Research Article

Effectiveness of Geoelectrical Resistivity Surveys for the Detection of a Debris Flow Causative Water Conducting Zone at KM 9, Gap-Fraser’s Hill Road (FT 148), Fraser’s Hill, Pahang, Malaysia

Table 3

Attribute of various zones based on resistivity values.

NumberZoning symbolDescription

1aResistivity values above 5000 Ωm, are the fresh granite rock mass
2bResistivity value between 3000 Ωm–5000 Ωm, granite slightly weathering and highly fractured
3cResidual soil (IAEG, V-IV) (600 Ωm–3,000 Ωm)
4dWater conducting zone or high water content (<600 Ωm)