Everything about Gatineau Hills totally explained
The
Gatineau Hills are a geological formation in Canada that makes up part of the southern tip of the
Canadian Shield, and acts as the northern shoulder of the
Ottawa Valley. They are also the foothills of the
Laurentian Mountains which stretch east through
Quebec, beginning north of
Montreal and joining up with others into
Vermont and
New Hampshire.
The geology of
Gatineau Park, which encompass these foothills, is related to the Eardly Escarpment, which is a
fault line that lies along the southern edge of the hills. This escarpment makes the part an attractive location for rock climbers and hikers, offering a beautiful view of the relatively flat fields below, which extend to the
Ottawa River. The Eardley Escarpment is part the northern side of the
Ottawa-Bonnechere Graben, which is an ancient
rift valley.
The Gatineau Hills are also significant as a
skiing destination, serving the neighbouring communities of
Ottawa,
Ontario and
Gatineau, Quebec.
Gatineau Park contains over 190 km of cross-country trails, and plays host to the annual
Gatineau Loppet competition. Downhill skiing is also available, at locations including
Camp Fortune,
Mont Cascades, and
Vorlage. The hills are small compared to the ski areas in the northeast, such as
Mont Tremblant and
Mont Ste-Anne, or southeast in
Vermont,
New Hampshire and
New York in the
USA.
The location of the hills are also useful for communications, and
Ryan Tower, a prominent communications tower at
Camp Fortune, provides a large portion of the area's broadcast television and radio signals.
The area is a prime tourist attraction, particularly during the October weeks when the foliage is turning colour. Photographs and paintings of the area are a popular tourist item.
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