30.11.2012 Views

Wanted: Oscar Obsidian - Auckland Museum

Wanted: Oscar Obsidian - Auckland Museum

Wanted: Oscar Obsidian - Auckland Museum

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

Background<br />

Shapes of <strong>Auckland</strong> Volcanoes<br />

<strong>Auckland</strong>'s volcanoes come in a variety of landforms,<br />

depending on the style of eruption. Each<br />

volcano is formed by one eruption, or a short<br />

series of eruptions lasting no longer than a few<br />

months. Then a plug of lava solidifies in the vent,<br />

and later bubbles of magma find another place<br />

to erupt.<br />

Fieldtrips Around <strong>Auckland</strong>'s Volcanic Field<br />

The following is a list of places which provide a<br />

great opportunity to study <strong>Auckland</strong>'s volcanic<br />

field at first hand. The list does not include all the<br />

possibilities.<br />

Meola Reef, Pt Chevalier - <strong>Auckland</strong>'s longest lava<br />

flow, home to burgeoning mangrove swamps and<br />

being redeveloped as a park.<br />

Mt Eden, One Tree Hill, Mt Albert, Big King,<br />

Mangere Mountain etc - Scoria cones, craters and<br />

lava flows, also providing evidence of use by<br />

Maori and Pakeha. Use the map to check out volcanoes<br />

in your area.<br />

Three styles of eruption were involved in building<br />

the <strong>Auckland</strong> volcanic field. Each has produced its<br />

own type of rock and landform. While some volcanoes<br />

were created by one style, others were<br />

created by a combination. The landforms and<br />

eruption styles have been discussed previously, but<br />

this chart provides a summary of the events in<br />

forming <strong>Auckland</strong>'s volcanoes.<br />

Eruption Style Rock type Volcanic Shape Examples<br />

Lava Flows and<br />

Fields<br />

Conditions:<br />

Magma is free of gas and<br />

oozes out of volcano rim or<br />

side vent<br />

Fire fountaining<br />

Conditions:<br />

Gas-rich magma reaches<br />

surface without contact with<br />

water<br />

Explosive eruption<br />

Conditions:<br />

Rising magma meets<br />

groundwater causing<br />

superheated steam<br />

Solid basalt<br />

There are two types of<br />

lava flow:<br />

pahoehoe fluid, fast<br />

flowing and smooth.<br />

a'a thick, slowmoving and<br />

rough<br />

<strong>Auckland</strong> <strong>Museum</strong> 11<br />

Shield Rangitoto<br />

<strong>Auckland</strong> Domain - Tuff ring, <strong>Auckland</strong>'s first<br />

water supply and one of the earliest quarries,<br />

evidence of layers in tuff ring.<br />

Rangitoto - shield volcano, lava caves.<br />

In addition many volcanoes<br />

have lava flows but are<br />

not shield volcanoes.<br />

Meola reef is the longest<br />

flow and was extruded<br />

from the Three Kings<br />

volcano.<br />

Scoria Scoria cone Mt Eden, Three Kings, Mt<br />

Albert, One Tree Hill etc<br />

(these also exhibit other<br />

eruption styles)<br />

Tuff (ash and lapilli) Tuff ring <strong>Auckland</strong> Domain. Lake<br />

Pupuke, Panmure Basin<br />

Old Mt Eden Prison Quarry (<strong>Auckland</strong> Grammar<br />

land) - basalt columns.<br />

Takapuna Beach - fossil forest which was engulfed<br />

by lava from Lake Pupuke.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!