If you have a fossil collector, rock hunting, or have an interest in Geology, Fossil Bluff, Tasmania is a must destination. It 'was classified as a geological monument and is surrounded by other geological wonders.
Fossil Bluff is a bluff of sandstone layers of fossils trapped in stone. And 'separate waves of Bass Strait, the ocean, which washed Tasmania from mainland Australia. This reef was below sea level in the Oligocene geological period(Approximately 38 million years ago) and it is on the upper parts of the moraine, which were deposited by glaciers during the Permian (about 280 million years ago). Can bluff around low tide on foot and see where the sand and meet Tillit. Some of the sandstone layers rich in fossils, some do not, however, shows the different climatic conditions that occurred during the Oligocene million. The fossils are not unlike many shells foundcollected on the beaches today.
Unfortunately, they have the right to make copies of fossils from the Bluff.
At low tide you can walk to Fossil Bluff and along the beach, the Silver Gull rookery at the mouth of the Inglis River. Little Penguins, also known as penguins, most of the nests along the coast and from September to February, well known and can find their breeding sites by looking for telltale signs of their excrement. Do not disturb the penguins, since their numberappear to be declining, probably due to the proximity to Wynyard Golf Club, located on the top of the Fossil Bluff. Little Penguins (Eudyptula minor) is the smallest species of penguin, to 43 cm (16 inches) high and is located just off the coast of southern Australia and New Zealand
West of Fossil Bluff, Cape table is a circular plug of volcanic origin with a slope rising to 170 meters north (560 feet) above sea level. The volcanic soil of the Cape is home to a variety of crops andconsidered the richest agricultural land in Tasmania. The basalt is about 13.3 million years old, which is geologically recent.
To the east and west of the beach and at regular intervals for many miles to the east is a flat gray stone. This is the Tillit Wynyard, about 280 million years, which originated in the Permian geological period. It was formed in the era of ice ages, while Australia was part of the super-continent called Gondwana. The glaciers flowed fromSouth to north, and when melted, reaching areas of depression, slowed down and let the stones wore. Over time, the mud covered rocks, which was a mudstone conglomerate. You can find (and hold) granite, flint, quartz, jasper and agates in the moraine and on the beach, like pebbles.
Fossil Bluff is just 3 km (2 miles) from the town of Wynyard, Tasmania. It is formed on the tip of the tongue of the Inglis River, where they metBass Strait. Wynyard based on a direct flight from Melbourne or 40 minutes by car from the terminus for the ferry Spirit of Tasmania from Melbourne to Devonport. Bus services available from Redline Wynyard Hobart / Launceston / Devonport.
The main road in Wynyard has all the facilities ... Restaurants, bars, pharmacy, fresh fish at Wynyard Wharf, supermarket, butchers, post office and store magazine with a variety of shops to browse through the Online Access Centres in the local library and alsoWonders of Wynyard Information Centre.
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