Pyroclastic Rocks Flashcards

(23 cards)

1
Q

What is an ignimbrite?

A

A deposit of a pyroclastic density current rich in pumice or pumiceous ash shards
Tuff, lapilli-tuff and breccia

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2
Q

What is a pyroclastic density current?

A

Ground hugging current of pyroclasts and air

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3
Q

Give 4 features of welding

A

High temperature emplacement of PDC
Pumice and glass still malleable
Fusing together of pumice and shards
Compaction

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4
Q

What is fiamme and how is it formed?

A

A lens

Forms from flattened pumice shards in a welded ignimbrite

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5
Q

How does temperature effect depositonal features?

A

Welded or non-welded
Agglutination - rapid syn depostional welding of hot pyroclasts - clasts visible
Coalescence - rapid syn depostional welding of hot pyroclasts - clasts not visible

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6
Q

What lava like features can an ignimbrite have?

A

Flow banding and folding

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7
Q

How do you distinguish between lava and lava like ignimbrites?

A

Evidence of fragmentation (vitroclastic textures, broken crystals
Field characteristics - tuff gradations, internal variations in flow laminae, internal breccia zones, no basal autobreccia
Vertical chemical stratification is impossible in lava

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8
Q

Where do fountain-fed lavas come from and what are they typically composed of?

A

From fissure eruptions and central veins
Variably welded spatter and sporia
Fall deposits coalesce

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9
Q

How do PDCs behave?

A

Deposits accumulate gradually, reflect material collected at a particular time
Prolonged with waxing and waning over time

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10
Q

How do fully dilute PDCs move?

A

Collisional momentum has little effect, transport dominated by turbulence of the fluid phase, usually involves traction and saltation
Essentially suspension
Non-stratified

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11
Q

Why is there high shear at flow boundary in fully dilute PDCs?

A

Individual clasts subjected to lift and drag of fluid
Slide, roll and saltates along substrate before deposition
Impingment of eddies cause entrainment and segregation

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12
Q

How do granular fluid dilute PDCs move?

A

Collision between grains dominates, little turbulence

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13
Q

Describe granular fluid dilute PDC deposition

A

Typically massive deposits
Grain interactions dominate clast support
Preferential deposition of fines by overpassing and perlocating

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14
Q

Summarise fluid dilute and granular fluid based conditions

A

Fully dilute - direct fallout and traction dominated

Granular dilute - granular flow dominated and fluid escape dominated

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15
Q

What do matrix supported lithic blocks show in ignimbrites?

A

Thickness of aggraded unit before deposition

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16
Q

Where do lithic blocks come from in ignimbrites?

A

Erosion/collapse of vent walls
Avalanches into PDC
Erosion of substrate by PDC
Ballistic blocks ejected from vent

17
Q

What does normal grading in lithics show?

A

Waning current

Decreasing lithic avaliability

18
Q

What does inverse grading in lithics and pumice show?

A

Waxing current

Increasing lithic and pumice avaliability

19
Q

What four features demonstrate sustained eruptions?

A

No palaeosols, lavas, sedimentary rocks or fall deposits

20
Q

Why might an ignimbrite only give a partial record of PDC?

A

Bypassing currents may leave no deposits for part of the deposition
Erosion through groove marks - long linear clasts filled by ignimbrite or gutter clasts - erosional scours

21
Q

What effect does water have on fragmentation?

A

Enhances it, produces abundant fine grained ash

22
Q

How does moisture create ash aggregates?

A

Hydrostatic and electrostatic agglomeration of ash

23
Q

What does an ash aggregate do and what forms can it come in?

A

Simple fall deposits from plume

Ash pellet, cored pellet, coated ash pellet, accretionary lappilus, Cored accretionary lappilus