Save
...
paper 1- physical
coastal landscapes and change
key words
Save
Share
Learn
Content
Leaderboard
Learn
Created by
in
Visit profile
Cards (36)
lithology
the physical characteristics of a rock
morphology
the
geological
structure,
shape
or form of a feature
submergent coastline
a coastline that is inundated by the sea su to eustatic or isostatic uplift/rebound (e.g Haff coast)
Emergent coastline
a coastline that has been exposed by
receding sea levels
or
isostatic uplift
/rebound
concordant
rock structure (lithology) runs
parallel
to the
coast
(creates coves)
discordant
rock lithology runs
perpendicular
to the coast creating bands of alternate rock types (e.g
headlands
and bays)
proxy records
records or data collected from other sources (e.g books or paintings)
geomorphology
the study of origins and evolution of the earth's
landforms
, and the factors wich
affect
them
sedimentary rock
rock formed over millions of years due to the accumulation of
sediment
(e.g
sandstone
)
Igneous
rock
rock formed by the cooling of
molten
magma (e.g
granite
)
Metamorphic
rock
rock formed from other rocks that have been changed due to heat or pressure (e.g
glacial till
)
Unconsolidated
often loosely formed mass of
soil
,
rock
and other parts that is weak and easy to break
permeability
allows liquid to pass through it (e.g sandstone)
impermeable
will not allow liquid to pass through it (e.g
Granite
)
temporal
realting to
time
hydraulic action
mechanical weathering caused by the force of moving
water currents
rushing into the cracks in the
rock face
, forcing it apart
attrition
weathering away of
materials
as it
collides
together
corrosion
erosion caused by the
acidity
within the
water
abrasion
erosion caused by the process of
scraping
or
wearing
something away
sediment cell
cells within the movement of sediment is
functionally
separated and
discrete
from the next
dynamic
equilibrium
the state in which inputs into a system is
equal
to the outputs
longshore drift
the movement of material along a coast by
wave action
, which approach at an angle to the shore but
recede
directly away form it
tombolo
a bar of
sand
or shingle
joining
an island to the mainland
cuspate
forelands
formed due to longshore currents by the accretion of
sediment
, they extend outwards from the shoreline in a
triangular
shape
rotational slump
when the slope fails and slides down due to undercutting or
weathering
or
unconsolidated
material
mass movement
soil,
sand
and rock move
downslope
typically as a mass, largely under the force of gravity or erosion
rotational scars
the scar left behind sue to a
rotational slump
fjord
long,
narrow
,
deep
inlet of the sea between high cliffs formed by the submergence of a glacial valley
isostatic
the movement of
land
sue to
glacial
melt or thermal expansion of the oceans
eustatic
a change of sea level due to
glacial melt
or
thermal expansion
of the oceans
accretion
the gradual growth of
sediment
accumulated by the
coast
storm surge
a rising of the sea as a result of
wind
and
atmospheric pressure
changes associated with a storm
depression
a weather front where
low
pressure causes air to rise; as it cools it condenses and forms
clouds.
tropical cyclone
very intense low-pressure
wind system
, forming over tropical oceans and with winds of
hurricane force
emergent coastline
a stretch along the coast that has been exposed by the
sea
by a relative
fall
in sea levels by either isostatic or eustatic change
submerging
coastline
a stretch along the coast that has been inundated by the
sea
by a relative
rise
in sea levels from either isostatic or eustatic change