Geography of Tasmania

Tasmania, the largest island of Australia, has a landmass of and is located directly in the pathway of the notorious "Roaring Forties" wind that encircles the globe. To its north, it is separated from mainland Australia by Bass Strait. Tasmania is the only Australian state that is not located on the Australian mainland. About south of Tasmania island lies the George V Coast of Antarctica. Depending on which borders of the oceans are used, the island can be said to be either surrounded by the Southern Ocean, or to have the Pacific on its east and the Indian to its west. Still other definitions of the ocean boundaries would have Tasmania with the Great Australian Bight to the west, and the Tasman Sea to the east. The southernmost point on mainland Tasmania is approximately at South East Cape, and the northernmost point on mainland Tasmania is approximately in Woolnorth / Temdudheker near Cape Grim / Kennaook. Tasmania lies at similar latitudes to Te Waipounamu / South Island of New Zealand, and parts of Patagonia in South America, and relative to the Northern Hemisphere, it lies at similar latitudes to Hokkaido in Japan, Northeast China (Manchuria), the north Mediterranean in Europe, and the Canada-United States border.

The most mountainous region is the Central Highlands area, which covers most of the central western parts of the state. The Midlands located in the central east, is fairly flat, and is predominantly used for agriculture, although farming activity is scattered throughout the state. Tasmania's tallest mountain is Mount Ossa at . Much of Tasmania is still densely forested, with the Southwest National Park and neighbouring areas holding some of the last temperate rain forests in the Southern Hemisphere. The Tarkine, containing Savage River National Park located in the island's far north west, is the largest temperate rainforest area in Australia covering about . With its rugged topography, Tasmania has a great number of rivers. Several of Tasmania's largest rivers have been dammed at some point to provide hydroelectricity. Many rivers begin in the Central Highlands and flow out to the coast. Tasmania's major population centres are mainly situated around estuaries (some of which are named rivers).

Tasmania is in the shape of a downward-facing triangle, likened to a shield, heart, or face. It consists of the main island as well as at least a thousand neighbouring islands within the state's jurisdiction. The largest of these are Flinders Island in the Furneaux Group of Bass Strait, King Island in the west of Bass Strait, Cape Barren Island south of Flinders Island, Bruny Island separated from Tasmania by the D'Entrecasteaux Channel, Macquarie Island 1,500 km from Tasmania, and Maria Island off the east coast.
Tasmania features a number of separated and continuous mountain ranges. The majority of the state is defined by a significant dolerite exposure, though the western half of the state is older and more rugged, featuring buttongrass plains, temperate rainforests, and quartzite ranges, notably Federation Peak and Frenchmans Cap. The presence of these mountain ranges is a primary factor in the rain shadow effect, where the western half receives the majority of rainfall, which also influences the types of vegetation that can grow. The Central Highlands feature a large plateau which forms a number of ranges and escarpments on its north side, tapering off along the south, and radiating into the highest mountain ranges in the west. At the north-west of this, another plateau radiates into a system of hills where takayna / Tarkine is located.

The Interim Biogeographic Regionalisation for Australia (IBRA) divides Tasmania into 9 bioregions:
Ben Lomond, Furneaux, King, Central Highlands, Northern Midlands, Northern Slopes, Southern Ranges, South East, and West.

Environment

Tasmania's environment consistes of many different biomes or communities across its different regions. It is the most forested state in Australia, and preserves the country's largest areas of temperate rainforest. A distinctive type of moorland found across the west, and particularly south-west of Tasmania, are buttongrass plains, which are speculated to have been expanded by Tasmanian Aboriginal burning practices. Tasmania also features a diverse alpine garden environment, such as cushion plant. Highland areas receive consistent snowfall above ~1,000 metres every year, and due to cold air from Antarctica, this level often reaches 800 m, and more occasionally 600 or 400 metres. Every five or so years, snow can form at sea level. This environment gives rise to the cypress forests of the Central Plateau and mountainous highlands. In particular, the Walls of Jerusalem with large areas of rare pencil pine, and its closest relative King Billy pine. On the West Coast Range and partially on Mount Field, Australia's only winter-deciduous plant, deciduous beech is found, which forms a carpet or krummholz, or very rarely a 4-metre tree.

