Childrens Illustrated Encyclopedia

(Marvins-Underground-K-12) #1

104


Caves

HOW CAVES FORM
Large cave systems lie
beneath the ground
in regions made of
limestone rock. For
thousands of years,
rainwater, which is
naturally acidic,
dissolved away the
limestone. Small
cracks formed, slowly
widening to create deep
holes, which became
underground caves and
rivers as water continued
to erode the rock.

STALACTITES
Slender stalactites
often hang from
a cave roof. Drops
of water seeping
down from above
dissolve a white
mineral called
calcite from the
rock. As the water
dries, small
amounts of calcite
are left behind.
These build up
to form stalactites.
This process is
usually very slow;
stalactites grow only
about 1 in (2.5 cm)
in 500 years.


STALAGMITES
Water dripping
from the roof or
from a stalactite
falls to the cave
floor, leaving layers
of calcite on the
floor. In this way,
a pillar called a
stalagmite slowly
builds upward.


BENEATH THE SURFACE of Earth lies a secret world. Caves run through the 
rock, opening out into huge chambers decorated with slender stone columns.
Underground rivers wind through deep passages, and waterfalls crash down
on hidden lakes. Caves such as these are many thousands of years old; they were
formed as water slowly dissolved limestone rocks. But not all caves are underground.
Sea cliffs contain caves that have been eroded by the waves. Caves also develop inside
glaciers and within the solidified lava around volcanoes.
Caves are damp, dark places. Some are only large enough
to contain one person; others, such as the network of caves
in Mammoth Cave National Park, in Kentucky, stretch for
hundreds of miles. One of the world’s deepest caves, in
France, lies almost 1 mile (1.5 km) below the ground.
Prehistoric peoples used caves for shelter. Caves at
Lascaux, France, contain wall paintings and ancient
tools that are perhaps 20,000 years old. A few cave
dwellers still live today in parts of Africa and Asia.

SPELUNKING
The sport of exploring caves is called
potholing or spelunking. Clambering
around in caves is a dirty and often
wet pastime, so spelunkers wear tough
clothing. Other important equipment
includes nylon ropes, a helmet with
a light, and ladders made of steel
cables. Spelunkers work in teams and
may stay in a cave for several days.
Spelunking can be dangerous; rain
can cause flooding, and spelunkers
can be trapped by sudden rockfalls.

Spelunkers marvel at the
fascinating rock formations
around an underground lake at
the mouth of a cave in France.

Groundwater
fills a previously
dry cavern to the
level of the water
table, which can rise
and fall over time.

Stalactites and stalagmites take
thousands of years to grow.

Sinkhole—point at which a
stream plunges underground

Sparse vegetation

Stream emerges via cave mouth
and flows along the valley bottom.

Later passage
eroded by
Underground lake stream.

Steep channel
carved by stream.

Water seeps through rock
joints; rock develops cracks,
which widen into potholes.

Ridges and grooves in
the limestone surface Steplike rock
formations

Stream emerges over waterfall.

Craggy limestone cliffs

Water drop
falls from tip
of stalactite.


A stalactite and stalagmite
may grow and meet to
form a column from floor
to roof.

Find out more
Bats
Geology
Prehistoric peoples
Rocks and minerals
Volcanoes
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