Unconformities Flashcards

1
Q

Deposition in fluvial basics

A

Meandering stream
braided stream
Flood plain

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2
Q

energy and velocity changes in rivers

A

energy-
high at source
drops at med
low at mouth
high on outside of bend
low on inside of bend

velocity-
high where steep gradient
lowers where flatter
high on outside of bend
low on inside of bend
low where tributary or lake joins

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3
Q

effect of velocity on dep

A

As velocity decreases deposition increases
e.g. inside of bend

must be very low to dep fine sed e.g. clay

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4
Q

meandering stream

A

high e on outside of bend = erosion
low e on inside of bend = deposition

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5
Q

braided stream

A

semi arid area = lack of rainfall

sudden deposition due to lack of rain or melt water

dep of C material e.g. sand and pebbles leads to blockages that the river braids around

dep at front of blockages

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6
Q

Flood plain

A

flat plain adjacent to body of water

flooded at times of high energy

very low energy, allows for dep of very fine particles e.g. clay

may see dessication cracks if irregularly flooded

good for fossils as low e and fine sed

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7
Q

Breccia vs conglomerate

A

Breccia-
C grain
angular- short transport
poorly sorted- rapid dep
e.g. wadi/alluvial fan

conglomerate-
C grain
rounded- longer transport
poorly sorted- rapid dep
e.g. river/beach

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8
Q

Hot desert enviro basics

A

wadi conglomerate
aeolian sandstone
alluvial fan arkose
playa lake evaporates

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9
Q

Wadi conglomerate

A

wadi- desert stream channel dry except for rainy season (often ravine or valley)

high energy- transports coarse material

lack of rain- rapid dep as water seeps into porous rock = poorly sorted

conglomerate= poorly sorted, subrounded (more rounded as more transport/ Secondary transport e.g. melt water)

red due to iron oxide

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10
Q

alluvial fan arkose

A

water rushes down then spreads out= fan shape (rapid dep)

dep nearer the mountain= coarse then fines out

breccia near mountain

arkose near middle

arkose= sand stone with 25% + feldspar (often from granite upstream)

arkose shows little weathering as quartz and feldspar=hard

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11
Q

aeolian sandstone

A

aeolian = wind

aeolian sandstone= formed from wind

often see large crossbedding/asymmetrical ripples

red due to iron oxide

Very well sorted + rounded and highly spherical

frosted due to attrition

entirely quartz due to weathering away

silica cement

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12
Q

Playa lake evaporates

A

playa= dry lake bed

playa lake= temp lake in arid enviro

h20 evaporates,
dissolved ions become concentrated,
least soluble salts come out of solution on edge of lake,
more soluble salts further in

playa lakes form as streams don’t reach sea due to high evaporation
infiltrate playa lake instead

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13
Q

Dep in carbonate environments basics

A

Shallow-
bioclastic/fossiliferous
reef
oolitic

deep-
chalk
micritic

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14
Q

Bioclastic/fossiliferous limestone

A

Up to 75% fossils

rest= calcareous + og deterial mud

Grey and crumbly
hard and well jointed and massive beds
contains broken segments of crinoids

commonly formed mid jurassic

sometimes whole fossils mostly broken due to transport

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15
Q

reef limestone

A

CO3 secreting algae engluf reef and cement it together

mostly coral

unbedded and has trilobite+ bivalve fossils

form in warm (23-25) shallow(>25m) high e

atoll- coral colonise Island, island sinks, coral ring

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16
Q

Oolitic limestone

A

white/yellow if iron stained

often crossbedding

oolith= nucleus rolled in CO3 mud bu current in tropical climate less the 2m

shallow sea

aragonite to calcite as more stable

common see fossils prev on sea floor- some whole some fragment

17
Q

Chalk

A

white, hard, massive, well jointed

compound of coccoliths, cancerous disks or oval platelets (from single celled planktonic algae)

