lammonsiirtostruktuurit
Lammonsiirtostruktuurit, often translated as "lamella transfer structures" or "sheet transfer structures," refer to a specific type of geomorphological feature found in certain glacial landscapes. These structures are characterized by the deposition of sediment in thin, elongated, and relatively flat layers, known as lamellae. They are typically formed by meltwater streams that flow over or beneath glaciers.
The formation process involves the entrainment and transport of sediment by glacial meltwater. As the water
Lammonsiirtostruktuurit are often associated with areas of low gradient where meltwater flow is relatively steady. They