Page 24 - 雕鐫海之角

三 貂角在臺灣島上的地理位置具有 an Diego cape lies
特殊意義，是雪山山脈極北端與
Swhere the nor thern
海相連的地方，也是雪山山脈東側的邊
most par t of Sheishan
界－梨山斷層（或稱匹亞南斷層）離開
三貂角-大里 本島的地點。該斷層線沿著礁溪海岸、 mountains meet the sea.
The shape is controlled by
蘭陽溪中上游的河谷、梨山、霧社，一 the Piyanan fault which is
地質公園 路延伸到玉山的東北方，幾乎將臺灣本 one of the most important

島從中央的部分切成兩半。 structural line of the island.
San Diego Cape–Dali 海岸線非常平直，海蝕平臺發展良好。 stream, the river vally of
It extends along Jiaosi
萊萊的位置在臺北縣貢寮鄉東邊，

Geopark 我們在海蝕平臺上到處可以看見發達的 the upper and middle parts
of the Langyang stream,
Lishan, Wushe, and reaches
線形圖案（狀似洗衣板），這是由於岩
the northeastern side of
層傾斜，受到波浪切割成海蝕平臺之
Yushan. This line almost
後，就會呈現一列列平行排列的線型圖
cuts the island into two
案。 halves.
北關擁有東北角沿岸形勢最險要、 Lai-Lai is in the east

規模最大的單面山，又有外形最整齊的 of Giungliau town of Taipei
county. The coastline is
豆腐岩，以及風小浪平的小海岬。
very straight, and the
shore platform is very well
developed. We can see line-
shaped patterns everywhere
on the platform, the form
is like washing board. This
is because of the slope the
variable strength of the rock
stratum. Beiguan possesses
a large scale cuesta from
bean-curd-shaped rocks
and a small sea cape in the
northeast coast.

地質圖書 Geopark at Northeast and Yilan Coast National Scenic Area