Monday, November 22, 2010

Beach Five update



Visited beach 5 today and took these photos of the fore-dune. To the West the dune looks alot more stable compared to the view East where the active undercutting is visible. The seaward half of the inter-tidal zone is fluffy with the transported sand. I also counted 6 dead Shearwaters. Also found my 1st Pipi from here with a Natacadea borehole. Usually these predatory snails are out competed by more efficient hunters.

Wednesday, November 17, 2010

What is a Spit?

The geomorhpic definition of Spit is a sandy bar projecting from the mainland into open water. Spits are formed by deposition of sediments moved by longshore drift. (here is a wikipedia link on spits, if you want more details)


So the Big question; Is Point Symthe a Spit?

Well it is widely described as a spit in tourist literature guide books, Often as Victroia's largest spit. However there may be a few problems calling it a true spit
1) The Andersen inlet estuary is no longer "open water" and there is a very strong tidal inflow and outflow cutting across the longshore drift
2) Observations in this project suggest that the longshore drift does change directions and has been larger going southwards for the past few years
3) It doesn't have the characteristic hooked end.

Yet physically it is a very large continuous section of sand and the present situation may represent a very late stage of spit development. Where by the entrance to Andersen inlet may close over with a continous sand bar from Point Symthe to Inverloch.

However as Andersen inlet gradually fills with sediment (not sure if anyone is accurately measuring this) The effects of the tidal flows (it is the same amount of tidal change but in a progressively shallower inlet) mean that there is now considerable erosion cause along the main chanels giving outlet to the sea. These infact are behaving like a meandering streams thrashing back and forth across the inlet floor and heavily eroding the coast & beaches but just at very specific locations (where the chanels curve most).

Who will win? Longshore drift or the tidal flow from Andersen Inlet.

Thursday, October 28, 2010

migration mishap

IMGP6481-1
IMGP6479Now is the time of migration for many of the birds that nest along out coast. The shearwater [Puffinus tenuirostris] (more common knownly as the mutton birds) flies in from as far north as the Siberia, the Aleutian Islands and even the Californian coast. Unfortunately this year something happened and the beaches at Venus Bay are littered by hundreds of dead bird. Stormy weather probably isn’t to blame as most bird appear to have only recently died, a period of mild weather and calm seas and light sea fog. Presumably they died of exhaustion from their trip unable to summon the strength to continue to their nesting sites.

IMGP6480In 1798, Mathew Flinders recorded watching an almost continuous line for several hours of shearwater leaving the waters of northern Tasmanian and heading across bass straight on the start of their migration north.  He estimated that there were at least one hundred million birds within a single flock!

Sunday, October 17, 2010

Beach-Nesting Birds Workshop & Beach Walk

Learn about Birds Australia’s Beach-nesting Birds project and how to safely monitor nesting
birds. All welcome!

Location: Venus Bay Surf Life Saving Club (Surf Drive)

Date: Saturday 6th November
Indoor presentation: 11:00 am -12:00 pm
Break for lunch 12:00 - 1:00pm
[Bring along your lunch; tea/coffee/juice and cake will be provided]

Beach walk*: 1:00pm departing Number one beach (end of Surf Drive), heading east along the beach. We will walk at least 1km and depending on your fitness, there is the option join us on a longer walk.



* For those going on the beach walk, please be prepared for the weather and bring along wet weather gear or sun protection as required. If you have binoculars, please bring these along. You might want to bring along a bottle of water to keep hydrated.