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The soil-mantled sinkhole is generally shallower than the collapsed sinkhole and receives local drainage; it may become clogged with clay and hold a small lake.
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The East China Sea, with an area of 290,000 square miles (751,100 square km), is generally shallow, having an average depth of only 1,145 feet (349 m).
It is generally shallow, with depths of 165 to 260 feet (50 to 80 metres), deepening at its western edge, where coral reefs have grown at depths of nearly 2,000 feet (610 metres).
From 4.5 to 213 miles (7 to 342 km) in width and 393 miles (632 km) long, it is generally shallow with depths less than 700 feet (210 m).
The separating syncline of the anticline lines is generally shallow and continuous.
Given the depth of groundwater is generally shallow in the model area, the evapotranspiration (ET) is considered significant.
The quartzites and the basal part of the massive limestone are good aquifers, and the permanent water table in these is generally shallow.
The results show that the preferred conformation of α-maltose in vacuo depends strongly upon the hydroxyl group orientations ('c'/'r'), but the energy landscape moving away from the minimum-energy position is generally shallow and transitions between conformational positions can occur without the addition of significant energy.
In the north, the shelf is generally shallow and as narrow as 20 km, with ribbon-reefs at the shelf edge forming a nearly continuous barrier.
Fibrous root systems are generally shallower than taproot systems.
The focal depths of relocated hypocenters determined using OBS data are generally shallower than those determined by JMA in the study area.
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