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Interactive map

Otago Central Rail Trail interactive map preview image

The map linked below shows the Otago Central Rail Trail route between Clyde and Middlemarch. More information is available for the locations marked by stars.

Interactive map of the Otago Central Rail Trail

The circuitous path of the Taieri river in East Otago


The Taieri river drains only the eastern Otago uplands, and follows an almost circular path from its source to the sea. The Taieri River discharges to the Pacific Ocean at Taieri Mouth, only 60km from its source area in the Lammermoor and Lammerlaw Ranges.

Evaporative salts in Central Otago

salts (7)_thumb

The combination of high temperatures, low rainfall, and wind-driven evaporation has resulted in localised accumulation of evaporative salts in inland parts of Otago, and Central Otago in particular.

Sutton Salt Lake

The salt lake when full. Schist tors surround the lake 226px

The Sutton Salt Lake is the only saline lake in New Zealand, and has formed in a windy cool-temperate maritime climate. Consequently, the lake is distinctly different from most of the world's saline lakes that form in arid continental settings.

Hyde – Eocene quartz gravels

Steeply dipping gold-bearing Hogburn Formation quartz gravels (white, left) faulted against middle Cretaceous Kyeburn Formation (brown, background), Kyeburn valley 226px

On a regional scale, the gold-bearing gravels occur close to the Waipounamu Erosion Surface. The Eocene gravels are immediately below the erosion surface, and rest on the basement unconformity.

Tiroiti – sediments below the Waipounamu Erosion Surface

Blocks of Eocene (40 million years old) Hogburn Formation quartz gravels (top and right) in a bridge of the Otago Central Rail Trail at Tiroiti, north of Hyde 226px

Fluvial (river) sediments immediately beneath the Waipounamu Erosion Surface typically grade upwards into estuarine sediments and then to fully marine sediments at the erosion surface.

Naseby – Alluvial gold recycling

Pliocene gravels at Naseby, dominated by greywacke cobbles and pebbles (greenish brown) 226px

Gold from both Eocene and Miocene gravels has been recycled by erosion during fault-related uplift between Pliocene (2-5 million years ago) and Recent. This recycling process can result in dilution of the gold content by eroded basement material.

North Rough Ridge – Waipounamu Erosion Surface today

Topographic images from across Otago, showing the variations in effects of young (last few million years) deformation on the flat Waipounamu Erosion Surface 226px

The Waipounamu Erosion Surface is now visible in the topography of East and Central Otago as broad areas in which the basement surface is essentially flat, with minor dissection by active rivers and streams

Ida Burn gorge – River drainage redirection

Sketch block diagram of the modified river drainage pattern after diversion of some of the rivers 226px

The intersection of NW- and NE-trending active structures along the Hawkdun Fault Zone in central Otago has resulted in uplift of the synformal (down-folded) basins in the complex structural zone.

Oturehua – Gold-bearing veins at Oturehua

Oturehua Vein map. Veins have a northwest-southeast trend and range in length from ~10m to 750m 226px

There were two principal stages of gold mineralization in the Otago Schist basement: Jurassic-early Cretaceous, as at Macraes, and middle Cretaceous. The vein system at Oturehua is part of the latter group.

Pennyweight Hill – Alluvial gold along the northeast Otago margin, Miocene quartz gravels

Pennyweight Hill historic alluvial gold workings, looking west 226px

The Miocene gravels (Dunstan Formation) in Central Otago rest on the Miocene unconformity which is close to the Waipounamu Erosion Surface.

Fiddlers Flat – Blue Lake Fault Zone, Regional setting

Blue Lake map. The Blue Lake Fault zone, which trends northwest-southeast, seperates Schist from greyacke. Blue Lake is on the north east side of the Fault 226px

The Blue Lake Fault Zone occurs at a major crustal boundary between Otago Schist and Torlesse greywacke, on the northeast margin of the Otago Schist belt.

St Bathans and Blue Lake

The Blue Lake alluvial gold mine, St Bathans, Central Otago 226px

Blue Lake, at the foot of Mt St Bathans in Central Otago, is one of several important historical gold mines in the area. Mt St Bathans is made up of 200 million year old greywacke and that continues deep under the Blue Lake area.

See also DOC page on the history of St Bathans

Patearoa gold: Alluvial concentrations in a dynamic environment

Oblique view of Patearoa area, seen from the north 226px

Patearoa is an historic gold mining area on the southern edge of the Maniototo Basin. The goldfield lies on the northern slopes of the actively rising Rock & Pillar Range, near to the historic Hamiltons Diggings alluvial gold mining area. The gold at Patearoa has been concentrated in gravel deposits (=alluvial gold) that accumulated in alluvial fans on the slopes of the actively rising Rock and Pillar Range.

Hamilton Diggings

Location of Patearoa on the western side of the northeast trending Rock and Pillar ranges 226px

Hamilton's Diggings has some remnants of 40 million year-old quartz gravels, and 20 million year-old quartz gravels occur on the west side of the Maniototo valley. These quartz gravels contain abundant gold, especially where they rest on the schist.

Gold at Alexandra

Oblique view of Tucker Hill from the northwest, with Manuherikia River, rail trail, and town of Alexandra in the foreground 250px

The most prominent feature of the faulted zone in the Raggedy Range is Tucker Hill, between Galloway and Alexandra. This relatively rugged valley wall contrasts strongly with the gentle slopes of the northeastern and central portions of the Raggedy Range.

Gold at Ophir

Manuherikia River gorge downstream of the historic Daniel O'Connell Bridge, Ophir 250px

The southern portion of the Raggedy Range has been made more complicated by the presence of a set of faults at the margin of the valley. The faults are geologically ancient, but some of these faults have acted as weak zones during the present folding of the region.

Poolburn gorge

Oblique view of the Raggedy Range from the northwest, with Manuherikia River in foreground and Poolburn valley in background 250px

The smooth gentle slopes of the Raggedy Range reflect the folded structure of the schist bedrock, and this fold is still developing as the range rises. The rising range has forced the Poolburn to cut a deep gorge through the range, through which the rail trail passes.

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