Unconformities As + A2 Flashcards
Deposition in fluvial basics
Meandering stream
braided stream
Flood plain
energy and velocity changes in rivers
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
effect of velocity on dep
As velocity decreases deposition increases
e.g. inside of bend
must be very low to dep fine sed e.g. clay
meandering stream
high e on outside of bend = erosion
low e on inside of bend = deposition
braided stream
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
Flood plain
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
Breccia vs conglomerate
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
Hot desert enviro basics
wadi conglomerate
aeolian sandstone
alluvial fan arkose
playa lake evaporates
Wadi conglomerate
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
alluvial fan arkose
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
aeolian sandstone
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
Playa lake evaporates
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
Dep in carbonate environments basics
Shallow-
bioclastic/fossiliferous
reef
oolitic
deep-
chalk
micritic
Bioclastic/fossiliferous limestone
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
reef limestone
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