The diagram illustrates the formation of the Hawaiian
island
chain in the central Pacific Ocean Use synonyms
as a result
of volcanic activity associated with a stationary hot Linking Words
spot
beneath the Earth’s crust.
Use synonyms
Overall
, the Hawaiian Islands were formed sequentially as the Pacific tectonic plate moved northwestwards over a fixed mantle hot Linking Words
spot
, causing a series of volcanic eruptions. As the plate continued to shift, older volcanoes became inactive Use synonyms
while
new ones developed, resulting in an age gradient across the Linking Words
island
chain.
At the base of the process, a plume of magma rises from a hot Use synonyms
spot
located approximately 2,883 kilometres beneath the Earth’s surface. As magma reaches the ocean floor, repeated eruptions lead to the accumulation of solid rock, gradually building volcanic mountains that eventually emerge above sea level to form islands. The youngest volcano develops directly above the hot Use synonyms
spot
and continues to grow through frequent eruptions.
Meanwhile, the Pacific plate moves at a rate of approximately 7–9 centimetres per year, carrying older islands away from the hot Use synonyms
spot
. As these volcanoes drift Use synonyms
further
from the magma source, they become extinct and erode over time. Linking Words
This
explains why the oldest volcanic rocks, dating back around 80 million years, are found at the far end of the Linking Words
island
chain, Use synonyms
while
the youngest volcanic activity occurs on the Linking Words
island
of Hawaii.Use synonyms