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Kōrero: Rock, limestone and clay

Main sources of aggregate

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Main sources of aggregate

New Zealand is well endowed with high-quality rocks suitable for aggregate. Greywacke and argillite (shown in yellow) are the most widespread, as they form many of the country’s mountain ranges. Rivers eroding these mountains wash down billions of tonnes of sand and gravel onto the plains (in green). Quarries that work these deposits are termed gravel pits as they are simply holes dug into the plains. The word quarry usually refers to places where bedrock is mined, often with explosives. Many New Zealand basalts and andesites, which are volcanic rocks (in red), also make ideal aggregate. These are quarried from hard rock.

Te whakamahi i tēnei tūemi

Te Ara - The Encyclopedia of New Zealand

Source: GNS Science

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Ngā whakaahua me ngā rauemi katoa o tēnei kōrero

Me pēnei te tohu i te whārang

Carl Walrond, Rock, limestone and clay – Aggregate, Te Ara – the Encyclopedia of New Zealand, https://teara.govt.nz/mi/map/5214/main-sources-of-aggregate (accessed 4 June 2026).

He kōrero nā Carl Walrond, i tāngia i te 2 March 2009.