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		<summary type="html">&lt;p&gt;CSV import&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;== Earthflow ==&lt;br /&gt;
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&amp;lt;!--[[File:Earthflow.jpg|--&amp;gt;[[An example of an earthflow in California]]&lt;br /&gt;
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An &amp;#039;&amp;#039;&amp;#039;earthflow&amp;#039;&amp;#039;&amp;#039; is a type of [[landslide]] characterized by the slow, downslope movement of saturated soil and rock materials. It is a common geological phenomenon that occurs in various regions around the world, particularly in areas with steep slopes and abundant rainfall. Earthflows can cause significant damage to infrastructure, pose risks to human settlements, and have long-lasting impacts on the landscape.&lt;br /&gt;
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=== Formation ===&lt;br /&gt;
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Earthflows typically occur in areas with specific geological and environmental conditions. They are commonly triggered by heavy rainfall or snowmelt, which saturates the soil and reduces its strength. The combination of gravity and the weakened soil structure causes the downslope movement of material. Additionally, the presence of clay-rich soils, known as [[silt]] or [[loess]], is often a contributing factor to the formation of earthflows. These fine-grained soils have a high water-holding capacity, making them prone to becoming saturated and losing their stability.&lt;br /&gt;
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=== Characteristics ===&lt;br /&gt;
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Earthflows are characterized by their slow and continuous movement, which distinguishes them from other types of landslides. The movement can range from a few centimeters per year to several meters per day, depending on the slope gradient, soil composition, and water content. The material involved in an earthflow can vary from fine-grained sediments to larger rock fragments. As the material moves downslope, it often accumulates at the base, forming a distinct lobe-shaped feature.&lt;br /&gt;
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=== Impacts ===&lt;br /&gt;
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The movement of earthflows can have significant impacts on both natural and human environments. In natural settings, earthflows can alter the topography of the landscape, creating new landforms and modifying drainage patterns. They can also disrupt ecosystems and cause changes in vegetation patterns. In urban areas, earthflows can damage infrastructure such as roads, buildings, and pipelines. They pose risks to human settlements, as the slow movement can gradually undermine foundations and structures, leading to potential collapse or damage.&lt;br /&gt;
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=== Mitigation and Management ===&lt;br /&gt;
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Managing and mitigating the risks associated with earthflows require a comprehensive approach that involves understanding the geological conditions, monitoring the movement of the earthflow, and implementing appropriate engineering measures. Some common strategies include slope stabilization techniques, such as the installation of retaining walls or drainage systems to control water flow. Additionally, land-use planning and zoning regulations can help prevent development in high-risk areas prone to earthflows.&lt;br /&gt;
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=== See Also ===&lt;br /&gt;
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* [[Landslide]]&lt;br /&gt;
* [[Slope stability]]&lt;br /&gt;
* [[Geotechnical engineering]]&lt;br /&gt;
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=== References ===&lt;br /&gt;
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&amp;lt;references /&amp;gt;&lt;br /&gt;
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[[Category:Geology]]&lt;br /&gt;
[[Category:Landslides]]&lt;br /&gt;
[[Category:Geomorphology]]&lt;br /&gt;
[[Category:Environmental hazards]]&lt;/div&gt;</summary>
		<author><name>Prab</name></author>
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