Monaro (New South Wales)
Monaro is a high, mostly treeless plateau region in southern New South Wales, Australia, noted for its cool climate, grazing country, distinctive soils and close links with Canberra and the ACT.
Overview
The Monaro is a broad highland area in the south of New South Wales in Australia, extending a short distance into Victoria. It lies near the Snowy River National Park and is commonly associated with the neighbouring Australian Capital Territory. Many towns on the Monaro have close economic and social connections with Canberra. The region is often described by its wide, undulating plains and comparatively sparse tree cover compared with surrounding high country.
Image gallery
1 ImageLandscape and natural features
The Monaro occupies a high plateau or tableland that stands at roughly 1,000 m above sea level (about 3,281 ft). It is bounded to the north by the valleys of the Murrumbidgee River and falls away more steeply towards the eastern coastal ranges. Parts of the region are gently undulating, while other sectors rise into more rugged country, such as the Tinderry Mountains. Between the main river systems the basalt-capped Monaro Range separates the Snowy and Murrumbidgee catchments.
Soils, vegetation and land use
Soil types on the Monaro are variable. Localised basaltic areas around centres such as Cooma and Nimmitabel produce deep, dark fertile soils— regarded as among the best in Australia—while much of the plateau rests on ancient granitic materials that yield thin, relatively infertile soils. Before European settlement the land supported dry forest and native grasslands; since then extensive clearing has converted much of the area to pasture. Because of the cool climate and soil distribution the dominant agricultural enterprises are grazing, notably sheep and beef cattle, rather than intensive cropping.
Climate
Situated to the east of the Snowy Mountains, the Monaro lies in a rain-shadow zone created when westerly systems deposit most moisture on the alpine slopes. Annual precipitation typically ranges from about 430 mm (around 17 in) in the western and southern parts to roughly 700 mm at the eastern escarpment, though occasional storms can deliver much larger short-term totals—one recorded event at Nimmitabel produced 256 mm in a single day. Summers are warm to warm–hot with average maxima near 28 °C (about 82 °F) in lower-lying areas; nights remain cool. Winters are noticeably cold for mainland Australia outside the alpine zone, and frosts are common.
Settlements, transport and economy
The region's principal towns include Cooma and Bombala, with other communities such as Berridale, Adaminaby, Delegate, Dalgety, Nimmitabel and Jindabyne serving local farming and tourism needs. The Monaro Highway provides the main road link to Canberra and to southern destinations. Economic activity centres on pastoralism, service towns that supply the rural hinterland, and tourism linked to nearby alpine and river national parks. Proximity to the national capital gives additional employment and market opportunities for residents.
History, name and significance
The name "Monaro" is commonly thought to derive from an Aboriginal word meaning a plain or high plain, reflecting the region's sweeping, open character. The plateau has long been used for grazing and has a colonial history tied to early overland routes and later road improvements that connected southern New South Wales with coastal and alpine districts. Today the Monaro is valued for its distinctive landscapes, rural communities and the way it forms a transitional zone between the high alpine country and lower coastal environments.
- Regional links: New South Wales, Australia, Australian Capital Territory.
- Key physical features: plateau, Murrumbidgee River, Snowy River National Park.
- Representative data points: elevation ~1,000 m (3,281 ft), rainfall ~430 mm to 700 mm (17 in), summer maxima near 28 °C (82 °F).
- Towns and transport: major town Cooma, others include Jindabyne and Canberra-linked centres; Monaro Highway provides the main route.
- Drainage and ranges: Monaro Range separates Snowy and Murrumbidgee catchments; the area is in a rain-shadow.
For further reading on local geology, climate and rural industries see specialist sources and regional guides that focus on the Monaro's unique combination of elevation, soils and pastoral history.
Questions and answers
Q: What is the Monaro region?
A: The Monaro region is a large plateau located in the south of New South Wales, Australia. It also includes a small area of Victoria near Snowy River National Park and the Australian Capital Territory is often considered part of the region.
Q: What type of soils are found in the Monaro region?
A: The Monaro region has both granitic soils which are very infertile, as well as chernozems which are some of the best soils in all of Australia, found near Cooma and Nimmitabel.
Q: How much rainfall does the Monaro region get on average?
A: Annual rainfall ranges from 430 mm (17 in) around Dalgety to 700 mm (28 in) at the eastern edge of the plateau. Occasional storms can produce very heavy rainfall.
Q: What type of vegetation was supported by these soils before clearing for farming?
A: Before clearing for farming, dry forest vegetation was supported by these soils.
Q: What is the main industry in this region?
A: Because the climate in basaltic areas is too cold for crops, raising sheep and beef cattle is currently the main industry in this region.
Q: What are some towns located within this region?
A: Some towns located within this region include Cooma, Bombala, Berridale, Adaminaby, Delegate, Dalgety, Nimmitabel and Jindabyne.
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Author
AlegsaOnline.com Monaro (New South Wales) Leandro Alegsa
URL: https://en.alegsaonline.com/art/65958