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Wineglass bay Red mountains and crescent bays of Freycinet Peninsula, Tasmania
Geographic formation of wineglass bay (Tasmanian geographic)
//The balancing force to winter’s westerly winds and waves in south-east Tasmania are the summer sea breezes. They are reliable as clockwork in coming ashore early each summer’s afternoon. As they form five to ten kilometres off-shore they have sufficient fetch to allow small to medium waves to be generated. Sea breezes typically make their land-fall at right angles to the shoreline – so around the south-east coastline they are typically blowing in from an easterly direction. This fortuitous combination of two opposing wind and wave directions has resulted in one of the ideal conditions for isthmus formation to be met.//
Geology and landform:
Honey moon bay
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Hobart central YHA
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