Explain talus scree slopes
State the landform left behind by rotational slumping
State the landform left behind by mudflows
often occur when water is channelled locally to saturate the soil – thus creating rills (eroded gullys) and lobes (front edge of deposition).
State three distinctive landforms at the coast
talus scree slopes, rotational scars, terraced cliff profiles
Landform left by blockfalls
– Debris material tends to stay in larger sizes - often leaves a clean scar above along the failure line (e.g bedding plane)