Тароона жоғары мектебі: тарихы мен географиясы

The school's most notable former student is Queen Mary of Denmark.

The school is located on the shore of the Derwent River, with a rocky beach. In 2003 Taroona High School underwent a major redevelopment. The school feeder zone covers students in the southern suburbs of Hobart such as Taroona, Dynnyrne and Sandy Bay but students also come from access schools in a wide range of other areas such as West Hobart and Blackmans Bay. B Block is composed of a mixture of general classes as well as art rooms on the top floor, with kitchens for food based courses, general purpose classrooms on the ground floor, as well as Design and Technology workshop facilities and a fully equipped Canteen on the lower ground floor. and two mobile computer labs contained within the science prep room. The link block connecting A and B block was constructed between 1987 and 1988. During the concrete pour for level 1 the formwork collapsed.

Art at Taroona High School includes the International Orange mural (which is blue and white) painted in 2015 by Josh Foley. in 2011 in the Art for Public Buildings Scheme, a work called Chaos Theory was made in sandblasted glass and cut vinyl by Designhaus. The exterior of the building and logo thereon was painted by Dyson Painters using Wattyl Solagard.

Lobbying for a high school south of Hobart to take students from Sandy Bay, Taroona, and the Channel district happened in 1952. The school opened in 1958. Nine students were hurt and hospitalized after an explosion following a reaction of sodium with water on 2 May 1985. On 3 July 1990 two students and a teacher from the school drowned in Mystery Creek Cave near Lune River.

There is a Taroona High School Council, Student Representative Council, Parents and Friends Association, Parents Auxiliary and Old Scholars Association.

Taroona High School is located in Taroona on the shore of the Derwent River. A small sandy beach on the northeast side is called Dixons Beach. A creek runs in a north east direction north of the buildings and main oval, and meets the sea between the car park and the archery field. This is called School Creek. To the south of the school campus is its access road, Meath Avenue and Melinga Place. The rock beneath the school is Paleogene sandstone and conglomerate. A boulder bed formed in the Paleogene makes up the point. A bed of tuff just to the south of A block heads east northeast to the coast and southwest inland. The whole region north from Belhaven Avenue to School Creek is unstable ground undergoing a slow moving landslide called "School Creek Landslide". This started hundreds of years ago before there were any buildings constructed. Movement to the northwest is happening, the tennis court moved about 40 mm in 11 years, and a survey marker near the road entrance has shifted 0.4 m since 1961. Several smaller landslips are parasitic or nearby. These are the Archery Field Landslip, north of the creek; the Dixons Beach Landslip and Carpark Landslip which moved a couple of metres in the late 1980s; and Channel Highway Landslip between the Channel Highway and the primary school. The soil in the area is highly reactive expanding and contracting with changes in water content. The situation is being monitored with a real time inclinometer, and a vibrating wire piezometer, as well as survey markers and a GPS station to see where the school moves.