törmelékkúphoz

Törmelékkúphoz is a Hungarian term that translates to "scree cone" or "talus cone" in English. It refers to a geological landform created by the accumulation of rock debris, known as scree or talus, at the base of a steep slope, cliff, or mountain. This accumulation occurs due to gravitational processes such as rockfalls, landslides, and erosion.

These cones are typically found in mountainous or hilly regions where weathering and erosion are significant. The material forming the törmelékkúphoz is usually angular and unsorted, ranging in size from fine gravel to large boulders. The angle of the slope of the törmelékkúphoz is dependent on the size and shape of the individual rock fragments, as well as the presence of any binding material like soil or vegetation.

The formation of a törmelékkúphoz is a continuous process. As rocks weather and break down, they fall or slide down the slope, gradually building up the cone. Over long geological periods, these cones can become quite substantial features. Vegetation may eventually colonize the surface of older törmelékkúphoz, helping to stabilize the debris and slow down further accumulation. The study of törmelékkúphoz can provide insights into the erosional history and geological activity of a region.