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GEOGRAPHY
WEATHERING
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Created by
Laragh Cunningham-Ash
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Cards (20)
Denudation
Weathering
and
erosion
Weathering
1. A
process
2. Causes
rocks
to be
broken
3.
Over time
Weathering
Happens in
situ
(the place where a rock happens to be)
Erosion
A process that
breaks
rocks into smaller pieces by transporting sediments by agents of
erosion
(rivers, sea, glaciers and wind)
Types of weathering
Mechanical
weathering
Chemical
weathering
Biological
weathering
Mechanical
weathering
Physically breaks rocks apart
Produces broken rock called
scree
Chemical weathering
Involves rock being
dissolved
gradually over time
Biological weathering
Occurs when rock is broken apart by
burrowing
animals or by
plant growth
Freeze-thaw action
1.
Rainwater
gathers in rock
joints
2.
Water freezes
and
expands
by 10%
3.
Expansion widens joints
4. Over time, rock breaks and
collapses
into
scree
Carbonation
A chemical weathering process where rock is
dissolved
by
weak
carbonic acid
Limestone
Soft
sedimentary
rock
Composed of
calcium carbonate
from
fossils
Has bedding planes and
joints
that make it
permeable
Acid
rain falls on
limestone
Dissolves
the weaker parts of the
limestone
surface
Karst landscape
Pattern of joints and grikes formed by
carbonation
weathering of
limestone
Features of the Burren
Varied
flora
and
fauna
Spring
gentians,
early-purple
orchid and mountain avens
Feral
goats, stoat, pine marten and
Irish
hare, rare insects and butterflies
The
Burren
is a large area of exposed
limestone
, or karst, in Co. Clare
The
limestone
rock in the Burren was deposited under a
shallow
ocean when Ireland lay at the equator, 365 million years ago
Most of the soil in the
Burren
was removed by
glacial erosion
, leaving the rock bare and exposed to the weather
Stalactites
Slender columns of
calcite
that hang from the ceiling of a cave, formed by water
evaporation
Stalagmites
Thick columns of calcite that build up on the floor of a
cave
, formed by
water evaporation
If a
stalactite
and stalagmite meet they form a
pillar