Nivation
Encyclopedia
Nivation is a collective name for the different processes that occur under a snow patch
. The primary processes are mass wasting
and the freeze and thaw cycle
, in which fallen snow
gets compacted into firn
or névé
. The term glacier
is applied only when ice has accumulated enough for the mass to achieve motion.
Nivation has come to include various subprocesses related to snow patch
es which may be immobile or semi-permanent. These sub-processes include erosion
(if any) or initiation of erosion, weathering
, and meltwater
flow from beneath the snow patch.
Weathered particles are moved downslope by creep
, solifluction
and rill wash. Over time, this leads to the formation of nivation hollows which, when enlarged, can be the beginnings of a cirque
.
Snow patch
Snow patch is a geomorphological pattern of snow and firn accumulation which lies on the surface longer time than other seasonal snow cover. There are two types to distinguish; seasonal snow patches and perennial snow patches. Seasonal patches usually melt during the late summer but later than rest...
. The primary processes are mass wasting
Mass wasting
Mass wasting, also known as slope movement or mass movement, is the geomorphic process by which soil, regolith, and rock move downslope under the force of gravity. Types of mass wasting include creep, slides, flows, topples, and falls, each with its own characteristic features, and taking place...
and the freeze and thaw cycle
Frost weathering
Frost weathering is a collective name for several mechanical weathering processes induced by stresses created by the freezing of water into ice. The term serves as an umbrella term for a variety of processes such as frost shattering, frost wedging and cryofracturing...
, in which fallen snow
Snow
Snow is a form of precipitation within the Earth's atmosphere in the form of crystalline water ice, consisting of a multitude of snowflakes that fall from clouds. Since snow is composed of small ice particles, it is a granular material. It has an open and therefore soft structure, unless packed by...
gets compacted into firn
Firn
Firn is partially-compacted névé, a type of snow that has been left over from past seasons and has been recrystallized into a substance denser than névé. It is ice that is at an intermediate stage between snow and glacial ice...
or névé
Névé
Névé is a young, granular type of snow which has been partially melted, refrozen and compacted, yet precedes the form of ice. This type of snow is associated with glacier formation through the process of nivation. Névé that survives a full season of ablation is referred to as firn, which is both...
. The term glacier
Glacier
A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation over many years, often centuries. At least 0.1 km² in area and 50 m thick, but often much larger, a glacier slowly deforms and flows due to stresses induced by its weight...
is applied only when ice has accumulated enough for the mass to achieve motion.
Nivation has come to include various subprocesses related to snow patch
Snow patch
Snow patch is a geomorphological pattern of snow and firn accumulation which lies on the surface longer time than other seasonal snow cover. There are two types to distinguish; seasonal snow patches and perennial snow patches. Seasonal patches usually melt during the late summer but later than rest...
es which may be immobile or semi-permanent. These sub-processes include erosion
Erosion
Erosion is when materials are removed from the surface and changed into something else. It only works by hydraulic actions and transport of solids in the natural environment, and leads to the deposition of these materials elsewhere...
(if any) or initiation of erosion, weathering
Weathering
Weathering is the breaking down of rocks, soils and minerals as well as artificial materials through contact with the Earth's atmosphere, biota and waters...
, and meltwater
Meltwater
Meltwater is the water released by the melting of snow or ice, including glacial ice and ice shelfs over oceans. Meltwater is often found in the ablation zone of glaciers, where the rate of snow cover is reducing...
flow from beneath the snow patch.
Weathered particles are moved downslope by creep
Downhill creep
Downhill creep, or commonly just creep, is the slow downward progression of rock and soil down a low grade slope; it can also refer to slow deformation of such materials as a result of prolonged pressure and stress. Creep may appear to an observer to be continuous, but it really is the sum of...
, solifluction
Solifluction
In geology, solifluction, also known as soil fluction, is a type of mass wasting where waterlogged sediment moves slowly downslope, over impermeable material. It occurs in periglacial environments where melting during the warm season leads to water saturation in the thawed surface material ,...
and rill wash. Over time, this leads to the formation of nivation hollows which, when enlarged, can be the beginnings of a cirque
Cirque
Cirque may refer to:* Cirque, a geological formation* Makhtesh, an erosional landform found in the Negev desert of Israel and Sinai of Egypt*Cirque , an album by Biosphere* Cirque Corporation, a company that makes touchpads...
.