论文代写:意大利翁布里亚
意大利翁布里亚地区是意大利20个地区之一。它位于意大利中部。这是意大利唯一与其他国家拥有海岸线的地区。它有特拉西梅诺湖,马尔莫尔瀑布,它横跨台伯河。该地区以其风景和遗产而闻名。该地区有山,山,谷和历史发展。这座城市西接托斯卡纳,南接拉齐奥,东接马尔托罗。可以暗示,这个城市部分是丘陵和山区。它部分平坦而肥沃,基于台伯河谷。翁布里亚有两个山谷。这是翁布里亚山谷和台伯河谷。第一个来自Cittàdi Castello,他们与拉齐奥接壤。台伯河有三条流向翁布里亚的主要支流。 Chiasco盆地可以被认为是相对无人居住的巴斯蒂亚温布拉。据称,该地区东部有许多断层,经常遭受地震袭击。最后一个是1997年,而2016年的则是在诺尔恰和瓦尔内利亚之间进行的。滑坡危害可能由各种可能的裂缝,山脊和陡坡造成,并解释切割和填充失败。
论文代写:意大利翁布里亚
土地和土地解剖的分析有助于对区域内可能发生的滑坡问题进行预测性分析。下面描述了最常见的山体滑坡。最常见的山体滑坡之一就是滑梯。这些可以是平移幻灯片或旋转幻灯片。在某些情况下,它可能是泥石流。这是一种快速的质量运动形式,其基于地表水流的强度或由于较重的降水而发生。这些是造成这些山体滑坡的因素(Guzzetti et al。,2005)。山体滑坡是基于地震活动而发生的。它表明地震或其他可能存在的危险地区的可能性。绘制的地图表示基于土地物理地形方面的可能的滑坡区域的类型。这些有许多特征会导致特定的事件发生并导致该地区的土地的创建。这些在下一节中进行了探讨。
论文代写:意大利翁布里亚
The Umbria area in Italy is one of the 20 regions of Italy. It is located in the central Italy. It is the only region in Italy that has a coastline with other nations. It has the Lake Trasimeno, Marmore Falls and it is crossed by the River Tiber. The region is known for its landscapes and legacy. The region has hills, mountains, valleys and historical development. The city is bordered by Tuscany in the west, Lazio to the south, Marcho in the east. It can be alluded that the city is partly hilly and mountainous. It is partly flat and fertile that is based on the valley of Tiber. Umbria has two valleys. It is the Umbrian valley and the Tiber Valley. The first one is from the Città di Castello and they border with the Lazio. The Tiber has three principle tributaries that flow towards the Umbria. The Chiasco basin can be considered to be relatively uninhabited as far as the Bastia Umbra. It has been stated that the eastern part of the region has many faults and it is often hit with earthquakes. The last one is 1997 and those of 2016 are struck between Norcia and Valneria. Landslide hazard can be caused by kinds of possible cracks, ridges, and scarp along with explaining the cut-and-fill failures.
论文代写:意大利翁布里亚
The analysis of the land and the anatomy of the land help in the predictive analysis of defining the plausible landslide issues in the areas. The most common kinds of landslides are described in the following. One of the most common landslides is known as the slide. These can be the translational slides or the rotational slides. In some cases, it can be a debris flow. This is a form of rapid mass movement that occurs based on the intensity of the surface-water flow or due to heavier precipitation. These are the factors that cause these landslides (Guzzetti et al., 2005). The landslides occur based on the seismic activity. It indicates the probability of earthquake or other probable areas of dangers that exist in the land. The maps are drawn to denote the kinds of probable landslide region based on the aspects of the physical terrain of the land. These have a number of features that cause a particular event to occur and lead to the creation of the land in the area. These are probed in the following section.