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Noosa Spit SEMP Final Report 7
Noosa Spit Shoreline Erosion
Table 2-1 Summary of Noosa River Mouth Channel Position
Imagery Observed Changes Wind Climate Notable Orientation Northern Spit Southern Spit Dominant Flow High Tide High Tide
Date (since previous image) Compared to Average Rainfall and Condition Length and Length and Channel Recreational Recreational
(since previous (since of Mouth Condition Condition Beach Beach
image) previous Availability at Availability at
image) central Doggie eastern
Beach Doggie Beach
July 1982 Paraphrased from Tomlinson and Chamberlain (2006): Double Island Point: Data not N-S Short above Average and Northern, but Limited (fronted Limited (fronted
SE dominant over available HWM, long wide above multiple by shoals) by shoals)
Southern spit and ebb-tidal delta enlarged due to Main Beach nourishment.
preceding years submerged HWM, long channels
Channel in a similar position and shape to previously observed but the entrance
shoals to south submerged through shoals,
has migrated further north due to growth of southern spit and ebb-tidal delta. Tewantin:
shoals to north shoals adjacent
Northern spit eroded as a result of this migration. Northern channel is the Equal NE & SE, less S
to Doggie
dominant flow path but the southern channel may be re-opening. than average
Beach
May 1986 Paraphrased from Tomlinson and Chamberlain (2006): Double Island Point: Data not Shore-parallel Average, Short above Central, but None (fronted None (fronted
SE dominates, more E available west of narrow, HWM, long multiple by shoals) by shoals)
Several interceding years of photography were considered. The southern
Autumn 1983, more N coastline, then submerged submerged channels
channel reopened. A period of vacillation between opening and closing of the
Summer 1984 than N-S shoals to south shoals to north- through shoals,
southern channel occurred while sand was being supplied into the channel from
average west shoals adjacent
Noosa Woods (ocean) beach. While open the channel cut back slightly into
to Doggie
Noosa Woods. At the same time, the northern spit grew and the entrance Tewantin:
Beach
migrated southward. Eventually the southern channel increased in dominance Equal NE & SE, more E
as the major flow path. During this period, the orientation of the entrance in 1983, less S than
changed from north to east and back to north. average
December Paraphrased from Tomlinson and Chamberlain (2006): Double Island Point: Data not Shore-parallel Average, Minimal above Southern – None Wide (infilled
1990 SE dominates, less SE available west of narrow, HWM, average Hard up against shoals)
Several interceding years of photography were considered. The northern
in 1987, less N to NE in coastline, then submerged submerged Doggie Beach
channel breached the northern spit and became the dominant flow path while
Spring 1989 & 1990 NE-SW shoals to south shoals to north-
the material that previously formed the southern spit blocked the southern flow
than average west
path. The southern channel progressively re-established, resulting in both
channels operating simultaneously, sharing a single exit with two well developed Tewantin:
spits. The northern channel was progressively infilling. Equal NE & SE, less N
in 1990 than average
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