Last Updated：2022/12/24
Among relatively recent formations are the Manchurian and North China plains, which subsided along fairly clearly defined fault lines. However, while the present rolling topography of the Manchurian plain is largely of erosional origin, the North China lowland is entirely the product of the accumulation of sediments of the Yellow River.
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Among
relatively
recent
formations
are
the
Manchurian
and
North
China
plains,
which
subsided
along
fairly
clearly
defined
fault
lines.
However,
while
the
present
rolling
topography
of
the
Manchurian
plain
is
largely
of
erosional
origin,
the
North
China
lowland
is
entirely
the
product
of
the
accumulation
of
sediments
of
the
Yellow
River.
