Mackenzie River basins, mostly in Alberta. The cold northern permafrost regions beyond the Arctic Circle are very sparsely populated, mainly by indigenous peoples. Most of the Mackenzie watershed is unbroken wilderness and human activities have little influence on the overall water quality, although there are some localized impacts. Some parts of the Mackenzie basin are rich in natural resources – oil and gas in the Northwest Territories and in central Alberta, lumber in the Peace River headwaters, uranium in Saskatchewan, gold and zinc in the Great Slave Lake area and tungsten in the Yukon. As of 2003 there were two operational gold
Mackenzie River (Queensland) and splits as an anabranch on multiple occasions. The river is joined by twenty-four tributaries including the Isaac and Connors rivers and Funnel Creek. Northeast of Duaringa, the Mackenzie is joined by the Dawson River and together they form the Fitzroy River. From source to mouth, the Mackenzie River descends over its course. The Bingegang Weir near Middlemount contains barramundi, southern saratoga and golden perch. The Bedford Weir and Tartrus Weir are also stocked with barramundi. Bedford Weir is popular with water-skiers and camping is permitted adjacent to the reservoir. The river was discovered by colonial Europeans in 1844 by