Beach rock(English Page)
Beach Rock(Japanese Page)
TANAKA Yoshikuni : A study on the Formation
of Beach Rock in the Okinoerabu Island ,
Central Ryukyu Islands. Chiri-Kagaku ( Geographical Sciences ), vol.
38, (no. 2) pp. 91-101, 1983
English abstract
TANAKA Yoshikuni (Harima Yogo School,Tatsuno,Hyogo,Japan)
Beach rock is composed of beach sediments
that have been chiefly cemented by calcium
carbonate deposits. The cemented aggregates
may consist of bioclastics sand (mainly coral
,shell ,and foraminifera fragments) ,gravels
or of whatever else the beach may be composed
of. Typical beach rock seems to have developed
best along the sub-tropical and tropical
coasts.
Beach rocks have been found on the coasts
of Ryukyu Islands ,including the Amami ,Tokara
,and Ogasawara ( Bonin ) Islands. The beach
rock is found as far north as at Noto Peninsula
( N. Lat. 37 ) in Japan. Beach rocks crop
out at about mean tadal level or about mean
high tidal level providing the range is large.
In this report , the distribution of beach
rocks and ground-water springs on Okinoerabu
Island are shown ( Fig. 1 ) , and the source
of calcium carbonate is also discussed on
the basis of water qualtities of moat-water
, ground-water on the Otsukan beach abd Yakomo
beach in the south-western part of okinoerabu
Island. Beach rock runs some 500m long and
40m wide along the coast on the Otsukan beach
in Okinorabu Island. In this area , beach
rock can be seen in the intertidal zone.
Here the beach rock , which belongs to sandy
beach rock , is made of bioclastics sand.
It can be stated that the beach rock corresponds
with the intertidal beach rock reported by
Takenaga (1965).
The results of the present writer's study
of beach rock on Okinoerabu Island are as
follows;
There seems to be no relationship between
the distribution of beach rocks and that
of ground-water springs on Okinoerabu Island.
The calcium carbonate is supplied from moat-water
as the result of instrumental analysis of
moat-water and ground-water. Incipient consolidation
of beach rock on the surface of intertidal
zone or at the higher level is held by strong
insolation.
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