Catatan: Terjemahan untuk entri ini sedang dalam peninjauan kualitas, sehingga sebagian konten untuk sementara hanya ditampilkan dalam bahasa Inggris.
Entri ini belum diterjemahkan ke bahasa Anda, sehingga versi aslinya ditampilkan di bawah.
solifluction
This term is a specialized geological and geomorphological descriptor used primarily in the study of periglacial environments. It describes a specific type of mass wasting where the top layer of soil thaws and becomes saturated with water, allowing it to slide slowly over a frozen, impermeable substrate. This process is distinct from general landslides or mudflows due to its extreme slowness and its dependence on the freeze-thaw cycle.
In technical literature, the term is often associated with the formation of solifluction lobes or terraces, which are characteristic landforms found in tundra or high-altitude regions. Because it is a precise scientific term, it is rarely used outside of academic, environmental, or geological contexts.
Meanings
Examples
Solifluction occurs when the active layer of soil thaws but cannot drain into the frozen permafrost below.
Solifluction occurs when the active layer of soil thaws but cannot drain into the frozen permafrost below.
Look at those lobes on the hillside; they are classic signs of solifluction.
The slow process of solifluction gradually reshapes the tundra landscape over centuries.
Is solifluction different from a standard landslide?
Water-saturated regolith moves downslope via solifluction during the summer thaw.
I wonder if solifluction is responsible for the distorted patterns in these ancient soil layers.
The geologist explained how solifluction creates distinct terracettes on the slope.
High moisture content and a steep gradient accelerate the rate of solifluction.
Solifluction is a primary mechanism of mass wasting in periglacial environments.
Solifluction is a primary mechanism of mass wasting in periglacial environments.