Search by property

From CSDMS

This page provides a simple browsing interface for finding entities described by a property and a named value. Other available search interfaces include the page property search, and the ask query builder.

Search by property

A list of all pages that have property "Theory movie" with value "A debris flow is a fast moving mass of unconsolidated, saturated debris that looks like flowing concrete. They differentiate from a mudflow by terms of the viscosity of the flow. Flows follow a steepest descent generally, although they are known the “climb” opposite valley walls in extreme cases. The front of the debris flow, or the toe, forms a lobe, marking flow front. This lobe often contains a great deal of the larger sediments including cobbles and boulders. Early pulses or previous debris flows form levees that channel the flow until they are breached. The presence of older levees indicates the recurrence and characteristics of debris flows in a particular area. This can be an important indicator of past debris flow activity for developing land on alluvial fan terrace surfaces. But, flows can carry clasts ranging in size from clay particles to boulders, and may contain woody debris. During later phases of the event, more viscous mud that contains sands, silts, and fines runs through the flowpath. Debris flows can be triggered by large amounts of rainfall, snow melt, or glacial/permafrost melt, or a combination of all. Speed of debris flows can vary from 0.5 m/s to 16 m/s in extreme conditions. Variables in the conditions that affect debris flow characteristics are slope, available sediment and vegetation in the flowpath. Debris flow are extremely destructive to life and property. This particular event happened on July 2nd, 2006. This is during the middle of the Southern Hemisphere's Austral Winter, but the temperature was unseasonally high at 32º C! It was the warmest July day ever recorded (pers. comm. W. Keller). This debris flow event is attributed to hydrothermal alteration of the local mountain flank and the melting of permafrost.". Since there have been only a few results, also nearby values are displayed.

Showing below up to 2 results starting with #1.

View (previous 50 | next 50) (20 | 50 | 100 | 250 | 500)


    

List of results

    • Movie:DebrisFlowChile  + (A debris flow is a fast moving mass of uncA debris flow is a fast moving mass of unconsolidated, saturated debris that looks like flowing concrete. They differentiate from a mudflow by terms of the viscosity of the flow. Flows follow a steepest descent generally, although they are known the “climb” opposite valley walls in extreme cases. The front of the debris flow, or the toe, forms a lobe, marking flow front. This lobe often contains a great deal of the larger sediments including cobbles and boulders. Early pulses or previous debris flows form levees that channel the flow until they are breached. The presence of older levees indicates the recurrence and characteristics of debris flows in a particular area. This can be an important indicator of past debris flow activity for developing land on alluvial fan terrace surfaces.</br>But, flows can carry clasts ranging in size from clay particles to boulders, and may contain woody debris. During later phases of the event, more viscous mud that contains sands, silts, and fines runs through the flowpath.</br>Debris flows can be triggered by large amounts of rainfall, snow melt, or glacial/permafrost melt, or a combination of all. Speed of debris flows can vary from 0.5 m/s to 16 m/s in extreme conditions. </br>Variables in the conditions that affect debris flow characteristics are slope, available sediment and vegetation in the flowpath. </br>Debris flow are extremely destructive to life and property.</br></br>This particular event happened on July 2nd, 2006. This is during the middle of the Southern Hemisphere's Austral Winter, but the temperature was unseasonally high at 32º C! It was the warmest July day ever recorded (pers. comm. W. Keller). This debris flow event is attributed to hydrothermal alteration of the local mountain flank and the melting of permafrost.ntain flank and the melting of permafrost.)