Geography, Environment, Peoples, and Government 3
and timber milling locked it into the networks of global capitalism. Sailing
ships,
followed by steam ships, then airplanes, and from the 1960s jet
airliners have broken down what the Australian historian Geoffrey
Blai-
ney has called the "tyranny of distance." Connection to the international
cable system from 1876, the expansion of telephone services soon after,
the popularity of radio from the 1920s, then television after
1960,
and the
widespread use of the fax machine and Internet in the
1990s
have enabled
New Zealand to enjoy full and active membership in the global village.
As a result, today's visitor to New Zealand finds a country apparently
little different from many others in the developed world. Yet the distinc-
tive environment and history of this group of large and mountainous
islands covering 103,000 square miles (about the same area as Colorado)
and stretching over 1,000 miles from north to south (from subtropical 34
degrees to subarctic 47.5 degrees south) make any similarities rather su-
perficial.
ENVIRONMENT AND GEOGRAPHY
Less than a quarter of the New Zealand landmass lies below 650 feet,
and there are 253 named peaks over 7,000 feet tall. The Dutch explorer
Abel
Tasman
accurately labeled it "a land uplifted high." Extensive moun-
tain ranges drag down precipitation from the surrounding oceans to create
an unpredictable climate. In general terms, it is temperate (especially com-
pared with Britain or the northern United States) and lacks the freezing
winters and scorching summers of continental countries. But the weather
never locks into predictable patterns like those of southern California or
the Mediterranean, creating headaches for meteorologists. The country is
subject to bouts of severe flooding, while the so-called El Nino and La
Nina oscillation produces frequent droughts on the east coast and
snow-
storms in the
mountains—as
featured so vividly in Peter Jackson's movie
version of The Lord of the Rings.
These climatic hazards are amplified by geological instability. New Zea-
land straddles the large Pacific and
Indian-Australian
tectonic plates,
which are moving in opposite directions. Consequently, earthquakes oc-
cur regularly. Among the most destructive were those that leveled Wel-
lington in
1855
(now the capital city, but still a village when the earthquake
struck) and flattened the small cities of Napier and Hastings in
1931.
Strict
building codes and clever engineering initiatives have helped reduce the
risks of earthquake damage, but a large event is inevitable, especially in
Wellington, which like San Francisco is sited on a fault line. Three large
volcanoes in the central North Island are still active, and spectacular erup-