印尼即坐落在极不稳定的“火山带”上。这条火山带呈弧形，围绕着太平洋周边地区，充满了地质不稳定。
Indonesia sits on the volatile "Ring of Fire," an arc of seismic instability around the Pacific rim.
古特伯赖特说，在铺设电缆的过程中，除了避免太平洋洋底的地质不稳定的地点之外，人们不可能预测地震会造成什么问题。
Gutberlet says, aside from avoiding seismically unstable spots on the ocean floor, it is impossible to forecast such problems.
散布于野外的地热区也反映了冰岛地质的不稳定性。
Iceland's geologic restlessness is also reflected in the geothermal areas that dot the countryside, such as these bubbling mud POTS.
金沙江流域的地质结构并不稳定，汶川大地震后，国家要求对水电站进行抗震覆核。
Geological structure of the Jinsha River basin is not stable, Wenchuan after the earthquake, the state requirements for seismic review of the hydropower station.
本文提出的评价方法在类似矿山不稳定边坡地质灾害危险性评估中具有参考和借鉴价值。
The evaluation method can be used for reference in the assessment of geological hazards in similar cases.
利用极限平衡法对边坡整体深层破坏模式进行分析，对岩体局部不稳定块体，利用常用的地质分析方法赤平投影法简要进行分析；
Based on limit equilibrium method and stereographic projection method, the stability of the deep layer slide and the superficial layer slide can be analyzed.
根据计算的单元格地质灾害发生概率值，将龙胜县地质灾害危险性划分为4个等级，即极不稳定、不稳定、基本稳定和稳定。
Based on the calculated cell goe-hazards probability of occurrence, the goe-hazards risk in Longsheng County is divided into 4 grades, namely extremely unstable, unstable, basically stable and stable.
康定县地质灾害类型众多，主要有滑坡、泥石流、不稳定斜坡(崩塌危岩体及滑坡变形体)等。
Landslide, debris flow, unstable slope (rockfall and landslide plasmodium) are the main types of geological hazards in Kangding county.
从自然的角度来讲，区域地质地貌、气候和水文等的异常变化是生态系统不稳定性和退化的自然成因。
The natural inducing factors refer the exceptional changes of regional geology and terrain, climate and hydrology situation;
与此同时，在距离震中较近的地区，由于长江在四川盆地形成了厚厚的沉积层，地质结构不稳定，震动更为严重。
Meanwhile, shaking closer to the epicenter was made worse by a thick layer of sediment deposited in the Sichuan Basin by the Yangtze River, which makes the ground there unstable.
但该区处于新构造运动强烈、地质环境极不稳定的高山峡谷区，为强烈地震和地质灾害高发区。
This area is a new strong tectonic movement and highly volatile geological environment mountain valley areas, which has a high incidence of strong earthquakes and geological hazards.
但该区处于新构造运动强烈、地质环境极不稳定的高山峡谷区，为强烈地震和地质灾害高发区。
This area is a new strong tectonic movement and highly volatile geological environment mountain valley areas, which has a high incidence of strong earthquakes and geological hazards.
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