Landslides in Durban, also known as eThekwini, can be triggered by a variety of factors, including heavy rainfall, erosion of slopes, deforestation, and human activities. The region experiences a subtropical climate with high levels of rainfall during the summer months, which can saturate the soil and destabilize the slopes, leading to landslides. In addition, the city is situated on hilly terrain, which makes it more susceptible to slope failures.
Deforestation and land clearing for development purposes can also contribute to landslides in Durban. Removing vegetation from steep slopes can increase the risk of erosion and destabilize the soil, making it more prone to sliding during heavy rainfall events. Urbanization and construction activities can also disrupt natural drainage patterns and increase the likelihood of landslides in the area.
Human activities such as mining and quarrying can also weaken the stability of slope surfaces and contribute to landslides in Durban. These activities can alter the natural geology of the area, creating unstable conditions that are more prone to slope failures. It is important for the city to implement proper land use planning and soil conservation practices to mitigate the risk of landslides and protect the residents and infrastructure of Durban.
What causes landslides in Durban(ethikwini) in 3 paragraphs
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