Клэрэнс өзені: Жаңа Оңтүстік Уэльс, Австралия

River in New South Wales, Australia
The Clarence River (Bundjalung: Boorimbah,) is a river situated in the Northern Rivers district of New South Wales, Australia. It rises on the eastern slopes of the Great Dividing Range, in the Border Ranges west of Bonalbo, near Rivertree at the junction of Koreelah Creek and Maryland River, on the watershed that marks the border between New South Wales and Queensland. It flows generally south, south east and north east, and is joined by twenty four tributaries including Tooloom Creek and the Mann, Nymboida, Cataract, Orara, Coldstream, Timbarra, and Esk rivers. It descends over the course of its length and empties into the Coral Sea in the South Pacific Ocean, between Iluka and Yamba.

The climate of most of the basin is subtropical (Köppen Cfa), though the highest areas with cooler weather are of the temperate Cfb type. Annual rainfall ranges from on the coast at Yamba down to in the shielded valley at Grafton (BOM Grafton Olympic Pool). At higher altitudes, rainfall may reach on exposed slopes but data are very poor. Most of the high areas actually receive no more rain than Grafton though variability from year to year is less. Temperatures are generally very warm, with maxima in lower area ranging from 27 °C (81 °F) in January to 19 °C (66 °F) in July. In the highlands, however, temperatures are much cooler and in July range from lows of around 2 °C (36 °F) to maxima around 13 °C (55 °F) though in January days remain very warm at around 25 °C (77 °F). Rainfall per month on the coast typically ranges from around in February and March to around in September; it can average as low as between May and September inland, where exposed areas sometimes suffer bushfires after droughts, as occurred in 1915 and 2000.

During Cyclone Oswald, the Clarence was subject to minor flooding, brought about due to the storm's residual effects and associated monsoon trough that passed over parts of Queensland and New South Wales. At Grafton, the river peaked at a new record height of Two years earlier, the river peaked , forcing the evacuation of 3000 people from their homes. On both occasions, the city's levee was credited with preventing more severe flooding. The local historical society has published an account of newspaper reports documenting flooding of the river from the late 1800s to 2011.

Tourism is also a significant industry in the Clarence Valley generating around A$457million per annum and employing around 2500 people. Most of the Clarence basin is heavily forested, with important areas of remnant subtropical and temperate rainforest occurring all along the course. Only in alluvial areas where soils are less leached is there major agricultural development: in these areas the chief industries are cattle rearing and the growing of sugar cane in lower lying areas. Of particular interest is the small island town of Harwood, where a Sperry New Holland factory and a quaint Bush Pub overlook the Clarence delta. Harwood is also the location of the local sugar mill, the Harwood Sugar Mill built in 1873 and is the oldest Australian mill still operational. The sugar mill is situated on the river due to its importance in transporting sugar cane from farms in the surrounding area in previous times. Harwood is just after the Harwood Bridge on part of Australia's National Highway from Sydney, Port Macquarie, Coffs Harbour to Brisbane. The freshwater reaches of the Clarence River support important populations of native freshwater fish including Eastern freshwater cod, an endangered fish species unique to the Clarence River system, and Australian bass.

The Indigenous Bundjalung people call the river Boorimbah, while the coastal Yaygir people call it the Ngunitiji. In November 1839 the Governor of New South Wales, George Gipps, officially changed the name to the Clarence River in honour of the previous King of the British Empire, William IV, 1st Duke of Clarence and St Andrews. The local government area of the Clarence Valley Council draws its name from the river and covers the lower half of the river valley.