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The conflagrations devastated steep slopes, which caused loss of vegetation and destabilization of the soil and greatly facilitated subsequent mudflows. The mudflows caused at least $177 million (2018 USD) in property damage, [2] and cost at least $7 million in emergency responses [2] and another $43 million (2018 USD) to clean up. [3]
Huge landslide at La Conchita, 1995. A geologic hazard or geohazard is an adverse geologic condition capable of causing widespread damage or loss of property and life. [1] These hazards are geological and environmental conditions and involve long-term or short-term geological processes.
The Highland Towers complex was built in phases between 1974 and 1982. It was constructed at the western base of a steeply sloped hill, terraced extensively in the early 1980s. Block 1 was the southernmost building, Block 2 was built north-northwest of Block 1, and Block 3 was built west of Block 2.
Some landslides are complex in the sense that they feature different movement types in different portions of the moving body, or they evolve from one movement type to another over time. For example, a landslide can initiate as a rock fall or topple and then, as the blocks disintegrate upon the impact, transform into a debris slide or flow.
2.4.1.1 Large diameter wells. 2.4.1 ... Download as PDF; Printable version; In other projects ... Landslide mitigation refers to several human-made activities on ...
The most common examples of statute liability are in areas where an individual is required by law to effect insurance, e.g. workers' compensation and motor vehicle compulsory third party. Property, hotel and operations managers should become familiar with the various types of contracts involved in commercial and retail activities.
The 2010 Gansu mudslide was a deadly mudslide in Zhouqu County, Gansu Province, Gannan Tibetan Autonomous Prefecture, China that occurred at midnight on 8 August 2010. The floods were triggered after decades of clear cut logging practices had reduced the ability of the watershed to absorb heavy rainfall. [2] [3]
Sudden slumps usually occur after earthquakes or heavy continuing rains, and can stabilize within a few hours. Most slumps develop over comparatively longer periods, taking months or years to reach stability. An example of a slow-moving slump is the Swift Creek Landslide, a deep-seated rotational slump located on Sumas Mountain, Washington.