Sedimentary Flashcards
Why is there a difference between the minimum erosion velocity and the maximum deposition velocity of a particle
-greater velocity is required to overcome inertia of the grain
-once moving it has momentum so less velocity required to keep it moving
-more energy needed to pick up than deposit
Why does the critical erosion velocity on a hjulstrom graph increases for particles smaller than 1mm
- higher velocity to produce the energy required to separate the clay particles
- which have flocculated
- because of a small charge
- cohesion
- stick together
Why are grains well sorted in a fluvioglacial deposit
- Because stream velocity would have been fairly constant
- transporting finer material downstream
How do we know that a sediment is fluvioglacial rather than glacial origin
Fluvioglacial sediments are
- rounded
- because of attrition
- sorted
- imbricated (overlap)
- indicate a unidirectional flow
What are physical characteristics of sediment particles that could influence the pick up, transport and deposition
- particle size
- particle density
- particle shape
Why are high stream velocities required to pick up particles smaller than 0.1mm
- smaller particles have higher cohesion
- greater charge per unit area
- water can’t get between/beneath grains
- smaller particles do not stick up so far in flow
- present a smooth surface which is more resistant
Once very fine grained particles (clay) are picked up how are they deposited on reaching the sea
- low energy/stagnant water - mud flats of estuary
- flocculation of particles when they reach the sea
- sea is an ionic solution which reduces the charge in the particles which prevent particle collision
- therefore clay particles collide and fall out of suspension
What are possible causes of a turbidity flow
- earthquake
- storm
- slump