文學院
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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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Item 臺灣北部地區主要瀑布群的地形學研究(國立臺灣師範大學地理學系, 1989-03-01) 沈淑敏The purpose of this research is to distinguish the factors which influence the form of water苯alls. The defination of a waterfall in the study is of which the height is higher than 5m and will not dry around the year. The form discussed here includes five parts, the face of waterfall (the ratio of width and length), the inclination of fall wall, the existence of plunge pool, the appearance of cap rock, and the relationship between the dip of strata bed and river orientation. The study area includes four waterfall groups in the northern Taiwan, named Pinhsi, Tatun. Wulai and Chiaohsi group. The geological setting are quite different among four groups. There are 40 waterfalls investigated totally, 12 in Pinhsi group, 8 in Tatun group, 11 in Wulai group and 9 in Chiaohsi group, respectively. After classifying each kind of forms and factors of 40 waterfalls, I analyze the relationship between each kind of forms and factors with methods of contingency table and X2 test. The conclusions are as follows: 1. Waterfalls mostly are splender type according to the face form, inclined type to the wall form, horizontal type and reverse type to the bed form. However, there isn't a special type obviously on the form of plunge pool and of cap rock. 2. For waterfall belongs to the small scale landform, the form of it is controlled mainly by the factors of lithology.Item 臺灣北部番子澳漁撈活動的時空間配置(地理學系, 1987-03-??) 陳憲明Based on the viewpoint of man-environmental relationship, this study attempt to use the time-space approach to design an analytical framework for dealing with the fishing activities at Fan-tsu-au, a coastal village in the northern Taiwan. Data were collected by direct observation of fishing activities on the sea, as well as by interviewing the fishermen. In the 1950s, the fishermen at Fan-tsu-au were engaged mainly in torch light net fishery. They organized three non-powered fishing crafts as a team and used weak fishing lamps to catch round herring, squids and other phototaxis fishes that migrate on the surface-water. The fishing season for torch light net fishery is from May to the beginning of October in each lunar year. In this period, because of moonlight which interferes fishing efficiency, the fishing activities formed a monthly cycle in compliance with the moon's transit, duration and intensity of moonlight. But, such fishery is restrided by such factors as the physical capacity of non-powered fishing crafts, illumination capacity of fishing lamps, prey-food habits of fish schools and sleeping requirements of fishermen. Therefore, the fishing activities are restricted to a space of three nautical miles from the shore and 2-3 hours after dark and before dawn. In 1950 to 1960, with the advance of fishing technology, and the powered fishing boats were popularly adopted, the fishermen at Fan-tsu-au has replaced traditional torch light net fishery with modernized stick-held dip net fishery, long-line fishery and spear fishing. Though the stick-held dip net fishery and torch light net fishery use the lamps to allure the fish schools on the surface-water, because of powered fishing boats, and increased illumination capacity of fishing lamps, the time-space scope for stick-held dip net fishery is expanded. At the moment, the fishing season for catching squids, from February end to the beginning of October in each lunar calendar, the fishermen woulItem 臺灣北部高冷地區農業土地利用的研究(地理學系, 1986-03-??) 陳憲明Item 臺灣北部海岸沙丘之地形學研究(地理學系, 1992-03-??) 石再添; 張瑞津; 林雪美; 張政亮; 連偵欽Item 臺灣北部地區主要瀑布群的地形學研究(地理學系, 1989-03-??) 沈淑敏The purpose of this research is to distinguish the factors which influence the form of water?falls. The defination of a waterfall in the study is of which the height is higher than 5m and will not dry around the year. The form discussed here includes five parts, the face of waterfall (the ratio of width and length), the inclination of fall wall, the existence of plunge pool, the appearance of cap rock, and the relationship between the dip of strata bed and river orientation. The study area includes four waterfall groups in the northern Taiwan, named Pinhsi, Tatun. Wulai and Chiaohsi group. The geological setting are quite different among four groups. There are 40 waterfalls investigated totally, 12 in Pinhsi group, 8 in Tatun group, 11 in Wulai group and 9 in Chiaohsi group, respectively. After classifying each kind of forms and factors of 40 waterfalls, I analyze the relationship between each kind of forms and factors with methods of contingency table and X2 test. The conclusions are as follows: 1. Waterfalls mostly are splender type according to the face form, inclined type to the wall form, horizontal type and reverse type to the bed form. However, there isn't a special type obviously on the form of plunge pool and of cap rock. 2. For waterfall belongs to the small scale landform, the form of it is controlled mainly by the factors of lithology.Item 臺灣北部區域製造業分布之研究(國立台灣師範大學地理學系, 1986-10-??) 李薰楓Item A Geomorphological Study of Active Fault in Northern and Eastern Taiwan(國立台灣師範大學地理學系, 1984-10-??) 石再添 張瑞津 黃朝恩 石慶得 楊貴三Item 臺灣北部地區觀光遊憩資源的空間分佈與遊憩需求空間系統(國立台灣師範大學地理學系, 1989-12-??) 曾國雄; 李銘輝