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                                                                    History of Yungaburra

Yungaburra takes it's name from the Yidinyji language, meaning a place of enquiring or questioning. The European settlement of Yungaburra spans from the early 1880s, but the history goes back much further.

Take the "Old Town Loop" walk around the historic buildings of Yungaburra. There are many excellent books researched and published by the Eacham Historical Society that detail the history of Yungaburra and the Atherton Tablelands, and give insight into the lives of the pioneers who settled here (see the web address at the bottom of this page).

A Volcanic Start A Short History of Yungaburra

The First Inhabitants

The geological history of the area stretches back 420 million years ago, when the Atherton Tableland was a deep ocean basin.

About 360 million years ago the region changed with sediments squeezed upwards forming high mountain ranges. About 260 million years ago violent eruptions and magma caused further changes in the landscape.

About 7 million years ago, vast amount of lava flowed form a number of shield volcanoes, spreading over the landscape and cooling to form a dense layer of basalt.

Volcanic activity has been intermittent on the tableland for the past 3 million years, with the most recent eruptions being perhaps as recent as 10,000 years ago or so.

Timber Cutter
Timber Cutter

Geological Features near Yungaburra:

Seven Sisters and Mt Quincan: Volcanic cones created by explosive eruptions. As air vents opened, volcanic ash and scoria (light weight volcanic rocks with gas bubbles) hurled into the air, falling to build up cones around them.

Lakes Eacham and Barrine:
Explosive craters known as maars are created when rising lava came in contact with the water basin. The resulting steam cause a violent explosion , producing a crater. The craters have filled with rainwater. Where the water is able to drain off, a swamp rather than a lake forms. (Bromfield Swamp). The craters of Eacham and Barrine are thought to have been formed as recently as 10,000 years ago.

MT Hypipamee Crater:
Known as a diatreme, this crater is thought to have been created by a massive gas explosion, causing a deep cylindrical pipe through the granite approximately 142m deep.


MT Hypipamee Crater

Yungaburra was originally called Allumbah Pocket. The district was developed in the early 1880's as an overnight stop for miners and settlers who came from the coast on their way to the tin and gold fields farther west. Shanties grew up along the pack tracks at Boar Pocket (near Lake Barrine) and Ball Pocket (later the township of Kulara which was flooded with the construction of Tinaroo Dam).

In 1886 the land around Allumbah Pocket and Lake Eacham was surveyed for settlement. In 1891 the settlers moved in. The 40 acre blocks were a mixture of scrub and open forest. Those who selected jungle-covered blocks had to clear them by felling the trees and then burning off. Homes were built of timber slabs, with roofs of bark or wooden shingles; beds were sackbag stretchers and cooking was done over open fires. The highest priority was to provide food. Maize, pumpkins, sweet potatoes and other vegetables flourished in the newly cultivated soil but crops had to be protected from wildlife. A pioneer saying was " the soil was so good that when you planted corn it would come up overnight - it did too, for the bandicoots would bring it up". Eventually grass was sown and a few cows introduced to provide milk, butter and beef. Often it was the women and children who remained alone on their blocks of land while the men took casual employment elsewhere to provide money for basic necessities of living.

A small commercial area was developing in Allumbah to serve the new settlers. 1910 was a very significant year for our town. The railway line linking Cairns with the Tablelands reached Allumbah, which was then renamed Yungaburra to avoid confusion with another town. The new railway station caused a geographic shift in focus from the original settlement, which was located towards the north west of the new commercial centre. Buildings were constructed or relocated near the railway. A period of rapid development then began with the construction of a sawmill, a hotel and a number of shops and houses near the railway station. Three churches and the Bank of NSW were built, the school was moved to the present site and a Police Station was established.

Yungaburra remains largely unchanged since those early days.

For more information please contact:
Eacham Historical Society
PO Box 533   Qld    4885
email: eachist@qldnet.com.au
web: users.qldnet.com.au/~eachist

Reference Book: 'The Pioneers Speak' by Mary Allen, compilation of photographs, quotes and information for the Yungaburra District Centenary, 1890 to 1990.

Before non-indigenous settlement, the Wet Tropics rainforests were populated with approximately 16 different tribal groups of Aboriginal people.

They were small in stature with slender limbs. The forests were able to provide a rich diet of plants, nuts and fruit, supplemented with eels, wallabies, tree-kangaroos, possums, fish, birds and turkey eggs. Some unique cultural elements that reflect features of the rainforest habitat are dome-shaped, rain proof thatched huts that were used as semi-permanent wet- season camps.

Train at Yungaburra Station
Train at Yungaburra Station

Pathways through the rainforest to pockets of cleared areas provided the routes of travel and trade that formed the basis of their social system. The cleared areas were thought to have been maintained by fire, and the grassy areas providing food for the wallabies, part of their diet.

At the onset of white settlement, the system of tracks through the rainforest were used by travelers, with the grassy pockets providing fodder for the wagon teams.

A Ngadjon story of the origin of the three volcanic crater lakes Yidyam (Lake Eacham), Barany (Lake Barrine) and Ngimun (Lake Euramo) fits well with studies that show the rainforests around the craters are about 7,600 years old. "Two newly-initiated men broke a taboo and angered the rainbow serpent, major spirit of the area. As a result the camping-place began to change, the earth under the camp roaring like thunder. The wind started to blow down, as if a cyclone were coming. The camping-place began to twist and crack. While this was happening there was in the sky a red cloud, of a hue never seen before. The people tried to run from side to side but were swallowed by a crack which opened in the ground....'

As the settlements increased, the rainforest people were forced to retreat to the inaccessible areas they lost the use of their full range of habitats. Tribes were probably reduced to less than 20% of their pre-contact numbers within 20 years from European diseases and conflicts with settlers.

For a more detailed look at the Ngadjonji Tribe who traditionally occupied an area of upland rainforest country at the headwaters of the Russell and North Johnstone Rivers in north east Queensland, please visit this web site.


 

 

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