Weringa County, Queensland

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Rosebury County Queensland. Rosebury County Queensland 6.png
Rosebury County Queensland.

Werenga County Queensland is a cadastral division of Warrego Land District of Southern Queensland and a County of Queensland, Australia.

The county dates from the 8th March 1901, when the Governor of Queensland issued a proclamation legally dividing all of Queensland into counties under the Land Act 1897. [1]

Like all counties in Queensland, it is a non-functional administrative unit, that is used mainly for the purpose of registering land titles. From 30 November 2015, the government no longer referenced counties and parishes in land information systems however the Museum of Lands, Mapping and Surveying retains a record for historical purposes. [2]

The entire County is incorporated lands.

Climate

Carcory Homestead Ruin, from N (2011). Carcory Homestead Ruin, from N (2011).jpg
Carcory Homestead Ruin, from N (2011).

The county has a hot desert climate (BWh in the Köppen climate classification) with an average of only 22 days of rain a year. Summers are extremely hot and dry, with winters being mild to warm. The median annual rainfall for the area is 133 mm (5.2 in) [3] The actual amount of rain which falls is highly variable, for example, in 1914 just 14 mm (0.55 in) was recorded while 659 mm (25.9 in) fell in 1917. Dust storms are most likely during periods of strong wind which typically occur in spring. [3] Birdsville has recorded the highest confirmed temperature in the state of Queensland, with 49.5 °C (121.1 °F) having been recorded on more than one occasion.

Related Research Articles

Desert climate Arid climate subtype in the Köppen climate classification system

The desert climate or arid climate, is a climate in which there is an excess of evaporation over precipitation. The typically bald, rocky, or sandy surfaces in desert climates hold little moisture and evaporate the little rainfall they receive. Covering 14.2% of earth's land area, hot deserts are the second most common type of climate on earth after polar climate.

Climate of Australia Overview of the climate of Australia

Australia's climate is governed mostly by its size and by the hot, sinking air of the subtropical high pressure belt. This moves north-west and north-east with the seasons. The climate is variable, with frequent droughts lasting several seasons, thought to be caused in part by the El Niño-Southern Oscillation. Australia has a wide variety of climates due to its large geographical size. The largest part of Australia is desert or semi-arid. Only the south-east and south-west corners have a temperate climate and moderately fertile soil. The northern part of the country has a tropical climate, varying between grasslands and desert. Australia holds many heat-related records: the continent has the hottest extended region year-round, the areas with the hottest summer climate, and the highest sunshine duration.

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References

  1. A Proclamation". Queensland Government Gazette. 75. 8 March 1901. pp. 969.
  2. "Locality boundaries - Queensland". Department of Natural Resources, Mines and Energy. 27 August 2017. Archived from the original on 31 March 2018. Retrieved 2 October 2018.
  3. 1 2 Hesse, Paul B. (2010). "The Australian desert dunefields: formation and evolution in an old, flat, dry continent". In Bishop, P.; Pillans, B. (eds.). Australian Landscapes . London: Geological Society. p.  145.