Inside the Earth
Oceanic crust is dominated by mafic and ultramafic intrusive igneous rocks whereas continental rocks are dominated by granitic (felsic) intrusive igneous rocks.
The difference in density has an impact on isostacy of crust floating on the semi-fluid upper mantle (asthenosphere), with continental crust (about 2.7g/cm3) rising or floating above oceanic crust (about 3.5 g/cm3).
The continental crust is by far the older of the two types of crust.
The mantle, oceanic crust, and continental crust all have different compositions due to a process called partial melting.
Because continental crust is less dense than oceanic crust it floats higher on the mantle, just like a piece of Styrofoam floats higher on water than a piece of wood does.
On Earth
Types of Plate Boundaries
Plate boundaries can be categorised in three fundamental types:
(a) Divergent boundaries, where plates separate and move in opposite directions, allowing new lithosphere to form from upwelling magma. This either occurs at mid-ocean ridges (the so-called seafloor spreading) or at rifted continental margins.
(b) Convergent boundaries, where plates move towards each other. One plate either sinks beneath the other along a subduction zone or plates collide.
(c) Transform fault boundaries, where plates move horizontally past each other.
Based on the three types of plate boundaries, a global network of approximately twelve major plates of irregular shape and size cover the Earth's crust. Where one type of plate boundary is terminated it is transformed into a boundary of a different type.
Tides are caused by gravitational pull of the moon and the sun.
The rise and fall of the tides play an important role in the natural world and can have a marked effect on maritime-related activities.
Tides are one of the most reliable phenomena in the world. As the sun rises in the east and the stars come out at night, we are confident that the ocean waters will regularly rise and fall along our shores.
Tides are very long-period waves that move through the oceans in response to the forces exerted by the moon and sun. Tides originate in the oceans and progress toward the coastlines where they appear as the regular rise and fall of the sea surface.
When the highest part, or crest, of the wave reaches a particular location, high tide occurs; low tide corresponds to the lowest part of the wave, or its trough. The difference in height between the high tide and the low tide is called the tidal range.
New Zealand lies on the boundary between two tectonic plates. When the sub-ducting plate melts the buoyant magma can come to the surface and erupt. New Zealand has many volcano types, three main types are recognised. Eruptions are different depending on the type of magma.
Inside the Earth there is a red-hot liquid rock, called magma. Volcanoes happen when magma rises to the surface of the earth, which causes bubbles of gas to appear in it. This gas can cause pressure to build up in the mountain, and it eventually explodes.
When the magma bursts out of the earth, it is called lava.
Like earthquake activity, volcanoes in New Zealand usually occur along the plate boundary. Beneath New Zealand, the Pacific plate is pushing into the Indo-Australian plate and is being forced down into the Earth’s mantle. This creates a zone of subduction where the plate melts. Magma rising from this “subduction” zone produces a line of active volcanoes known as a volcanic arc. Most of New Zealand’s active volcanoes are caused by this process.
New Zealand’s volcanoes are part of a larger zone of active volcanism at plate boundaries that rim the Pacific Ocean – the "Pacific Ring of Fire".
Earth’s tilted axis causes the seasons. Throughout the year, different parts of Earth receive the Sun’s most direct rays. So, when the North Pole tilts toward the Sun, it’s summer in the Northern Hemisphere. And when the South Pole tilts toward the Sun, it’s winter in the Northern Hemisphere.
Earth's axis is an imaginary pole going right through the center of Earth from "top" to "bottom." Earth spins around this pole, making one complete turn each day. That is why we have day and night, and why every part of Earth's surface gets some of each.