| The cause of the times | Stratum name | Feature | Thickness (m) |
| Q4ml | Miscellaneous soil | Miscellaneous colors, mainly grayish-yellow and gray; loose to slightly dense; mainly composed of construction waste, containing a large number of bricks, stones, concrete blocks, and a small amount of silty clay; the surface is partially concrete floor | 1.00∼4.10 | Plain filling soil | Grayish-yellow, grayish-brown; loose to slightly dense; mainly composed of clayey soil, see shells and screw fragments, mixed lime, and a small amount of macadam | 0.60∼2.20 |
| Q4al+l | Muddy silty clay | Gray, grayish-brown; flow plastic; soil quality is uneven, with horizontal bedding, sandwiched with silt and a thin layer of silty sand, showing thousands of layers of cake; the middle and lower part of the sand content is gradually higher, with high pressure, occasionally see shell fragments and rotten plants | 0.80∼22.40 | Silty sand (medium dense) | Gray, bluish-gray; medium dense; poor gradation; mineral composition is mainly quartz, feldspar, see mica debris, local sandwiched with a thin layer of silty clay | 1.80∼15.00 | Silty sand (dense) | Gray, bluish-gray; dense; poor gradation; mineral composition is mainly quartz, feldspar, see mica debris, local sandwiched with a thin layer of silty clay | 1.30∼17.40 | Silty clay with silty sand | Grayish brown; soft plastic; soil quality is uneven, with horizontal bedding; the thickness of the single layer is about 5 mm to 20 m, the thickness of the single layer is about 2∼5 mm silt and silty sand, and the thickness ratio is about 4 : 1 | 0.90∼3.1 |
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