代写演讲稿：地质构造板块

代写演讲稿：地质构造板块

其他可能的因素包括旋转横向距离，分离下加利福尼亚和变形范围和盆地。北部部分穿过霍利斯特向北移动，经过国家海岸的雷斯岬，最终向近海移动(Brenguier et al. 1480)。南段一直延伸到萨尔顿海从公园田向南移动。爬行的中央部分包含了从霍利斯特到公园的一切。众所周知，这个断层有一个明显的大拐弯，推动着南加州一些最壮观的山脉。这种混合导致了地质构造板块之间的拉伸和挤压。

代写演讲稿：地质构造板块
地壳上的压力是通过挤压来减轻的，挤压会形成山脉，而在更远的地方地壳会断裂或断裂，就像洛杉矶(纳多和杜伦克390)的断层一样。通过大量的调查和从深钻项目中获得的证据，湿滑的粘土可能是圣安德烈亚斯断层爬行的一个因素。发现了一些类滑石矿物，与南北向断裂相比，它们的摩擦较少。因此，最脆弱的部分是最容易爬升的中间部分。

代写演讲稿：地质构造板块

Other possible factors include rotating Transverse Range, separating Baja California and deforming the Range and Basin. The northern segment is running across Hollister moving north by the National Seashore of Point Reyes, while moving offshore eventually (Brenguier et al. 1480). The southern segment has been stretching across the Salton Sea from Park field moving south. The creeping central section is inclusive of everything from Hollister to Park field. The fault is known for having a visible Big Bend pushing some of the most spectacular mountain ranges of southern California. This blend results in the creation of geologic stretching and squeezing between both the tectonic plates.

代写演讲稿：地质构造板块
The stress places on the crust of Earth are relieved by squeezing that builds mountains and further ahead breaks or faults the crust of Earth like the faults slicing up the area of Los Angeles (Nadeau and Dolenc 390). On massive investigation and the evidences obtained from project of deep drilling, slippery clays can be one element responsible for some of the behaviour of creeping in alignment with the San Andreas Fault. Some talc-like minerals have been found that are known to have less friction in comparison with the fault of southern and norther segment. Therefore, the most vulnerable segment is the central one with maximum chances of creeping up.