May = micofossils of calc foraminifera/ Marco fossils of brachiopods

Low e and deep (<200m)

only if little sed supplied from land

Flint nodules common

18
Q

Micritic

A

Fine, hard (crystalline) from diagenisis of calcareous mud

calcareous mud produced by precipitate from sea / by CO3 secreting algae

planktonic foraminifera to calcareous ooze buried diagenesis to micritic limestone

buried as O crust moves away from the ridge to greater depth

19
Q

Beach

A

Includes Lattoral zone

sed dep here by rivers

High e and bilateral flow = sym ripple marks

May have shells + fossils (shelled orgs or trace fossils)

back= large clasts e.g. boulder/pebbles
Mid= gravel to C sand
In H2O= med + fine sand to mud (silt+clay)

clay settles out last as smallest

After mud oft limestone (remains of shelled orgs)

20
Q

Shallow sea

A

Lowest tide to cont shelf

sed dep here from rivers

lower e than beach + unidirectional flow = assym ripple marks

average H2O depth 130m

transgression = fining up

Regression = fining down

Also great e.g. of Walthers law
lime, Shale and sand

21
Q

What is a delta + description?

A

Where river flows into sea

Carries sed, meets the sea, loses E, dep sed

Delta= fan shape as load spreads wide

coaser closer to mouth
finer further out

22
Q

Conditions to preserve a delta

A

Little wave action and low tidal range

Non in Uk

23
Q

What causes distributary channels?

A

River channels quickly fills with sed as high dep
splits
distributary channels
many routes to sea

24
Q

Different sections of Delta Dep

A

Delta top- above water

Delta front- where river meets sea

Pro Delta- far Into sea

25
Q

Delta top

A

Above water
mostly dis channels + swap + flood plains

swap = anaerobic = form peat = diagentic processes = form coal

Trees grow here = form seat earth (sand and clay rich soil

delta switching- channles oft change course
lateral changes in coarse to sea

Sep dep here called TOP SETS
C grained + gravel to Channel sandstone (often crossbedded)

26
Q

Delta Front

A

River meets sea
C grained dep first to silt last (finer lower down and marine fossils may be found)

front of delta eventually migrates into sea - leads to vert succession (fining down)

Sed dep here called FORE SETS
C sand oft crossbedded

crescent shaped mouth bars form here

E lost as enters sea = very clean sand
as current removes fine sed

27
Q

Pro Delta

A

Dep at low E in deeper H2O

Dep here called BOTTOM SET
clay and silt

thinly bedded
lacks sed structures

lithify = form Shale
May contain marine fossils

28
Q

Pro Delta

A

Dep at low E in deeper H2O

Dep here called BOTTOM SET
clay and silt

thinly bedded
lacks sed structures

lithify = form Shale
May contain marine fossils

29
Q

sed sequences in Delta

A

form as Delta progrades into sea

D top overlays earlier D front

Shale-silt-sandstone-seat earth-coal (upward)

coal and roots give away

30
Q

Formation of disbrutary mouth bars

A

Cresent shaped mouth bars

silt and sand

where dis channel enters sea

31
Q

Sed transport in rivers

A

Sorted by size

often sub mature

C nearer source
med downstream e.g. sand
fine at mouth e.g. clay

some rivers end in shallow marine=quick dep

32
Q

Sed transport by wind

A

Min mature
eroded by attrition and abrasion

calcite sometimes present
usually in sol to dry and arid

texturally mature (W rounded and sorted)

Highest E

33
Q

Sed transported by Glacier

A

Poor sorted
tillite has large range

angular

Glacial till = dep name

May be transported by melt water = fluvial glacial dep= like river

34
Q

Shallow siliciclastic

A

sep dep in littoral zone (H to L tide)

High E

also dep on cont shelf

see sorting with distance

35
Q

Types of Conglomerate

A

Polymicritic = C grained sed rock containing clasts of many diff rock types

Oligomictic = “ few diff rock types

Monomicritic = “ single rock type

36
Q

Dep in shallow siliciclastic enviros basic

A

Beach and Shallow sea