Hong Kong's natural terrain
is dominated by mountains and hills with
steep slopes. The highest point in Hong
Kong is Tai Mo Shan in the New Territories
at 957 metres above Principal Datum. The
deepest point is 66 metres below Principal
Datum in Lo Chau Mun (Beaufort Channel)
north of Po Toi Island. The mountains
consist primarily of volcanic rocks, with
some of the lower hills formed of granite.
Low-lying areas tend to be formed of granite
or sedimentary rocks. In places, hill-slope
debris forms a mantle over the bedrock
and alluvium fills some of the valleys.
Much of the seabed is covered by marine
mud with some scattered sand banks.
The oldest exposed rocks
are Devonian fluvial sediments that were
deposited 400 million years ago. The region
was subsequently inundated by a shallow
sea. Sediments from this period are represented
by the carboniferous marble of Yuen Long
and Ma On Shan. From the Jurassic to Cretaceous
periods, between 170 and 140 million years
ago, Hong Kong was the scene of violent
volcanic activity. Thick accumulations
of lava and ash were deposited. The eruptions
were associated with the development of
several giant craters (calderas). At deeper
levels, the volcanic deposits were intruded
by molten magma, which slowly crystallised
to form granite. Igneous activity ceased
60 million years ago. Rocks now seen on
the island of Ping Chau represent sediments
laid down in a lake on the edge of a desert.
During the Quaternary
period, spanning the last two million
years, major glaciations in polar regions
affected the global sea level, which fell
to 120 metres below the present level,
leaving the site of present-day Hong Kong
as much as 130 kilometres from the coast.
In interglacial periods, such as at the
present time, the global sea level rose
to its present level and higher, and marine
sediments were deposited. Detailed information
of the geology of Hong Kong can be found
in a series of 15 geological maps at a
scale of 1:20 000 and six accompanying
memoirs. These were produced by the Hong
Kong Geological Survey, a part of the
Geotechnical Engineering Office. The Hong
Kong Geological Survey has also recently
published two new memoirs and a set of
1:100 000 geological and thematic
maps that synthesise and summarise the
current state of knowledge of the geology
of Hong Kong. |