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There are several factors affecting mass movement:
- The ground freezes and re-freezes throughout a year.
This leads to water being trapped above the permafrost.
- The temperature isn’t high enough for the water to evaporate.
- There is little vegetation to hold the soil together
The ground is often on slopes
Mass Movement Cont…
Solifluction = important periglacial process as widespread occurrence
Definition = when the active later thaws in summer, excessive lubrication reduces the friction between soil particles – leads to solifluction or lobes
Appearance = these are rounded, tongue-like features often forming terraces on the sides of valleys
Effect = to reduce and smooth out the relief as weathered and loose deposited materials are transferred from upper slope to downslope
Therefore, there are more features at the foot of the slope:
Mass Movement Cont
The formation of lobes and terraces gives it a greater form
by making the lower slopes rounder and flatter areas:
There are two types of lobes
These are both controlled by the amount of vegetation
Lack of vegetation cover, stone-banked lobes/terrace formed:
Small-lobes – rising up to 5m then extending up slope to form terrace between 10-30 metres long
Distinctive feature – each lobe is the stone wall behind the finer material
Stones on surface travel quicker downslope that finer materials until something changes the movement, e.g. vegetation
Finer material accumulates behind the wall to form a terrace
Mass Movement Cont
Forms under continuous vegetation cover where frost heaving is less effective at raising stones to surface
Turf-banked lobes and terraces form instead, as it is the surface layers of turf and topsoil which are moved by solifluction
Terraces are created where minor relief obstructs movement, rolling up the turn flow backwards under continued surface movement
= forms as the riser below the lobe
When held together by vegetation and roots, lobes usually and cover larger areas on lower slopes then stone-banked areas
Mass Movement Finally!!!
Fossil solifluction deposits are the most widespread periglacial relict feature in the British Isles
General term for this = Head deposits
Widespread below outcrop of granite on Dartmoor and elsewhere in S.W England
Coombe Rock =
Name given to fans of chalk below escarpments and in dry valleys in down land regions in Southern England
Lobes/terraces identified in uplands of Scotland and Wales are exposed to actions of solifluction for the longest time in the British Isles
Frost Action and Resulting Landforms
Freeze-thaw is the most common weathering process in periglacial areas.
It brakes down the majority of rocks on the mountainsides and many of the landforms lower down.
Name given to very irregular surfaces of mostly hollows and small hummocks.
These pitted surfaces resemble those formed by solution in some karst areas of limestone.
Small domes that form on surface due to frost heaving with the onset of winter are only features.
They then collapse in summer thaw leaving small surface depressions.
Some ice lenses grow and form surface hummocks whish may last many years before they thaw.
Small circular hills up to 50 or 60 m high
Occur in groups
Add to variety of thermokarst scenery
Pond in central crater makes even more distinctive
Greatest number found on flat lands in and around the Mackenzie Delta on Artic coast of N.W. Canada
Within each pingo is a large ice core, responsible for the frost heaving which forms the conical hill
After the lake forms, its ice core is no longer insulated against summer warmth – the gradient thaws away and the pingo form is lost
Stones in periglacial areas seemed to sort themselves out in to patterns. This is due to frost heaving.
The ice freezes underneath the stones which expand and pushes the stones upwards.
When they reach the surface they roll outwards.
Other Periglacial Processes and Landforms • Mechanical weathering by freeze-thaw is widespread. • Low temperatures, sparse vegetation cover and poorly developed soils reduce the likelihood of chemical and biological weathering taking place. • Lack of vegetation increases wind (aeolian) action. • Further erosion occurs as the wind-blown sand grains abrade rock outcrops. • Wind action produces semi-circular dunes of sandy outwash material. • It also produces wind-blown loess. • Loess is a fertile, easy to work soil. • A loess belt extends across Europe C
Europe’s Loess Belt C Loess
Artic Streams • The amount of transport and erosion in Arctic streams is also huge. • The high load comes from flowing over areas liberally covered by loose debris from glaciers. • The high discharge comes from melting ice. • 80% of the discharge comes in one or two months of the year. C