Shark Bay is located on the most western point of the coast of Australia.
Shark Bay lies 800km north of Perth, the capitol city of Western Australia.
Shark Bay is of international siginificance, being listed as a World Heritage Site in 1991.
LANDSCAPE The Bay comprises a landscape of north-south facing peninsulas,cliffs and islands which separate inlets and bays from each other and the Indian ocean.
Shark Bay has an area of more than 2 million hectares, with over 1 million hectares protected in marine parks,
marine nature reserves, terrestrial nature reserves and National parks. The Shark Bay region represents a meeting
point of three major climatic regions and forms a transition zone between two major botanical provinces.

Shark Bay is renowned for its marine fauna. The region has one of the largest population of dugong in the
world, at approximately 16,000. This is approx 12.5% of the worlds dugong populations.
The bay was originally named 'Sharks Bay' by the English buccaneer William Dampier in the late 17th
century. The name was given due to the large number of sharks caught by Dampiers fleet whilst fishing. Tiger sharks
(pictured above right) and other smaller shark species are still abundant, especially during the warmer summer months.
Dolphins are abundant, humpback whales use the Bay as a staging post in their
migration along the coast. Killer whales and southern right whales have also been sighted.
Green and loggerhead turtles are found in Shark Bay near their southern limits. The turtles come to nest
on the beaches of Dirk Hartog Island and Peron Peninsula. Dirk Hartog is the most important nesting site for
loggerheads in Western Australia. Six species of sea snake have also been recorded.

Terrestrial fauna is also of great importance in Shark Bay. The area has 5 of the 26 threatened Australian
mammal species. They include the Burrowing bettong, Rufous hare-wallaby, Banded hare-wallaby, Shark Bay mouse and
Western barred bandicoot.
Over 230 bird species have been recorded in the area. The region supports over a 100 recorded species of
Amphibians and reptiles (supporting 9 endemic species). Many species of both bird and herpetofauna are at the
northern or southern limit of their range.


The Mallee Fowl is a large bird, approximately double the size of a domestic chicken. The male builds a
nest or 'mound' to incubate eggs. The mounds are large, using up to 3-5 metres of soil and vegetation. The male
guards the nest and protects the eggs, females play no role in caring for eggs.
Mallee fowls were once widespread through out the Shark Bay area. Feral foxes, cats and clearing of native
vegetation caused populations to decline.
In 1997 and 1998 mallee fowl hatchlings were released into the
park with the hope of re-establishing a long term viable population. Three mounds have recently been sighted in the
park, which confirms that mallee fowl are breeding and new mallee fowl are being produced.
Mallee fowl are part of the successful conservation program known as
, developed
by the Dept. of Environment and Conservation (DEC). Faure Island (located in Shark Bay) is a wildlife sanctuary
that is run by the Australian Wildlife Conservancy.
Mangroves exist only in small, relatively isolated areas in the southern and western areas of the Bay.
Shark Bay has 12 of the 25 species of sea grass that exist in Australia. The most abundant species is Amphibolis
antarctica, covering 90% of the seagrass bed area.
TOWNSHIP The record of
aboriginal occupation of Shark Bay extends to 22,000 years BP. A considerable number of aboriginal midden sites have
been found, especially on Peron Peninsula (pictured right) and Dirk Hartog Island.
Currently Shark Bay has a population of approximately 800, principally located in the towns of Denham
and Useless Loop. The economy of the region includes tourism, fishing, mining (salt mine pictured right) and
pastoralism.
The Stromatilite community in Hamelin Pool, Shark Bay is the most abundant and diverse microbial ecosystem
in the world. The Stromatilites (pictured below right) are microscopic organisms or 'cyanobacteria' that concentrate
and recycle nutrients which combine with sedimentary grains to form towers of rock-like materials. These 'living
fossils' are 2000- 3000 million years old.