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Fig. 1 Shallow landslides near Dayi, Guizhou Province, on June 6 , 2011
Fig. 1 Shallow landslides on the northeastern rim of Aso caldera (image courtesy of Kokusai Kogyo Co., Ltd ,Japan).
(1) Shallow depth aquifer: extends up to a depth of 20 m bgl (below ground level) and mainly consists of top soil and weathered rock.
The main findings of this study are as follows: (1) Shallow seawater samples (0 100 m) taken from the ECS in early July showed a strong correlation between δ 18Osw and salinity.
Three distinct styles of microstructure are present in the thin sections: (1) shallow, relatively high connected porosity (~ 10 21%) samples contain variable microstructure with occasional large dissolution pores and partially precipitated microcracks with altered margins (Fig. 5a, b).
Isotopic and hydrogeochemical results show that (1) shallow groundwater was associated with local precipitation in the Ayouqi and Yabulai regions, (2) lake water was mainly recharged by groundwater in the desert hinterland, (3) shallow groundwater of the desert hinterland, Yabulai Mountain and Gurinai Grassland had a common recharge source.
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They consist of (1) shallow-water carbonate platform, (2) carbonate platform slope, and (3) basin, (4) pelagic chalk, and (5) carbonate drift.
The Lake is small (3.6 × 104 m2) and shallow (4.5 maximum depth).
Divide among 4 shallow serving bowls.
Divide crab salad evenly among 4 shallow soup plates.
Lightly butter and flour a 9in (20cm) shallow plate pie dish.
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