NA ="Kingston, Tinderbox, Howden, Margate,  Snug, Oyster Cove, Kettering, Woodbridge";
FE1[0]=" The D'Entrecasteaux Channel with its sheltered coves and bays make it a favourite haunt of boating enthusiasts and recreational fishermen and wineries that offer wonderful views and cool climate wines. A vehicular ferry departs fr";
FE2[0]="om Kettering for the northern end of Bruny Island, which has its own winery. Take the vehicular ferry from Kettering and walk or drive to the island's beautiful nooks and crannies.  Named Lunawannaalonna by Tasmanian Aborigines, C";
FE3[0]="aptain James Cook first visited the island in 1777, landing at Adventure Bay and tying his vessel to a tree - still standing - and named in his honour. The Huon-Channel-Bruny region is best explored by following one of Australia's";
FE4[0]=" finest coastal touring routes, the Huon Trail. From Hobart, the Trail runs south along the banks of the River Derwent, the D'Entrecasteaux Channel and the Huon River, offering dazzling water views for the best part of 160 kilomet";
FE5[0]="res. With the Trail being a loop route, you have the option of returning to Hobart 'the short way', via Mount Wellington's foothills, with their big-picture outlook over the entire Huon-Channel-Bruny region. There are eight wineri";
FE6[0]="es in the Northern part mostly near Tinderbox and Kettering areas. Perhaps the most famous is Herons Rise Vineyard overlooking the D'Entrecasteaux Channel and Bruny Island. This winery has been producing fine wines for about ten y";
FE7[0]="ears. Gerry and Sue White run this one-hectare vineyard at Kettering, growing pinot noir and muller thurgau, sold as dry white. The wines, made by Andrew Hood, are very good and there is high quality accommodation at the vineyard.";
FE8[0]=" Overlooking the boating harbour of Kettering, the one and two bedroom Cottages are the perfect place for the ultimate Tasmanian food and wine experience, just a 30-minute drive from Hobart. The area was first explored by Bruni D'";
FE9[0]="Entrecasteaux in 1792 and was settled in the early 1800s by timber cutters, whalers and sealers.";
LA1[0]=" The geology of the North West Bay River catchment and other catchments in the Kingborough Municipal Area draining into the west coast of the D'Entrecasteaux Channel is predominantly dolerite and sedimentary rock types with small a";
LA2[0]="reas of rock types belonging to the alkaline intrusion group located on the western edge of the catchment inland from Kettering. The Channel is, geologically, an offshoot of the Derwent Valley. The coastline is highly indented and";
LA3[0]=" consists predominantly of Jurassic dolerite or commonly cliffed Permian and Triassic sediments. The gross form of the Channel and the surrounding landscape probably developed around 60 million years ago, during the final break up";
LA4[0]=" of the super continent Gondwana. Associated tension in the earths crust resulted in widescale block faulting, some blocks (Mt Wellington) were forced up and others (the Derwent Valley and the Channel) were forced down. Up until a";
LA5[0]="bout 20 or 30 million years ago the climate was warm and wet and river action further developed the Derwent and Huon Valley's and parts of the Channel. Higher sea levels during this time probably inundated parts of the Channel. Ov";
LA6[0]="er the last two million years the floor of the Channel and the Derwent Estuary have probably been exposed on five or six occasions. The Derwent was the largest River flowing across extensive floodplains and into the ocean south of";
LA7[0]=" Storm Bay while the Huon entered the ocean south of Bruny Island. In the Channel area lower sea levels would have exposed broad undulating plains between Bruny Island and the Tasmanian mainland. Rising sea levels up until 6000 ye";
LA8[0]="ars ago would have drowned the Channel 'valley' and, again, isolated Bruny Island.";
LA9[0]="";
CL1[0]=" The climate is similar to Hobart, which lying on latitude 43 degrees South, is no further from the equator than New York or Madrid and has a milder climate than these cities. The Climate is described as Temperate maritime. The dai";
CL2[0]="ly average maximum temperatures in Hobart are 12 degrees C in winter and 21.5 in summer. Hobart gets about 630mm (25 inches) of rain a year, making it Australia's second driest capital city. Average wind strength is 11.3 km/hr. Br";
CL3[0]="ight sunshine ranges from an average of 2500 hours per year in the northern Midlands to less than 1750 hours per year on the west coast and western highlands. Hobart receives an average of 2100 hours annually and Launceston around";
CL4[0]=" 2400 hours. The regions around Hobart are coldest and the challenge here is to grow grapes out of the wind. On the banks of the Huon River it is especially cold. The maritime influence and hence aspect and exposure to the sea or ";
CL5[0]="water is second in importance only to the sunshine hours provided in the long autumn. This is not true in all subregions; the Coal River and the upper Derwent Valley are subject to minimal maritime effects. The climate summaries f";
CL6[0]="or the northern part of D'Entrecasteaux Channel show that rainfall is very evenly distributed throughout the year with a slight peak in October. Frosts are infrequent and average maximum and minimum temperatures are lowest in July";
CL7[0]=" (12 and 2 degrees C) and highest in January (21 and 11 degrees C). The mean number of clear days is highest in the ripening period of January to April, and lowest in Spring (September to November).";
CL8[0]="";
CL9[0]="";
HI1[0]=" The D'Entrecasteaux Channel is an area rich in the history. The French explorer, Bruni D'Entrecasteaux, was the first European to discover the channel separating Bruny Is. from the mainland. In 1792 D'Entrecasteaux's expedition sa";
HI2[0]="iled up the channel, charting the coastline& naming features. He named the large bay at the top of the Channel North West Bay. The expedition anchored there to collect fresh water. Many aborigines were observed in the area. It was";
HI3[0]=" not until the opening of the road to Hobart Town, known as Proctor's Road, in 1835, that great impetus was given to the area. In 1830 a Mr Proctor who owned a farm at Brown's River decided to construct a road between Hobart Town ";
HI4[0]="and his property at Brown's River. It took Proctor five long years to complete it.  Ironically, soon after Proctor's Road was finished the Government, having refused to provide any financial assistance to Mr Proctor, declared the ";
HI5[0]="road a public thoroughfare. Kingston developed into a holiday village, a weekend and summer holiday retreat. A number of the early holiday dwellings still exist at Kingston Beach and in the older part of Blackmans Bay. The surroun";
HI6[0]="ding rural area concentrated on timber felling, fishing, fruit production and dairying. The small rivers and streams flowing eastward from the Wellington Ranges, Snug Tiers and Woodbridge Hills provided small pockets of fertile al";
HI7[0]="luvial soils and at the mouths of these streams were reasonable anchorages for small boats. The settlements at the mouths of these locations - Kingston, Margate, Snug, Kettering and Woodbridge, took advantage of their location. Sm";
HI8[0]="all fishing fleets operated out of the settlements exploiting the D'Entrecasteaux Channel fishing grounds and small local timber mills were established. With the clearing of land for timber production, agriculture became establish";
HI9[0]="ed on the lower and flatter land around each of the settlements. Early crops were orchard and stone fruits and berry fruits, and pasture for dairy and meat production. Recently several wineries have established in the area.";