The
casual visitor to Taranaki may be forgiven for thinking that there is only
one volcano here. Strictly speaking, that’s true. Historically, Taranaki
has four volcanoes. Mt
Taranaki
is just the current flavour of the millennia. The Pouakai Range
(1400-metres) reached about 2000-metres 250-millennia ago before erosion
began its slow process. While the Kaitake Range reached about the same
height as Mt Taranaki (2518-metres), 500,000 years of
erosion has reduced
it to 684-metres. The Sugar Loaves, off the coast of New Plymouth, are the
eroded stumps of a 2000-millennia old volcano crater. With deep canyons,
numerous lava-rock caves, and the convergence of warm northern currents
and cold southern currents attracting diverse marine life, the Sugar
Loaves are also a marine park.
The
vast mudflows, or lahars, from Pouakai, some leaving deposits
nine-kilometres thick, were superceded by those of Mt Taranaki. Maori used
some of the mound-like lahars as little fortresses. These remarkable land
formations are best seen on the western ring plain.
Highlights
of Taranaki’s 300-kilometre coastline are the many 25-metre tall
pinnacles long since separated from the 100-metre distant cliffs. Standing
like silent sentinels, they are oblivious but will ultimately succumb to
the eroding sea. These spectacles are best seen on the White Cliffs
walkway between Pukearuhe and Tongaporutu. Look for White Cliff Walkway
signs. If you’ve only got 30-minutes, visit the outstanding Three
Sisters at Tongaporutu.
Out
east, 11 rivers drain the steep beef and sheep hill country. The
Tangarakau River winds its way through the 500-metre high hills, smothered
in impenetrable rainforest. The Tangarakau Gorge, part of The Forgotten
World Highway (SH
43) follows the river. Just pull over, turn off the engine, and listen.
And
look over thefertile plain ring where over 2700 dairy farms produce almost
20 percent of New Zealand’s total milk solids. To a cow - it’s heaven.
To a visitor - it’s green. Lush green.