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 臺灣東部河口地區之地形學研究(地理學系, 1995-10-??) 石再添; 張瑞津; 林雪美; 張政亮; 劉明錡; 陳政典The vincinity of the estuaries is one of the most populated area in the world. In order to ultilize the resources of this area more reasonably, the understanding of its geomorphological, hydrological and sedimentary characteristics becomes a main and basic task. Since estuary is located on the interface of river and sea, the morphology of estuary is influenced by the factors coming from both environments. The drainage basin area, shoreline length, shape factor, channel gradient, runoff, sediments and monthly discharge, etc. are factors coming from land, while the wind, current, wave and tide etc. coming from the sea. This study focuses on eleven estuaries of the eastern coast of Taiwan. Based on the stream slope, number of channels, discharge, etc., these estuaries can be divided into straight and braided pattern. The former has sandbars or spurs, such as Hualien Hsi, Hsiukuluan Hsi and Kangkou Hsi, while the latter have braided channels, sandy-gravel sediments and changeable sandbars, such as Hoping Hsi, Liwu Hsi and the estuaries in Taitung coastal area. The eastern coast is classified as wave-dominated type according to average wave height and tidal range. The wave impacting upon the area between Hoping Hsi and Hsiukuluan Hsi is severer. The forms of the estuaries in eastern Taiwan have significant seasonal change due to the seasonal differences of discharge, monsoon and typhoon. In the summer, the channels usually become wider and the sandbars are gentler and extended seaward for most estuaries. In the winter, however, these sandbars become narrower, steeper and extend toward right bank. The mouth of channels will be narrowed or even closed when typhoon coming. The forms of estuaries are stable in the long-term scale. Eleven estuaries have only slight change during the period from 1904 to 1989, moving back and forth within the distance of 250m. The channel migration of most estuaries, however, is obvious.Item 臺灣西南部河口地區之地形學研究(地理學系, 1995-03-??) 石再添; 張瑞津; 林雪美; 張政亮; 劉明錡; 陳政典The vincinity of the estuaries is one of the most populated area in the world. In order to ultilize the resource of this area more reasonably, the understanding of geomorphogical, hydrological and sedimentary characteristics becomes a main and basic task. Since estuary is located on the interface of river and sea, the morphology of estuary is influenced by the factors coming from both environments. The drainage basin area, shoreline length, shape factor, channel gradient, opening form, runoff, sediments, and monthly discharge etc. coming from the land. While the wind current, wave and tide etc. coming from the sea. This study area focuses on 20 estuaries of the south-western coast of Taiwan. The five of them are gravel estuaries and the rest are sandy. By correlation grain size of sandy estuaries has relationship with channel gradient below 100m, width of opening and shape factor. The forms of sand bar on estuaries are changed seasonly. Most of them has a tendency migrating southward due to northern moonsoon. The 20 estuaries can be classified into the wave dominated type, the tide dominated type and the runoff dominated type according average wave height, specific discharge and tidal range. Comparing the location of 20 estuaries during the period from 1904 to 1990(85 years). Most estuaries tend to migrate westward. The changes of estuaries are controlled by the intensity of wave and precipitation, the influence of reservior and hydraulic engineering and the changes of land use.Item 臺灣花東海岸海階的地形學研究(地理學系, 1988-03-??) 石再添; 鄭國雄; 許民陽; 楊貴三This paper is the first year report of the research project “A Geomorphological Study of Marine Terrace in Taiwan”. The Huatung coast is along the Pacific coast of Eastern Taiwan, adjacent to the convergent boundary of Eurasia Plate and Philippine Sea Plate, marine terrace is typically developed in this region. Based on air photo interpretation, geomorphometry, field excursion and accurate survey of altitude, the results are summarized as follows: 1. Classified and correlated by the continuity of altitude and extend of the marine terrace surfaces, there are three dominate marine terraces in study area. The flights of marine terraces in the southern part are comparatively more widely distributed than in the north, the lowest one and the newly raised wave-cut platform are well developed throughout the study area. 2. Altitude of terraces in the southern part is obviously more higher, expecially in the upper two steps, showing that there are wave-like uplifted and tilted slightly to the north. Yet the lowest steps together its newly raised wave-cut platform have almost the same height throughout the study area, this implies that recent uplift rates are progressing with equal amount, and in the upper steps, the tectonic movement has the property of accumulation. 