Lindsay Creek
Encyclopedia
The Lindsay Creek is a tributary of the Water of Leith
which runs through the northern suburbs of Dunedin
, New Zealand
. The Māori
name for the creek, now rarely used, is Puke-haukea.
The creek has its origins on the southern slopes of Mount Cargill
about 1 kilometre southwest of the summit, and flows south, passing through the popular recreation reserve of Bethunes Gully before reaching Dunedin's suburban area at Normanby. It continues south-southwest, its thalweg
running through North East Valley
, passing through Chingford Park
and along the foot of the Valley's Quarry Gardens before reaching the coastal plain of the Leith at The Gardens Corner. From here, it flows into Dunedin Botanic Gardens
where it joins the Water of Leith.
Several measures are underway to widen the channel of the creek at various points, in an attempt to provide more protection against floods. The creek has flooded on numerous occasions, most significantly in the Leith Flood of 1929 and in 1955, when it led to the inundation of many properties in North East Valley. Protection works have been built over the years, most notably realignment and walling of the channel in the lower part of North East Valley after the 1929 flood and further work on the same area in 1965. Further walling of the channel in the central part of North East Valley was undertaken during the 1970s.
Water of Leith, New Zealand
The Water of Leith , is a small river in the South Island of New Zealand.It rises to the north of the city of Dunedin, flowing for 14 kilometres southeast through the northern part of the city and the campus of the University of Otago before reaching the Otago Harbour...
which runs through the northern suburbs of Dunedin
Dunedin
Dunedin is the second-largest city in the South Island of New Zealand, and the principal city of the Otago Region. It is considered to be one of the four main urban centres of New Zealand for historic, cultural, and geographic reasons. Dunedin was the largest city by territorial land area until...
, New Zealand
New Zealand
New Zealand is an island country in the south-western Pacific Ocean comprising two main landmasses and numerous smaller islands. The country is situated some east of Australia across the Tasman Sea, and roughly south of the Pacific island nations of New Caledonia, Fiji, and Tonga...
. The Māori
Maori language
Māori or te reo Māori , commonly te reo , is the language of the indigenous population of New Zealand, the Māori. It has the status of an official language in New Zealand...
name for the creek, now rarely used, is Puke-haukea.
The creek has its origins on the southern slopes of Mount Cargill
Mount Cargill
Mount Cargill is a 680 metre high volcanic outcrop which dominates the skyline of northern Dunedin, New Zealand. It is situated some 15 kilometres north of the city centre....
about 1 kilometre southwest of the summit, and flows south, passing through the popular recreation reserve of Bethunes Gully before reaching Dunedin's suburban area at Normanby. It continues south-southwest, its thalweg
Thalweg
Thalweg in geography and fluvial geomorphology signifies the deepest continuous inline within a valley or watercourse system.-Hydrology:In hydrological and fluvial landforms, the thalweg is a line drawn to join the lowest points along the entire length of a stream bed or valley in its downward...
running through North East Valley
North East Valley
North East Valley is a suburb of the New Zealand city of Dunedin.-Geography and demographics:...
, passing through Chingford Park
Chingford Stables
The Chingford Stables are located in North East Valley, Dunedin, New Zealand. The stables are now used for both private and public functions, and listed as a Category I Historic Place.-History:...
and along the foot of the Valley's Quarry Gardens before reaching the coastal plain of the Leith at The Gardens Corner. From here, it flows into Dunedin Botanic Gardens
Dunedin Botanic Gardens
The Dunedin Botanical Gardens are located at the northern end of central Dunedin, in the South Island of New Zealand. They are located close to the University of Otago and one of the city's most historic cemeteries, the Northern Cemetery, on a spur of Signal Hill and on the river plain immediately...
where it joins the Water of Leith.
Several measures are underway to widen the channel of the creek at various points, in an attempt to provide more protection against floods. The creek has flooded on numerous occasions, most significantly in the Leith Flood of 1929 and in 1955, when it led to the inundation of many properties in North East Valley. Protection works have been built over the years, most notably realignment and walling of the channel in the lower part of North East Valley after the 1929 flood and further work on the same area in 1965. Further walling of the channel in the central part of North East Valley was undertaken during the 1970s.