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To examine the possibility of the deeper or shallower extent of the source areas in Nankai Trough earthquakes, we compared tsunami heights predicted in the scenario with Mw = 9.03 to real damage caused by the 1707 Hoei earthquake event, i.e., we evaluated the degree to which the newly proposed Mw9-class Nankai Trough earthquake scenario was consistent with reality.
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Generally, due to the shallow extent of rock weathering, aquifers are unconfined and occur at shallower depths compared to those within other bedrock terrains.
As mentioned above, there is the possibility that the source area of Nankai Trough earthquakes extends to deeper or shallower extent.
A low-(Q_{text{P}}) and low-(Q_{text{S}}) zone also exists beneath the Kuju and Aso volcanoes, which is consistent with the shallow limited depth extent of the seismogenic zone due to high temperature.
At the end of the Triassic, increased tectonic activity contributed to rising sea levels and an increase in the extent of shallow continental shelf seas.
This study intended to assess the extent of shallow dug wells (SDWs) utilization and contribution of IK on management of SAs of indigenous people of Dodoma Municipality.
The Lake of Tanis and the Pelusiac branch had a long extent in the East-West direction (>25 km); during wind setdown this extent of shallow water can produce a vertical displacement of 2 m.
It is considered that SSEs occur along the same interface as ordinary tectonic earthquakes (Ide et al. 2007b), generally at the deeper extent of the shallow locked region, below the brittle ductile transition.
In the study area, we mapped more than 147 shallow soil slides for a total extent of about 0.14 km.
The simulated RDX and TNT contaminant plumes, shown in Figure 2, represent the extent of contamination in the shallow aquifer at the end of 2002.
The area of study is situated within the offshore depobelts of the Niger Delta in southern Nigeria (Fig. 1), covering an area extent of 102 km2 within the shallow marine environment of the continental shelf.
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