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These deposits appear to extend to a depth of 60 feet below the present sediment surface, but the quality of the deposits below 30 feet is unknown.
In many cases, however, the obtained VS profile does not extend to a depth of 30 m due to unfavorable field conditions and limitations of testing techniques.
Two-dimensional (2D) inversion of MT data and gravity models indicate the Wadi Kubbaniya is filled with loosely-consolidated sandstone and conglomerate that extend to a depth of ∼150 200 m into Cretaceous sandstone formations which overlie Precambrian crystalline rocks.
Our results show that low-velocity anomalies extend to a depth from 10 to 35 km (Fig. 9 (Y = 0km)).
In Bangladesh, the 5 boreholes are only ~125 m apart and extend to a depth of ~20 m.
The sedimentary cover ends with the Buntsandstein sandstones that extend to a depth of 1,405 m.
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It extends to a depth of about 60 mi (100 km).
The amorphized zone in B4C extends to a depth of almost seven times the indentation depth.
The low-velocity layer begins about 50 to 150 km (30 to 90 miles) below the surface and extends to a depth of roughly 300 km (180 miles).
Beneath this, a uniform hardened layer was formed, extending to a depth of approximately 200 μm below the surface.
This layer, named for the Swedish oceanographer V. Walfrid Ekman, extends to a depth of about 100 metres (about 300 feet).
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