Tasmania features a high concentration of waterfalls. These can be found in small creeks, alpine streams, rapid rivers, or off precipitous plunges. Some of the tallest waterfalls are found on mountain massifs, sometimes at a 200-metre cascade. The most famous and most visited waterfall in Tasmania is Russell Falls in Mount Field due to its proximity to Hobart and stepped falls at a total height of 58 metres.
Tasmania also has a large number of beaches, the longest of which is Ocean Beach on the West Coast at about 40 kilometres. Wineglass Bay in Freycinet on the east coast is a well-known landmark of the state.

The Tasmanian temperate rainforests cover a few different types. These are also considered distinct from the more common wet sclerophyll forests, though these eucalypt forests often form with rainforest understorey and ferns (such as tree-ferns) are usually never absent. Rainforest found in deep gullies are usually difficult to traverse due to dense understorey growth, such as from horizontal (''Anodopetalum biglandulosum''). Higher-elevation forests (~500 to 800 m) have smaller ground vegetation and are thus easier to walk in. The most common rainforests usually have a 50-metre canopy and are varied by environmental factors. Emergent growth usually comes from eucalyptus, which can tower another 50 metres higher (usually less), providing the most common choice of nesting for giant wedge-tailed eagles.

The human environment ranges from urban or industrial development, to farming or grazing land. The most cultivated area is the Midlands, where it has suitable soil but is also the driest part of the state.

Insularity

Tasmania's insularity was possibly detected by Captain Abel Tasman when he charted Tasmania's coast in 1642. On 5 December, Tasman was following the east coast northward to see how far it went. When the land veered to the north-west at Eddystone Point, he tried to keep in with it but his ships were suddenly hit by the Roaring Forties howling through Bass Strait. Tasman was on a mission to find the Southern Continent, not more islands, so he abruptly turned away to the east and continued his continent-hunting.

The next European to enter the strait was Captain James Cook on HMS ''Endeavour'' in April 1770. However, after sailing for two hours westward into the strait against the wind, he turned back east and noted in his journal that he was "doubtful whether they .e. Van Diemen's Land and New Hollandare one land or no".

The strait was named after George Bass, after he and Matthew Flinders passed through it while circumnavigating Van Diemen's Land in the ''Norfolk'' in 1798–99. At Flinders' recommendation, the Governor of New South Wales, John Hunter, in 1800 named the stretch of water between the mainland and Van Diemen's Land "Bass's Straits". Later it became known as Bass Strait.

The existence of the strait had been suggested in 1797 by the master of Sydney Cove when he reached Sydney after deliberately grounding his foundering ship and being stranded on Preservation Island (at the eastern end of the strait). He reported that the strong south westerly swell and the tides and currents suggested that the island was in a channel linking the Pacific and southern Indian Ocean. Governor Hunter thus wrote to Joseph Banks in August 1797 that it seemed certain a strait existed.

Climate

Tasmania has a relatively cool temperate climate compared to the rest of Australia, spared from the hot summers of the mainland and experiencing four distinct seasons. Summer is from December to February when the average maximum sea temperature is and inland areas around Launceston reach . Other inland areas are much cooler, with Liawenee, located on the Central Plateau, one of the coldest places in Australia, ranging between and in February. Autumn is from March to May, with mostly settled weather, as summer patterns gradually take on the shape of winter patterns. The winter months are from June to August, and are generally the wettest and coldest months in the state, with most high lying areas receiving considerable snowfall. Winter maximums are on average along coastal areas and on the central plateau, as a result of a series of cold fronts from the Southern Ocean. Inland areas receive regular freezes throughout the winter months. Spring is from September to November, and is an unsettled season of transition, where winter weather patterns begin to take the shape of summer patterns, although snowfall is still common up until October. Spring is generally the windiest time of the year with afternoon sea breezes starting to take effect on the coast.

Climate data

Soil

Despite the presence of some Quaternary glaciation, Tasmania's soils are not more fertile than those of mainland Australia, largely because most are severely leached and the areas with driest climates (least leaching) were unaffected by glaciation or alluvia derived therefrom. Most soils on the Bass Strait Islands, the east coast and western Tasmania are very infertile spodosols or psamments

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