A very slow movement of rock downhill is <u>Creep</u>.
<h3>Further explanation</h3>
Landslide or soil movement is the process of mass transfer of rock or soil due to gravity. Landslides have been a concern of geologists because of their effects. They have caused many lives and property losses.
The internal factors of landslides are the weak binding capacity of soil or rock. Besides internal, the external factors that can accelerate landslides are the form of a slope, precipitation, soil or rocks moisture, and lack of vegetation.
→ The slow flowage landslides consist of:
a. Creep is the movement of rock and soil material toward the foot of a slope with very slow movements.
b. Soil creep is the movement of soil material toward the foot of a slope.
c. Talus creep is the movement towards the foot of a talus material slope.
d. Rock creep is the displacement toward the foot of the rock blocks slope.
e. Rock-glacier creep is displacement towards the foot of the slope from waste rock.
f. Liquefaction is a very slow flow to the foot of the slope from water-saturated rock debris material.
<h3>Learn more</h3>
- Metamorphic rocks: brainly.com/question/1580749
- The characteristic of lithospheric plates: brainly.com/question/2722711
- The soil profiles: brainly.com/question/138504
<h3>Answer details</h3>
Subject: Geography
Chapter: The Dynamics of the Lithosphere and Its Impact on Life
Keywords: creep, soil creep, kind of soil creeps, landslide, the factors of erosion