River Mole River Mole The River Mole is a tributary of the River Thames in southern England. It rises in West Sussex near Horsham and flows northwest through Surrey for to the Thames at East Molesey, opposite Hampton Court Palace. The river gives its name to the Surrey district of Mole Valley. The Mole crosses the North Downs between Dorking and Leatherhead, where it cuts a steep-sided valley, known as the Mole Gap, through the chalk. Much of the catchment area lies on impermeable rock (including Wealden Clay and London Clay), meaning that the river level responds rapidly to heavy rainfall. During
Ottawa Valley English neither feature is documented in the City of Ottawa itself or in other nearby urban areas, which speak Standard Canadian English. In the 1980s, linguist Ian Pringle and colleagues claimed that was a huge variation in dialect features throughout the thinly-populated Ottawa Valley, notably with large Hiberno-English influence; however, the nature of such variation has never been thoroughly described. At a general phonetic level, the Ottawa Valley twang of "Irish-descended people" is characterized by raising of and in all contexts, as opposed to the Canadian English's more typical "Canadian raising", which is context-dependent. In terms of syntax, the twang features