Final answer:
Solifluction areas usually have scarce drainage channels due to the slow downslope movement of soil and limited water infiltration into frozen ground.
Step-by-step explanation:
Solifluction refers to the slow downslope movement of soil and sediment due to the presence of water in the upper layers. It commonly occurs in areas with cold climates and , such as high latitudes and high altitudes. Solifluction usually happens in regions where the soil remains saturated with water but is frozen underneath, which prevents proper drainage. As a result, drainage channels are usually scarce in solifluction areas.
For example, in regions with solifluction, the waterlogged soil cannot seep into the frozen ground, leading to the formation of surface flow paths or small ponds. These areas have limited channels for water to drain away.
Therefore, the statement is True.