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Taipei Basin

Taipei MRT, like the pulse of the city

Every morning and evening, there are countless people

At the MRT station, the sound of hurried footsteps staggered

The flow of people is surging like a torrent

However, when the sound of the pit

we seem to be able to hear

The Pulse and Rhythm of Taipei City

Bustling, Modern, Fast Lifestyle

These voices are like a mirror of memory

let's think back to those days

In this bustling city, we grow together

The sound of the MRT coming into the station is like an exclusive emotion

Taipei MRT, like the pulse of the city

Every sound is a touch

Let us remember that the beauty and touch of this city

臺北盆地

地形

地質

人文

產物

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台北盆地_edited.jpg

因大屯火山群的爆發形成較高的火山地形,約40萬年前,位於林口和台北間的山腳斷層陷落,使台北陷落為盆地,而林口抬升為台地,為台灣第二大盆地。

台北盆地地表為沖積平原,周圍分佈最廣闊之地層為第三系沈積岩所組成,夾少許火山岩,基盤以上為第四紀地層,包含:松山層、景美層、五股層和板橋層。

在史前時代,台灣盆地是原住民-凱達格蘭族的居住地,漢族則是18世紀才開始遷入區域,逐漸成長為台灣人口最密集的區域。

臺灣的包種茶興於南港,當地氣溫適合發展茶業,積極從事包種茶研製改良,研發「南港式茶製法」,並傳授鄉人成為台灣包種茶有規模之始。

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