以上の記述に依り本地域の漁業地理部門一部の取扱を終るのであるが,此特殊漁網を通して濱波太の地域性をあらはすと言ふ地誌學的の目的を充分果し得なかつたことは遺憾である。更に他日を待つて補正したい。次に本稿の要約を掲げると次の如くである。
(1) 鰍建網漁業地は房總半島部では調査地52組合中20組合に見ることが出來た。何れも岩礁帶に装置する。全般的には今日この簡易なる定置底刺網が衰弱の傾向にあることが認められる。
(2) 地域に依てこの漁網に對する社會規約の程度が著しく異り,濱波太は調査地域の何れに比較しても最も鋭敏性を發揮してゐると見られた。
(3) 當地域に於けるこの漁網のかかる發育の原因としては,一挺漕卓越地域として其他の優越せる漁法を持たぬこと,資本の貧弱,漁港の不備等の人的要因と,地形的に小屈曲島嶼波蝕岩盤海藻等に恵まれ,特に仁右衞門島の存在に依る一方的風浪の保護等が明かにこの漁網に對する優れた自然性と見ることが出來た。
(4) 夫々の網入場に於ける漁網の張方差等等は海況並に魚類の習性との關係を考究せしめる手懸を與へ,特に沿岸性潮流・底盤との關係等は重要である。
(5) 慣行に依て他海區に迄本地域の網入場の進出が許されてゐることが,ここの純漁部落たる性質を物語ることとなり,且この漁網の當地域に於ける大なる存在價値の一面を説明することともなる。
(6) 魚期として冬場のイナダ夏場のイサキが代表的のものであるが,特に統制された漁網に依る纏まつた漁獲が帝都への送荷を好都合ならしめてゐる。

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There are two local towns, Matô and Kari, on the southwestern coastal plain of Taiwan. They lie about 20km north of Tainan City (the Capital of Tainan Prefecture), the former being situated 6km east of the latter. At the end of 1934, their respective populations were 11, 468 and 7, 655, the majority consisting of descendants of Chinese immigrants during the last three centuries (Matô 96%, Kari 90%).
The two towns are represented by closely combined quarters of two different settlement forms, rural and urban, both having nearly the same population, for which reason the writer introduces them as examples of the socalled compound settlement.
The rural settlement form of both towns under consideration, which is the compact type similar to most rural settlements predominating throughout South Taiwan, is distinguished from the scattered types so common in the northern part of the island. On the whole, the type of the rural settlement form in Taiwan follows that of the Chinese mainland beyond the strait. And since the rural settlement quarter is generally inhabited by farmers, whose houses are surrounded by small fields, vegetable gardens, or Citrus orchards, the area of the rural quarters is very extensive, the whole pattern of farmhouses being rather that of the scattered type as compared with the other ordinary compact forms that have neither fields nor gardens in their premises. Moreover, every farmhouse and on the borders of every premise are planted bamboo hedges and betel-nut trees, so that the rural quarter as a whole looks like a large forest.
The commercial quarters of these two towns are on the whole surrounded by rural settlements, and along the main communication roads through them, assume urban forms of “Strassendorf”. Both sides of the street are lined with retail and handicraft shops, markets, and official buildings. Thanks to the recent city improvements, the cultural landscape of the commercial quarters of both towns is fairly good with a modern aspect.
The formation of these compound settlements of the rural-urban settlement suggests that they represent a general tendency toward urbanization during the course of the development of all rural settlements. In other parts of Taiwan, however, almost all the rural settlements and the local commercial towns are at present separated from each other.
The particularly extensive areas occupied by the rural quarters of the two towns under consideration are mainly due to fertile soil and favourable water supply, these two important factors facilitating intensive farm management and rural living. The more extensive the development of the rural quarters, the more active are the commercial centers, said activities being enhanced by various causes political and industrial. It seems that originally the commercial center started in the form of a market in the foreground of shrines, gradually growing later to a “Strassendorf” with the development of commercial facilities along the main road.

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The Hida Range (about 3000m height) runs from N to S at the NE extremity of the Inner Zone of South-western Japan. Near the peaks of this range, between 2800m and 2300m, are remnants of the old erosion surface that were completed during the previous cycle. They are surrounded by steep valley walls of “aufsteigende Entwicklung” (Fig. 1) that show recent rapid uplift of the mountain land (Fig. 3).
The two Rivers Kurobe and Takase flow from S to N, dividing this range into two or three parallel mountain chains. The longitudinal profiles of the valley floors (Fig. 2, 7), which are steep in the uppermost part, become gradually gentler, and at 1500-1300m have already graded slope of full maturity. These erosion levels are called Upper Stream Levels (Daira. Level in the R. Kurobe and Yumata Level in the R. Takase). In their middle parts the inclination becomes again very steep and the valley form changes into young narrow gorges (Fig. I IV is a transverse section of the Daira Level, while II and III are those of the gorge). Here we find many knick points, which are called Middle Stream (or Simorôka in the R. Kurobe) Knick Points. The tributaries of these rivers also belong to the same type (Fig. 3).
The author traced and reconstructed the older erosion levels in the valley floors, which were formed during a stationary period of the earth movement. From these data he concludes that there were two phases of elevation -Pre- and Post Upper Stream Levels in this district.

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