The Waitomo Glowworm Caves attraction is a cave at Waitomo on the North Island of New Zealand, known for its population of glowworms,Arachnocampa luminosa. This species is found exclusively in New Zealand.
The name
"Waitomo" comes from the Māori words wai, water and tomo, hole or shaft. The local
Māori people had known about the caves for quite some time before the local
Māori Chief Tane Tinorau and an English surveyor, Fred Mace,
did an extensive exploration in 1887. Their exploration was conducted with
candlelight on a raft going into the cave where the stream goes underground.
This is now the exit for the cave. As they began their journey, they came
across the Glowworm Grotto and were amazed by the twinkling glow coming from
the ceiling. As they travelled further into the cave by poling themselves
towards an embankment, they were also astounded by the limestone formations. These formations
surrounded them in all shapes and sizes.
They returned many times after and Chief Tane
independently discovered the upper level entrance to the cave, which is now the
current entrance. Tane Tinorau and his wife Huti, by 1889, had opened the cave
to visitors and were leading groups for a small fee. The administration of the
cave was taken over by the government in 1906 after there was an escalation in
vandalism. In 1910, the Waitomo Caves Hotel was built to house the many visitors.
In 1989, the land and cave were returned to the
descendants of Chief Tane Tinorau and Huti. They now receive a percentage of
the cave’s revenue and are involved in the management and development of the
cave. These descendants encompass many of the employees of the caves today.
Geological
and volcanic activity has created around 300 known limestone caves in the
Waitomo region over the last 30 million years.
The limestone formations in the Waitomo Glowworm Caves
were formed when the region was still under the ocean about 30 million years
ago. The limestone is composed of
fossilized corals,seashells, fish skeletons, and
many small marine organisms on the sea beds. Over millions of years, these
fossilized rocks have been layered upon each other and compressed to create
limestone and within the Waitomo region the limestone can be over 200 m thick.
The caves began to form when earth movement caused the
hard limestone to bend and buckle under the ocean and rise above the sea floor.
As the rock was exposed to air, it separated and created cracks and weaknesses
that allowed for water to flow through them dissolving the limestone and over
millions of years large caves were formed.
The stalactites, stalagmites, and other cave formations grew from water
dripping from the ceiling or flowing over the walls and leaving behind
limestone deposits. The stalagmites form upward from the floor while the
stalactites form from the ceiling. When these formations connect they are
called pillars or columns and if they twist around each other they are called helicti. These cave
decorations take millions of years to form given that the average stalactite
grows one cubic centimetre every 100 years.
The most
renowned animal in the cave is the glowworm Arachnocampa luminosa.
There are several small underwater lakes that were created by freshwater creeks
or brooks.
The walls of the caves are covered with a variety of
fungi including the cave flower (a distant relation to the genus Pleurotus)
that is actually a mushroom-like fungus. The most common animals in the caves
are insects. This includes albino cave ants, giant crickets, and
of course the glowworms.
Source:
-http://en.wikipedia.org/wiki/Waitomo_Glowworm_Caves
- http://www.bestourism.com/items/di/7234?title=Waitomo-Caves&b=284
- http://extra-velganza.blogspot.com/2012/03/when-waitomo-glow-worm-cave-glowing-and.html
- http://secondglobe.com/item/glowworm-cave-waitomo-new-zealand/
Question:
1. Where is the glow worm cave?
a. New Island
b. Sidney
c. Manhattan
d. Mount everest
e. Waitomo
2. Actually, what is the glowworm?
a. Amphibi
b. Mammals
c. Bird
d. Insect
e. Reptile
Tidak ada komentar:
Posting Komentar