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

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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