Geilston Bay High School

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Geilston Bay High School
Location
Geilston Bay High School

Australia
Coordinates 42°50′15″S147°20′56″E / 42.8376°S 147.3488°E / -42.8376; 147.3488
Information
Type Government comprehensive secondary school
Established9 February 1972 (1972-02-09)
StatusClosed
Closed9 December 2013 (2013-12-09)
School districtSouthern
Educational authority Tasmanian Department of Education
OversightOffice of Tasmanian Assessment, Standards & Certification
Years 7-10
Gender Co-educational
Campus type Suburban
Colour(s)Gold and brown   
Geilston Bay High School

Geilston Bay High School was a government co-educational comprehensive secondary school located in Geilston Bay, a suburb of Hobart, Tasmania, Australia. Established in 1972, the school catered for students from Years 7 to 10 until its closure in 2013.

Contents

Overview

Along with Clarence High School, Rokeby High School, and Rose Bay High School, Geilston Bay High School was one of four government high schools within Clarence. The school emblem was the Eucalyptus risdonii , a local eucalyptus variety with bluish-silver leaves that is found only within the City of Clarence.

History

Construction of the school began in 1971 on the site of the old Lindisfarne Golf Course. The first phase of construction was completed on 1 July 1971.

Geilston Bay High School was opened on 9 February 1972 as the then Municipality of Clarence was enjoying a boom in residential expansion. The opening of the Hobart Bridge (1943), and later the Tasman Bridge (1964) saw a dramatic expansion of residential areas within Clarence. However, prior to the Tasman Bridge disaster in 1975, there were few facilities located on the eastern shore of the Derwent River. The severing of the bridge made local authorities realise the need for localised services in areas of commerce, health care and education.

Geilston Bay High School was the most recently opened high school within the City of Clarence, after Warrane High (1957), Clarence High (1959), and Rose Bay High (1961).

In 2007 Geilston Bay High School celebrated its 35th anniversary.

Geilston Bay High School closed on 19 December 2013. Low enrolment numbers was cited as the reason. [1]

Towards the head of the Bay, the (former) school playing fields cover what was once the Geilston Bay fossil site, which yielded fossil plants and animal bones in the nineteenth century of Late Oligocene (or possible early Miocene) age, including mammals that at one time were the earliest known from Australia. [2]

See also

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The Geilston Bay fossil site is a paleontological site of Late Oligocene age in south-eastern Tasmania, Australia. It lies within the suburb of Geilston Bay which, although it is a part of the municipality (city) of Clarence, is effectively a suburb of Hobart located on the eastern shore of the River Derwent. The Geilston Bay site is important as one of the few of its age to yield fossils of mammals from the Late Paleogene Period ; at the time of their redescription in 1975, the mammal (marsupial) fossils were considered the earliest then known from Australia, although that distinction has since been surrendered to fossils from the Murgon fossil site in south-east Queensland, whose fauna—known as the Tingamarra Fauna—is of Early Eocene age. In addition to the somewhat fragmentary mammal bones still in existence, a range of plant macrofossils have also been described from the site, which appear not to have survived. The limestone deposit in which the fossils occurred was extensively mined for the production of lime in the nineteenth and early twentieth centuries, and its location, while still publicly accessible, now lies buried beneath landfill under the playing fields of the former Geilston Bay High School.

References

  1. Paine, Michelle. "Geilston Bay High School to close at end of term". The Mercury . Hobart, Tasmania. Retrieved 6 January 2014.
  2. Tedford, R.H.; Banks, M.R.; Kemp, N.R.; McDougall, I.; Sutherland, F.L. (1975). "Recognition of the oldest known fossil marsupials from Australia". Nature. 255(5504) (5504): 141–142. doi:10.1038/255141a0. S2CID   4195697.