| L earning
Objective 18b
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18.b. Be able to describe the major events of formation
and weathering which have taken place on the island of Maui.
I. GENERAL FEATURES.
A. The present day island of Maui is actually part of
a more massive volcanic structure composed of six major volcanic masses.
B. Maui Nui, as this structure is called, is made of four existing
islands, Maui, Lana'i, Kaho'olawe and Moloka'i. In the recent geologic past
during lower sea levels, these islands would be united into a single structure.
Now they are separated by shallow seas.
C. The broad plain connecting the two volcanoes of West and East
Maui formed when new flows from the younger Haleakala volcano backed up
against the older West Maui volcano. This is much like the Leilehua plains
connecting the two mountain ranges of O'ahu.
II. TWO MAJOR PARTS OF MAUI correspond to the two vents of the hot
spot.
A. West Maui:
1. West Maui is the older part of the island. Its volcano may
be extinct. Its highest point is Pu'u Kukui, about 5,700 feet (1,736 m.),
and it is usually shrouded by heavy clouds.
2. Iao Valley's sheer cliff boundaries nearly coincide with the former boundary
of the main caldera. Lavas which once filled the caldera are now primarily
gouged out by stream erosion.
B. East Maui:
1. East Maui's Haleakala's volcano has erupted as recently as
200 years ago. It is considered dormant. Its crater is about 7 miles long,
2 miles wide and 1/2 mile deep.
2. The magnificent crater is primarily erosional in nature. It is formed by the expanded heads of two valleys resulting in a single large depression. After a very
deep erosional basin was formed, renewed volcanic activity flooded it with
lava flows and cinder cones.
3. Erosion has been uneven in the crater, with more rapid erosion on the
rainy northern and eastern side of Haleakala.
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