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Using Vertical Electrical Sounding for Locating Static
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Using Vertical Electrical Sounding for Locating Static
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Surface layer.
VES
38: Vertical electrical sounding (
VES
). Middle layer. Ground surface. Scale H: 1:50000. V: 1:2000. 11091. 52. 192. 90. 57. 90. 231. 904.
Research Journal of
Environmental Sciences ISSN 1819-3412
www.academicjournals.com
146000
148000
150000
152000
154000
156000
158000
160000
896000
896000
894000
894000
892000
892000
890000
890000
888000
888000
886000
886000
884000
884000
882000
882000
880000
880000
Legend Scale: 1:150,000 Alluvium
Basemen complex
0
1500
3000
4500 m
)U MN 1 AB
MN
I 2
AB
MN
3
4
A3
M3
A2
M2
A1
M1
N1
B1
N2
B2 N3
B3
(a) 75
VES38
140.743 50 90
Elevation (m)
25 0
192
Aquaba area Geolectrical cross section 1 VES39
VES37
904 57 90 231
VES40
581.16.1240
1693.129.870
46
46
VES42 120.79.319
77 52
11091
306
233
29595
91
112
-25 -50 -75 1984 -100 -125
Scale Surface layer Middle layer
H: 1:50000 V: 1:2000
VES 38: Vertical electrical sounding (VES) Ground surface
8
23
(b) 100 VES50 75 50140.743 90 25
85
1527.119 657 109 110
32
25
1262
336
2642.41 325
VES38
VES49
192
0 Elevation (m)
-25
52
-50 -75 -100 -125
Fault
Scale
Surface layer Middle layer Lower layer Deep layer
H: 1:50000 V: 1:2000
Legend VES 49: Vertical electric sounding (VES) Ground surface 192: Resistivity value (ohm-m)
1.25 (c) VES51 100 1314.176 419
VES49
75
1527.116 657 109
30 50
110
Elevation (m)
25 9229 0
-25
-50
26
Legend VES 49: Vertical electric sounding (VES) Ground surface 192: Resistivity vale (ohm-m)
-75 Fault Scale -100
-125
Surface layer Middle layer Lower layer Deep layer
H: 1:50000 V: 1:2000
334
0.0 Gravel and sand 3.5 m
Sand and sandy clay
30.0 m
Sandstone
38.0 m Gravel and sand 42.5 m
Sandstone
51.0 m Unknown
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