3. The displacement of terrace surfaces is observed as a short-wave length warping, upwarping has been taken place with the axes in the vicinity of Chanping, Chengkung and Tulan, the distance between the axes is about 25 to 30 km. 4. The third steps are furnished with multi-levelled terraces, at intervals of 2-5 m in elevation, deduces from the mode of seismic uplifts in the neighborhood, those multi-levelled terraces may originated by the co-seismic uplift. 5. The features of marine terraces are also influenced by geological setting, in the area of more?resistant rocks, marine terraces are very narrow and covered with thin marine boulders, coastal landforms such as wave-cut benItem 臺灣西部海岸沙丘之地形學研究(地理學系, 1993-06-??) 石再添; 張瑞津; 張政亮; 林雪美; 連偵欽Coastal sand dunes are widely distributed along the western coast of Taiwan from Touchien Hsi to Erhjen Hsi. Based on maps work, airphoto interpretation, particle size analysis, field investigation, etc, the study results are summarized as follows: 1. The form and the magnitude of the western coastal sand dunes have close relationship with the source of 13 rivers' sand supply, alongshore current and wave action, power and direction of wind, terrains, rainfall, evaporation and vegetation. 2. The coastal dunes develop well on riversides of Chung Kang His, Holung Hsi, Choshui Hsi and offshore bars along Chianan coast. Two principal types of these dunefield may be distinguished, namely, active dunes and stabilized dunes. The two dunefield types contain a variety of dune features, such as transverse dunes, barchans, longitudinal dunes, and dome dune etc. 3. The grain sizes of beach and dune sand are quite uniform. The Md φ and δ φ on average of the dune sand is smaller than the beach sand. This shows that wave process is stronger than wind process. 4. Comparing the maps published in 1926 and 1984. the change of coastal dunes is clear. Because the dunefield was used as fishery or watermelon and sugarcane planting, most of the sand dunes were leveled off entirely. Some of the residual sand dune still exist at present fixed by windbreak forest. For sand dunes have the function of protecting coasts, they had better be well-planned and well-used so as to main-tain the sustainable utilization of land souces.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 臺灣西南部嘉南平原的海岸變遷研究(地理學系, 1998-05-??) 張瑞津; 石再添; 陳翰霖嘉南海岸平原形成於晚更新世，海岸線的變遷與海水進退相對應，近三百多年來整體呈現向西推移的趨勢，古笨港、魍港（蚊港）及倒風內海已逐漸淤填，並被大量圍墾開發為魚塭或鹽田。濱外沙洲西側海岸除河口地區外，均向內侵蝕，在海汕洲及王爺港汕西側最大侵蝕率約達 12mn/yr。 外傘頂洲整體向東南方陸地漂移， 沙洲北段漂移速率甚至達58mn/yr。 沙丘主要分布於新港、鹿草一線以西，其中北港地區因濁水溪供沙充足，較嘉義沿海發達。 北港以西的海岸沙丘，大致分布在 7mn 以下，呈四列南北帶狀分布，隱示不同時期的海岸線位置， 應形成於大湖期海侵（ 3500-4000yr B.P. ）之後。 比較 1904-1926及 1990 年各時期之沙丘，其規模大致逐漸減小，係受人類開發利用影響所致。海岸平原地區向為人口稠密地帶，地形變遷常造成洪患威脅、丘沙漂移、土地利用改變、沿岸聚落興衰、土地權屬爭議及行政區劃定等之衝擊。相反的，人類擴張聚落、興建水庫、修築堤防、開鑿渠道、圍墾海埔地、取直河道等作為，也造成天然地形之改變，地形變遷與人類生活息息相關，其研究正可提供為土地規劃與開發利用的參考。Item 臺灣活斷層的地形學研究(地理學系, 1986-03-??) 石再添; 鄧國雄; 張瑞津; 石慶得; 楊貴三Item 臺灣西南部臺南海岸平原地形變遷之研究(地理學系, 1996-11-??) 張瑞津; 石再添; 陳翰霖The Tainan coastal plain in southern Taiwan had been formed since late Pleistocene. The coast was marked by the offshore bars and lagoons, and have prograded to the west about 13 km since last three hundred years. The large lagoon was named as "paleo Taichiang Inland Sea" in Ching dynasty historical document had been filled up and reclaimed as fish ponds and salt pans due to the rapid sedimentation. However, the west coast of offshore bars have been eroded with a maxium rate about 14 m/yr in Tingtouerh bar in this century. The coastal dunes are distributed mainly in Salun, Tainan and Kunshen. Among them, Salun and Tainan dunes were deposited in Tahu Transgression stage (3500-4000 yr B.P.) where as the Kunshen dunes developed on offshore bars in last three centuries. Besides, a series of dunes is still exsited along the former Tsengwen River. Due to the expansions of the cultivated and built areas, all the dunes have decreased in magnitude. The river channel changed significantly both in hills and coastal plains. In the hills, 13 meander neck cutoffs can be observed in Erhjen River and Tsengwen River. On the coastal plain, river channel shifted by meandering and avulted suddenly in typhoon season because of epesodic sedimentation in the river bed. There were four big channel avulsions recorded since 19 century in Tsengwen River and the range of channel avulsion from north to south is about 25 km. However, the channel was confined after the dyke had been constructed in 1934. Overall, the geomorphological changes of Tainan coastal plain were caused by long term physical processes but modified strongly by human agency in the recent time. The geomorphological changes have induced some impacts on the human beings such as the decline of port, moving of village to prevent flooding, confusion of administrative boundary, etc.Item 臺灣西南部嘉南海岸平原河道變遷之研究(地理學系, 1997-11-??) 張瑞津; 石再添; 陳翰霖臺灣西南海岸平原各河流的河道變遷，主要導因於曲流作用、暴風雨後主流的迅速淤積，以及河口段的河道延長。八掌溪及曾文溪下游即分別發生過五次及四次的改道，河道擺幅達20公里以上，但自1920年代河堤興建後，河道便少有大幅改道現象。因海岸平原向西擴展，河流下游呈現延長河的特性，以急水溪為例，1904至1990年間河口每年平均向西推移43m。海岸平原地區向為人口稠密地帶，地形變遷常造成洪患威脅、土地利用改變、沿岸聚落興衰、土地權屬爭議及行政區劃定等之衝擊。相反的，人類興建水庫、修築堤防、開鑿渠道、河道截彎取直等作為，也造成天然地形之改變，地形變遷與人類生活息息相關，其研究正可提供為土地規劃與開發利用的參考。Item 臺灣北端海岸的海階地形(國立台灣師範大學地理學系, 1988-12-??) 石再添; 許民陽