I visited Eggie between Christmas and New Year, and stayed a couple of nights on the mountain. More specifically, I started around Lake Dive and Dawson Falls on the southern side, and made my way around to North Egmont via the eastern side. If you’re after a remote wilderness experience then Egmont National Park isn’t the easiest place to get one. It’s quite small, and very few parts of it (if any) are out of reach of daywalks, especially during the long days of summer. On the other hand, I think it’s definitely worth visiting. Egmont National Park is an isolated circle, literally. It’s as if someone took a compass on a flat topographical map, and drew a circle around the centre of the mountain to define the national park. Trees and native bush outside this line have been removed, and generally converted to farm-land.
Lake Dive in front of Egmont
and Fanthams Peak.
Dates: 28th – 30th December, 2008
Location: Egmont National Park, Dawson Falls to North Egmont.
People: Just me.
Huts visited: Lake Dive Hut (1 night), Kapuni Lodge (0 nights), Hooker Shelter (0 nights), Waingongoro Hut (0 nights), Maketawa Hut (1 night).
Route: Lake Dive Loop from Dawson’s Falls (lower track then upper track), then around the eastern side of Egmont from Dawson Falls to Maketawa Hut on the lower track, and out via North Egmont.
[Photos]
Mt Egmont seen from New Plymouth,
with the Pouakai Range to the right.
As with most parks in New Zealand, Egmont has its own colour and character; this park is sharply defined by a solo cone-shaped volcanic mountain in the middle. There is actually a mountain range going through Mount Taranaki/Egmont, which is the consequence of a slowly moving volcanic centre of which remnants can still be seen poking out of the sea off the coast of New Plymouth, then climbing to the south into the Pouakai Range, continuing through Egmont’s discrete 2518 metre peak, and finishing at Fanthams Peak on the southern slope, which is the consequence of the most recent volcanic action. Although it’s been relatively dormant in the past few hundred years, the park is dotted all over with massive domes and bluffs, all of which are symptomatic of the mountain’s violent and continuing volcanic history.