he
long narrow peninsula extending some 800 kilometres north of Auckland
is known as Northland - or occasionally, in flights of fancy, as the
winterless north'.
The east and west coast of the peninsula differ
dramatically. In the east there are dozens of superb sandy beaches
and excellent harbours which once provided stages for the coastal
shipping which served the north. By contrast, the west coast extends
in a long curve from Cape Reinga to Auckland, broken only by the
Kaipara and Hokianga harbours.
Geologically, Northland has a varied history. Ancient
volcanic plugs, such as those of St Peter and St Paul at Whangaroa
and Mt Manaia at Whangarei contrast with vast sedimentary deposits
and the extensive dunelands backing onto the western beaches. Although
nowhere do the mountains reach any great heights, the land is rugged
and there are few plains except those edging rivers. This factor,
along with often poor soil, delayed development of the north until
relatively recently.
When the Pakeha (European) arrived, Northland was covered with
forest, dominated by kauri, a tree of great size and with excellent
timber. The logging and milling of kauri was the principal industry
north of Auckland for many years after Pakeha settlement and, although
there are a few stands left, the great trees that once flourished
in this area are now mostly gone. Today, the small patches of native
bush that remain between Auckland and Whangarei are usually too
small to support many native birds and the larger stands have few
tall trees.