Giant Hills
The Giant Hills are found to the east of the River Armont and south of the Collyner Mountains. Most scholars consider them a continuation of the main range of Collyner, although their average height is much lower. They are believed to have been formed during the eruption that caused The Year of No Summer.
The southern slopes of the Giant Hills form the north side of the Armontvale, a rich valley that supports arable farming. The settlement of Armontvale is the last town before the Giant Hills.
Tourism
The following is an excerpt from Trapadvisor's Guide to Westlo
The Giant Hills were once reputed to be a place of great sport and and excellent source of exercise for hillwalkers. Regrettably, such pastimes are no longer in fashion with the traveller of today, and the tourist economy of the Giant Hills has collapsed. This sad state of affairs is self-perpetuating, as lack of interest in the region has driven the locals to seek employment elsewhere, those remaining with little motivation to provide a tourist experience. The Giant Hills become wilder and less travelled with every passing year, until a change of fashion will make this wildness desirable again.
Type
Rolling Hills
Inhabiting Species
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