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  • 欠田 早苗, 和田 洋
    人類學雜誌
    1978年 86 巻 3 号 235-239
    発行日: 1978年
    公開日: 2008/02/26
    ジャーナル フリー
    紀ノ川沿岸には古墳が多数散在しているが,これからの発掘人骨の報告はない。今回の人骨は頭部の破損が少なく,修復することなく計測しえたので報告する。20才未満ではあったが頭蓋最大長が特異的に大きい値を示し,畿内人の特徴である短頭とはやや性質を異にする。
  • 岡崎 勉, 北島 美智子
    化学と教育
    1999年 47 巻 10 号 686-687
    発行日: 1999/10/20
    公開日: 2017/07/11
    解説誌・一般情報誌 フリー
  • 塚本 浩司, 樋口 幸江, 加納 誠
    日本物理学会誌
    2005年 60 巻 4 号 294-297
    発行日: 2005/04/05
    公開日: 2019/01/25
    ジャーナル フリー
  • (2)発掘人骨(弥生時代•古墳時代)
    池田 次郎
    人類學雜誌
    1981年 89 巻 4 号 505-514
    発行日: 1981年
    公開日: 2008/02/26
    ジャーナル フリー
  • 史学雑誌
    1978年 87 巻 12 号 1773-1796
    発行日: 1978/12/20
    公開日: 2017/10/05
    ジャーナル フリー
  • 中野 栄治
    人文地理
    1976年 28 巻 3 号 337-359
    発行日: 1976/06/28
    公開日: 2009/04/28
    ジャーナル フリー
    The aim of this theme is to find out a clue to the disclosure of the reclaimed land in the middle reaches of the Kino River, but its chief purpose is firstly to make a restorative research of the ancient land development or “jori chiwari” (land division) and secondly to restore the ancient landscape of the area. The area of this study is the middle reaches of the Kino River (Naga County) where the jori restoration still remains unrevealed.
    The methods of study are;
    1) drawing up of a map of the jori land division. 2) naming of the jori land division and finding out the possible location of Akinano-sho area. 3) jori land division and the topographical conditions. 4) its retation of irrigation. 5) the relation of “jori” with the Kokubunji Temple and with “go”.
    (1) The distribution of jori in the middle reaches of the Kino River can be roughly parceled into 7 blocks. (Fig. 1, A∼G jori sections)
    In the northern part of the river the main “jori” is made up of, the easy slope on the periphery of the composite fan which extends to the southern foot of the Izumi Mountains and the lower terrace. (Fig. 4)
    In the southern part of the river, we also can find the remains of such jori in the flood plain of the Kishi River, a branch stream of the Kino River.
    “jori” in the Kii Mountainous district extends as far as the Nogami Hachiman Shrine.
    (2) In the north, the direction of “jori” way of land division adopts the Seihoi (ditches of land are in the direction of North, South, East, West) with the Kokubunji-Temple as its center.
    In the upper reaches the maximan propencity is N14°W and in the lower reaches, N7°E. (Fig. 1)
    But as a whole, the dircetion of the land division takes un-“seihoi” taking the shape of a fan.
    This was influenced by the direction of the fan-shaped land on the northern bank.
    But there are frequent occasions of each “jori” being in succession.
    Each “jori” has the uniform characteristic in the north, while in the south “jori” is fragmentary.
    It is clear that they divided the land by the unit of 1 “cho” (section) (Fig. 2) but in the inner part can we sea many indefinite and irregular shapes.
    Only in the fan-shaped area, “haori”-shape variation and in the lower terraces “Nagaji”-shape variation are found.
    (3) In the north, the upper reaches (Ito) and the lower reaches (Nagusa) have the same way of naming, that is, “jori” is divided into 25 “zu” (jo) from east to west, 7 “ri” from south to north.
    The land belonging to the Kanshinji Temple and Akina-sho (a feudal manor) in the ninth century is presumably the “Shoiki”.
    This investigation will disclose how the alluvial fan was reclaimed in Heian period, how “jori” was named in the Kahoku district, and provide basic material concerning archaeological views.
    It is presumed that they adopted the way of naming based on “block”.
