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The preferred 3D resistivity models show that a moderately resistive structure (30 200 Ω m) is characteristic of most of the volcano, and were able to delineate a hydrothermal zone within the volcanic edifice.
At an elevation of 2000 m, the entire area is dominated by a uniform moderately resistive structure (40 200 Ω m) with embedded high-resistivity blocks (>800 Ω m).
The homogeneous half-space is a simple 1D moderately resistive model.
At the high elevation of 2700 m, a moderately resistive structure (50 320 Ω m) dominates the whole area.
The lower crust is characterized by a conductive (1 –30 ohm-m), to a moderately resistive (50 200 ohm-m), nature.
At an elevation of 2300 m, a highly conductive uniform layer (<25 Ω m) dominates the east model area whereas a moderately resistive structure (40 200 Ω m) dominates the northwest model area.
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moderately resistant.
2D DC results indicated a highly heterogeneous and moderately conductive waste rock underlain by a resistive bedrock containing numerous fractures.
The boundary between the anomalously thick, resistive sub-Piedmont lithosphere and the relatively thin, moderately conductive sub-Appalachian lithosphere corresponds within resolution to the modern Appalachian topographic escarpment.
The moderately shallow depth to basement and outcrops observed in the 2-D magnetic model and the orange/green/blue coloured band indicating high resistive substratum, especially the blue coloured band at the surface indicating outcrops observed in the 2-D resistivity structure, correlate with high resistive substratum (lateritic layer) in the geoelectric section.
"Moderately prosperous.
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