文學院

Permanent URI for this communityhttp://rportal.lib.ntnu.edu.tw/handle/20.500.12235/2

院成立於民國44年,歷經50餘年的銳意發展,目前設有國文、英文、歷史、地理、臺文等5個學系、翻譯和臺灣史2個獨立所,以及全球華人寫作中心和國際臺灣學研究中心。除臺史所僅設碩士班,其餘6個系所均設有碩、博士班;目前專兼任教師近250人,學生約2500餘人。

本院早期以培養優秀中學國文、英文、歷史和地理教師為鵠的,臺灣中學語文和史地教育的實踐與成功,本院提供不可磨滅的貢獻。近年來,本院隨師範體系轉型而調整發展方向,除維持中學師資培育的優勢外,也積極朝理論研究和實務操作等面向前進。目前,本院各系所師培生的教師檢定通過率平均在95%以上;非師培生在文化、傳播、文學、應用史學及環境災害、地理資訊系統等領域發展,也已卓然有成。

本院各系所教師的研究能量極為豐富,參與國內外學術活動相當活躍。根據論文數量、引用次數等指標所作的學術力評比,本院居人文領域全國第2名。各系所之間,無論是教師的教學與研究,或學生的生活與學習,都能相輔相成、榮辱與共,彼此渾然一體,足堪「為師、為範」而無愧。

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    臺灣海岸山脈泰源盆地河流地形之研究 
    (國立臺灣師範大學地理學系, 1990-03-01) 鄧國雄; 沈淑敏 
    Taiyuan Basin, located in the south part of Coastal Range in East Taiwan, is famous for its landforms of well-developed river terraces and meanders. The whole drainage basin belongs to the Mawuku Stream System. The number of different stages of river terraces that could be correlated is eleven and the three youngest terraces which developed in the outlet reach haven't extented to the basin yet. In the basin, the channel sinousity is rather large however the amplitude is quite small. The phenomena of seven cut-off meanders that formed at different stages indicate the streams are always meandering. There are two main factors that influence the development of Taiyuan Basin. One is the spatial arrangement of lithology difference of Tuluanshan and Takankao Formations; the other is erosion basis lowered intermittently by the effects of uplifted movement and sea-level eustacy.
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    臺灣海岸山脈泰源盆地河流地形之研究
    (地理學系, 1990-03-??) 鄧國雄; 沈淑敏
    Taiyuan Basin, located in the south part of Coastal Range in East Taiwan, is famous for its landforms of well-developed river terraces and meanders. The whole drainage basin belongs to the Mawuku Stream System. The number of different stages of river terraces that could be correlated is eleven and the three youngest terraces which developed in the outlet reach haven't extented to the basin yet. In the basin, the channel sinousity is rather large however the amplitude is quite small. The phenomena of seven cut-off meanders that formed at different stages indicate the streams are always meandering. There are two main factors that influence the development of Taiyuan Basin. One is the spatial arrangement of lithology difference of Tuluanshan and Takankao Formations; the other is erosion basis lowered intermittently by the effects of uplifted movement and sea-level eustacy.