    (4) As to the irrigation of “jori” paddy in the fan, in case of the basin of the Negoro River, the irrigation by the erosional valleys and ponds are thought to be old irrigation forms.
    (5) The 2 square “cho” domain belonging to the Kiikokubunji Temple adapts the “seihoi”. And the boundary of the temple domain connects with the jori in the vicinity with the transitional type. (Fig. 6)
    (6) The presumption of the location of 7 “go” of Naga county written in the “Wamyosho” will be submitted as a tentative plan (Fig. 2), taking the connection with the block “jori chiwari” into account.
  • 齋藤 武馬, 森本 元, 小林 さやか, 浅井 芝樹, 平岡 考
    山階鳥類学雑誌
    2018年 50 巻 1 号 35-85
    発行日: 2018/08/31
    公開日: 2019/08/31
    ジャーナル フリー

    From March 2004 to September 2017, Mr. Tatsuo Kazama donated his private bird skin collection to the Yamashina Institute for Ornithology. This collection is comprised of 851 specimens of 303 species. According to the labels, these specimens were collected mainly from Niigata Prefecture (86%) between 1953 and 2014. The collection covers an over 60-year period, and is valuable material for documenting the bird fauna in Niigata Prefecture.

  • 明治から昭和初期
    金坂 清則
    人文地理
    1975年 27 巻 3 号 252-295
    発行日: 1975/06/28
    公開日: 2009/04/28
    ジャーナル フリー
    Many studies have been published to deal with Japan's urban growth which began at the Meiji era, but there seems to be very few works which focus its examination on the urban functions and city and region relationship on a meso-scale, and have a scope to develop into macro-scale study of the whole region. Since a regon exists as a part of the whole, attention to such a direction will be urgently needed.
    The writer intends to explain a historical change in the city and region structure in the Niigata Plain-the country's second largest plain-and its surroundings for the period of about seventy years since the early Meiji era. To this end the processes of forming the Ura Nippon Region must be unraveled dynamically and regionally, and location and the sphere of influence of urban functions, which may be classified into four categories-administrative, cultural, economic and transportational, are examined in relation to city size and distribution of cities. Parts of the results obtained are summarised as follows.
    1. In 1879 there were thirty-three cities and towns in the objective region, and thirty-four in 1935. Cities in 1879 are classified into three, ie. a city in Class I, four in Class II, and twenty-eight in Class III (See Figure 1).
    2. The four cities in Classes I and II were separated each other by 30 to 40 kilometres, and the distances between Class III cities were around 6 to 9 kilometres, the intervals being quite uniform. The outline of this structure had already been formed by the middle of the eighteenth century. Since that time most of those cities have had periodical fairs, and half of them were nuclei of textile and hardware industries which had been located at the rural settlements around them (See Figures 1 and 2).
    3. On this foundation the administrative and cultural institutions such as government offices and schools began to be located corresponding to city size at the early years of Meiji. At the same time economic activities, especially of modern manufacturing industies which tend to be unevenly distributed, began to be accumulated around those cities. The framework of established orders among cities was therefore not broken down but was solidified more as the time passed.
    4. Consequently larger cities genarally developed more in proportion to their scale. If the Zipf's rule is applied, the three largest cities had smaller scale than the rule's ideal value, and Class III cities larger than the same in 1887, and the case was reversed in 1935. As a result the difference in the scale of the largest and the smallest cities increased by 2.7 times during the period. This was also the process when the order among cities became rank-sized (Table 11).
    5. After the middle of the Meiji era the objective region was gradually subordinate to Tokyo, and formed into a part of the Ura Nippon Region. The trend was definitely fixed at the mid-Taisho years. The cities developed only slowly in this region, and their influence over the countryside remained weak. Therefore the countryside began to be controlled by the cities outside this region and by the outer realm. The large-scale landlordship was the most important internal factor to keep the rural country into stagnation.
    6. Another factor to bring about such change to the region was a drastic change in transportation: a shift from maritime and river-borne traffic to the modern railway. This should not be overlooked.
  • 日本考古学
    1998年 5 巻 6 号 182-280
    発行日: 1998/12/10
    公開日: 2009/02/16
    ジャーナル フリー
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