Formal reserves
Over 1800 hectares of Bangor is formally protected in perpetual conservation reserves. These areas include some of the most valuable vegetation types such as grassy blue gum (Eucalyptus globulus) and black gum (E. Ovata) forests, the spring and summer home of the swift parrot.
Awards
Tom and Cynthia Dunbabin have been recognised nationally for their environmental management at Bangor. Awards include the 1996 National Landcare Nature Conservation Award and the 2004 McKell Medal for excellence and achievement in natural resource management. These are the most prestigious awards for excellence and achievement in natural resource management in Australia.
Vegetation
Of the 6400 hectare property, over 5000 ha is covered in native vegetation, from dense forests, to more open woodlands and grasslands, as well as coastal vegetation.
Shady gullies are dominated by dense, wet sclerophyll forest, the dominant trees being either stringy barks (Eucalyptus obliqua), blue gums (E. globulus) or black gums (E. ovata). The majority of Bangor's native forest however is drier, more open sclerophyll forest, which depending on aspect, slope and soil type is dominated by eucalypts such as blue gum, white peppermint (E. pulchella), white gum (E. viminalis), brown peppermint (E. amygdalina) and black gum.
Along the sheltered shoreline surrounding Blackman Bay, as well as the swan lagoon wetland, succulent herbs thrive in the saline conditions. The exposed ocean coastline is home to the hardy she-oak (Allocasuarina verticillata), which clings to the rocky cliff-tops and faces.
Geology and landforms
Geological events over millennia have shaped the landscape of Bangor. The majority of the property sits atop rocky dolerite hills and gullies, a common landform across south-eastern Tasmania. The dolerite is most spectacularly evident at Cape Fredrick Hendrick, where the towering cliffs rise 150 metres vertically from the sea.
The low lying Blackman Plains in the east were once part of an ancient seafloor, but now make up some of the most productive and fertile parts of the farm. Over the aeons, wind has moved sand around the landscape, resulting in a mosaic of sandy and heavy clay soils across the plains.
Mudstones and sandstones, formed by the deposition of marine sediments millions of years ago, are also present at Bangor. The fossils of shells and small animals which lived in these shallow seas are evident in the broken rocks.