löyhäkivet

Löyhäkivet is a Finnish term that translates to "loose stones" or "rubble" and typically refers to a geological formation or a specific type of terrain. It is characterized by an accumulation of fragmented rocks and debris that are not cemented together. These formations can occur naturally due to various geological processes, such as weathering, erosion, or glacial activity.

In a natural context, löyhäkivet can be found on hillsides, at the base of cliffs, or in areas where rock has been broken down over time. The size of the stones can vary from small pebbles to larger boulders. The composition of löyhäkivet depends on the parent rock material from which it originated, potentially including granite, gneiss, or sedimentary rocks.

The term can also be used in construction or engineering contexts to describe loose rock material used as fill or in the construction of certain types of walls or foundations. In these instances, the löyhäkivet are often sorted by size to achieve specific structural properties. The stability and suitability of löyhäkivet for construction depend on factors like the size and shape of the fragments, their arrangement, and the presence of any binding material. The term emphasizes the unconsolidated nature of the material.