| ◎ |
Sand seashores: scattered
along coastal areas of Baisha, Nanwan,
Kenting, Siaowan, Shadao and Fongchueisha. |
| ◎ |
Fringing reef shores:
scattered in the west coast and along the
coastal areas of Eluanbi. |
| ◎ |
Rock seashores: scattered in
the east coast to the north of Jialeshuei,
with the rock seashore of Jialeshuei being
the most well known. |
| ◎ |
Limestone tableland cliffs:
scattered on top of coastal fringing reefs
in areas such as Dapingding, Guanshanyan,
Maobitou, Sheding, Kenting Forest Park and
Eluanbi Tableland. |
| ◎ |
Isolated mountains:
including mountains formed by rocks from
other places on top of Kenting's strata such
as Menmaluoshan, Dashanmushan,
Dajianshihshan, Siaojianshihshan and
Cingwashih. |
| ◎ |
Slumping cliffs: scattered
along the east coast in Maobitou and from
Eluanbi to Fongchueisha. |
| ◎ |
River mouths: including the
estuaries of the Baoli and the Gangkou
Rivers. |
| ◎ |
Rivers and lakes: including
the Gangkou River and Longlyuantan. |
| ◎ |
Intermontane basins:
scattered in the surrounding areas of
Nanrenshan. |
| |
The rich topography of Kenting
National Park
reflects the active movements of earth's crust for
millions of years, which have caused the Hengchun
peninsula to sink, rise, crumple and collapse,
making it the best classroom for the study of
topography and geology. |