Sedimentary Flashcards

1
Q

Why is there a difference between the minimum erosion velocity and the maximum deposition velocity of a particle

A

-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

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2
Q

Why does the critical erosion velocity on a hjulstrom graph increases for particles smaller than 1mm

A
  • higher velocity to produce the energy required to separate the clay particles
  • which have flocculated
  • because of a small charge
  • cohesion
  • stick together
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3
Q

Why are grains well sorted in a fluvioglacial deposit

A
  • Because stream velocity would have been fairly constant
  • transporting finer material downstream
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4
Q

How do we know that a sediment is fluvioglacial rather than glacial origin

A

Fluvioglacial sediments are
- rounded
- because of attrition
- sorted
- imbricated (overlap)
- indicate a unidirectional flow

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5
Q

What are physical characteristics of sediment particles that could influence the pick up, transport and deposition

A
  • particle size
  • particle density
  • particle shape
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6
Q

Why are high stream velocities required to pick up particles smaller than 0.1mm

A
  • 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
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7
Q

Once very fine grained particles (clay) are picked up how are they deposited on reaching the sea

A
  • 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
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8
Q

What are possible causes of a turbidity flow

A
  • earthquake
  • storm
  • slump
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