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The South Maroochy river rises on the
northern slopes of Towen Mountain, a
small range complex that is a spur of
the Blackall Ranges, which form the
western boundary of the subcatchment. It
confluences with the North Maroochy
River near the town of Yandina to form
the estuary. Within the South Maroochy
subcatchment are two of the major dams
within the region, Cooloolabin and Wappa.
The
landform of the headwaters is a small
hill complex of Laterised Tertiary
basalt, grading to low, undulating hills
founded on the same landform that make
up the upper half of the subcatchment.
Throughout the upper subcatchment, the
landform never develops a continuous
alluvial plain of any size as this is
precluded by the steepness of the
terrain through which the river flows.
However, there are small creek lines and
some valley flats near the end of the
upper half, at the boundary of this
particular landform.
The
lower half of the subcatchment consists
of low steep hills formed on Rhyolite
and Andesite. The land form in this area
is similar to that found in the upper
subcatchment, low, steep hills that
prevent the development of alluvial
plains with only small valley flats
being observed.
Once the
river exits these low hills, it is able
to form a short alluvial plain just
prior to its confluence with the North
Maroochy River. This alluvial plain
consists of undifferentiated freshwater
sediment.
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