Results have indicated that major sliding surfaces are happened to pass through colluvium and sandstone. 而所评估之潜在滑动面则多通过五弯仔地区之崩积层与砂岩层。
Muddy siltstone formation of the whole residual weathered colluvium to residual main causes. 泥质粉砂岩全风化形成的残坡积土，以残积成因为主。
This study measures suction in the laboratory of four colluvium soils taken from middle and northern parts of Taiwan. 本研究针对台湾地区中、北部四个地区之崩积土壤进行室内之吸力量测试验。
With some reasonable assumptions, we can reproduce the region and characteristics of colluvium in Hungtsaiping area before Chichi earthquake. 亦可由于边界施加集集地震之地表加速度进行边坡受震模拟，使其产生之地表位移场与前人利用震前后航照分析相符合之结果。
Chen, H. and Lo, C. Y. (1993) The Sensitivity of the Huanku Colluvium and its Relevant Physical Properties, Jl. Geol. Soc. China, Vol.36, No.4, Pp.481-497. 陈宏宇;许景富（1992）宜兰地区瓷土矿之工程特性及其相关之坡体稳定性分析;中国矿冶工程学会会刊;第36卷;第4期;第9-17页.
