Risky night run along
the coast
Comment on chart
The chart shows a night time run
parallel to the coast under 'thick squalls'. Note the direction of the
wind (south-west), tending to push the ship towards the coast. Had a
major headland or rock suddenly appeared before the ship, the Investigator
would have had limited ability to manoeuvre under conditions at that
time.
Parts of the
coast are missing from the chart; the Captain had more important
things to do at this time than run his usual survey! (As well,
visibility was poor on this night). As time was running short to reach
Sydney, Flinders did not have the option of moving out to sea at night,
and waiting for morning to recommence the survey, as he was accustomed
to doing when time permitted. |
Port Campbell Coast, chart

Extract from Flinders' chart (South
Coast, Sheet IV)
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Sailing conditions were
poor for the crew of the Investigator; there was little visibility and a
southerly gale. Heavy rain and swell made this part of the expedition
risky. Glimpses were gained during the night of the dangerous cliffs
passing by as the ship headed southeast.
The
Twelve Apostles, and other features of the coast near the sheltered
inlet of Port Campbell, are famous and rugged landforms carved by the sea from the
limestone cliffs of SW Victoria. Originally the rock layers formed as
horizontal beds of calcite-rich sediment on the sea floor. This
rock is thus called sedimentary. Much originated from shells that
had accumulated on the sea
floor. |
'A bold projection ... Head seen
...
in a moonlight interval
of thick
squalls.'
- from Matthew Flinders' chart 
Photo 1: Twelve Apostles
Coastline, Victoria
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The cliffs of Loch Ard Gorge and the entire
coastline of this area are composed mainly of
horizontally bedded limestone, deposited when the area was under sea
millions of years ago. More recently the rock was gently uplifted and
exposed to marine erosion. There are few safe ways to approach the
land from the sea, and offshore reefs can be dangerous.
A
large range of erosional coastal features is found here, including
gorges, sea arches, island stacks, natural bridges, and blowholes. |
Loch Ard Gorge

Photo 2: Loch
Ard Gorge
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The Loch Ard Gorge contains a number of
sea caves
and overhanging areas at seal level (between tide lavels and a little above high tide
level). They have formed in the rock as a result of marine action at the
cliff base.
Consider the difficulty of
overnight survival here after a shipwreck. Perhaps a cave back from the shoreline could offer some
protection. To walk for help in daylight, it would be necessary to safely
climb the cliffs; at some beaches along the coastline this would not be
possible.
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Sea cave

Photo 3:
Features of Loch Ard Gorge
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Waves, and constant wetting and
drying of salt spray,
attack the rock, disrupting it both physically and chemically. Landform change is brought about through the
accumulation of these forces acting over time; the hydraulic pressure of
the water striking the rock face, assisted by abrasive force
of particles carried by waves, and the chemical weakening of the rock. It is
believed that in landform terms, the cliff faces here are being eaten away
relatively rapidly.
In places marine erosion is from
several different directions, causing islands to be carved from retreating
cliff faces. Vertical
columns remaining from these erosive processes (such as the Twelve Apostles) are called
stacks. An island can be further attacked, forming a sea arch (Island Archway,
as
shown) or a bridge.
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Sea
arch

Photo 4: Island Archway

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