Page 14 - 雕鐫海之角
P. 14

地質年代表 Correlation of Strata
         gradation zone, because of varing intensity of or tectonic stress.
             In Yehliu, and Longdongwang in Northeast coast, we can trace                                       same as present. When the typhoons
         of many fossils in different sizes and shapes, such as round, ellipse,                                 come in summer, the sea bed at the   時代 EPOCH  地層 STRATUM  性質 PROPERTY  距今年代 AGE
         rectangular , tubular branching and even irregular lines.  Some                                        shallow sea will be distributed by the   砂   丘SAND DUNE  砂、粉砂  Sand, silt
         urchin fossils, which are commonly called  “the sand money”. The                                       powerful waves, causing the death   全 新 世  沖積層ALLUVIUM  礫石,砂及黏土
         fossils are piled up in a layer of sandstone, but not each layer has                                   of animal on the sea floor. These   HOLOCENE  階地堆積層  Gravel, sand, and clay
                                                                                                                                                                   礫石、砂及黏土
         fossils, only a few part of the urchins are preserved intact. Most are                                 remains are carried by the current,    TERRACE DEPOSITS  Gravel, sand, and clay  1萬年內
         incomplete.                                                                                            and deposited elsewhere, forming       桂竹林層        泥質砂岩、頁岩
             The Daliao sandstone is formed in the shallow sea environment,                                     layers  of   sandstone.  Geologists    KUEICHULIN   Muddy sandstone, shale, whitestone 900-375萬年前
                                                                                                                                                       FORMATION
         which is about 10 to 20 meters of depth, 10-20 million years ago. A                                    utilize there trace fossils to judge how   南 莊 層   砂岩及頁岩互層、含煤層
         lot of creatures lived on the sea bed at that time, leaving abundant                                   animals lined in the floor, and obtain a   NANCHUANG   Alternations of sandstone and   1200-900萬年前
                                                                                                                                                       FORMATION
                                                                                                                                                                   shale, intercalated coal seams
         trace fossil in the sandstone. The environment at that time is the                                     greater understanding of the natural   南 港 層       砂岩、粉砂岩及頁岩
                                                                                                                environment and habitat.               NANKANG FORMATION Sandstone, siltstone and shale  1900-1200萬年前
                                                                                                                                                                   砂岩及頁岩互層、含煤層
                                                                                                                                                       石 底 層
                                                                                                                                               中 新 世   SHIHTI FORMATION  Alternations of sandstone and   2000-1900萬年前
                                                                                                                                               MIOCENE             shale, intercalated coal seams
                                                                                                                                                       大 寮 層       頁岩及砂岩
                                                                                                                                                       TALIAO FORMATION  Sandstone and shale  2200-2000萬年前
                                                                                                                                                                   砂岩及頁岩互層、含煤層
                                                                                                                                                       木 山 層       Alternations of sandstone and
                                                                                                                                                       MUSHAN FORMATION              2390-2200萬年前
                                                                                                                                                                   shale, intercalated coal seams
                                                                                                                                                                   砂岩及頁岩、白砂岩含煤
                                                                                                                                                       澳 底 層       層
                                                                                                                                                       AOTI FORMATION  Sandstone and shale, white   2390-2200萬年前
                                                                                                                                                                   sandstone, intercalated coal seams
                                                                                                                                                       大桶山層        硬頁岩夾泥質砂岩
                                                                                                                                                       TATUNGSHAN   Argillite intercalated with muddy   2750-2390萬年前
                                                                                                                                                       FORMATION   sandstone
                                                                                                                                                       蚊子坑層        硬頁岩夾泥質砂岩
                                                                                                                                               漸 新 世   WENTZUKENG
                                                                                                                                               OLIGOCENE           Argillite intercalated with muddy   3200-2750萬年前
                                                                                                                                                       FORMATION   sandstone
                                                                                                                                                       龍洞砂岩        石英岩、礫岩            >3200萬年前
                                                                                                                                                       LUNGTUNG FORMATION Guartzite, conglomerate

                                                                                                                                                                         (資料來源:經濟部中央地質調查所)
                                                                                                                                                                            (Source: The Central Geological Survey, MoEA)












        東北角海岸鳥瞰與地質圖 Bird View of North East Coast and Geological Information

                                                                                                                        ▲  南雅奇石/孔世龍 攝
                                                                                                                          Nanya Peculiar Rocks/Kong Shih-Long


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