - uploaded by Rohayu Che Omar
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Geological map of the site area
Source publication
This study presents the results of discontinuity mapping using terrestrial laser scanning (TLS) survey and the kinematic method. The results provide the current site and slope condition of comprehensive geological study using terrestrial laser scanning and discontinuity survey at Simpang Pulai, Perak. From the results obtained, it can be concluded...
Contexts in source publication
Context 1
... shown in Figure 1. The geology map in Figure 2 indicates the Kinta Limestone. This area has the existence of massive limestone bodies that are heavily jointed and fractured. ...
Context 2
... are seven (7) sets of major discontinuities with slope face (022 o /77 o ) at Area 6 as shown in Fig. 12. The results came from 141 readings of discontinuity survey along this area as stated in Fig. 13. Kinematic analysis for Area 5 is shown in Fig. 13. Based on the figure, three types of potential failures were identified in this area which is plane, wedge and toppling ...
Context 3
... shown in Figure 1. The geology map in Figure 2 indicates the Kinta Limestone. This area has the existence of massive limestone bodies that are heavily jointed and fractured. ...
Context 4
... are seven (7) sets of major discontinuities with slope face (022 o /77 o ) at Area 6 as shown in Fig. 12. The results came from 141 readings of discontinuity survey along this area as stated in Fig. 13. Kinematic analysis for Area 5 is shown in Fig. 13. Based on the figure, three types of potential failures were identified in this area which is plane, wedge and toppling ...
