著者

籠瀬 良明

出版者

The Human Geographical Society of Japan

雑誌

人文地理 (ISSN:00187216)

巻号頁・発行日

vol.2, no.3, pp.36-47,96, 1950-07-30 (Released:2009-04-28)

参考文献数

18

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In the plain of Takada can be traced an old watercourse of the Hokura about five kilometers in length. What characterize this old watercourse are free meandering and natural banks, running on both sides of it and higher than the level by one meter or two with fields and hamlets on them. A long succession of fine paddy-fields stretehes on this old course of the river, which were brought under cultivation in middle ages. (Especially, it is the case with the lower course of the river.)In the article two of those examples, Matsuhashi and Funatsu in the village of Honda are dealt.[The author made a lecture on other such examples, Honda-Enokii and Katatsu, at the autumnal meeting of Association of Japanese Geographers last year, and explained why the region should be supposed to have been cultivated in Middle Ages, also explaining its characteristics. The details are to be mentioned in next number.]

著者

籠瀬 良明

出版者

THE TOHOKU GEOGRAPHICAL ASSOCIATION

雑誌

東北地理 (ISSN:03872777)

巻号頁・発行日

vol.30, no.1, pp.24-33, 1978 (Released:2010-04-30)

参考文献数

1

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There are several irrigation channel patterns peculiar to Tsugaru Plain, which are classified as follows.1) Parallel channel group: Several channels run in parallel and each one flows into a group of fields.This pattern was perhaps established against heavy droughts in Edo era, whose origin is not yet certain and it has not been reported elsewhere in Japan. The peculiarity of this pattern is not recognized by local farmers.2) Passing through channel group: Several channels run long way through paddy fields of other village directly downstream.3) Channel group without distinct draining end4) Channel group without distinct nourishing origin.5) Crossing-over channel group

著者

籠瀬 良明

出版者

THE TOHOKU GEOGRAPHICAL ASSOCIATION

雑誌

東北地理 (ISSN:03872777)

巻号頁・発行日

vol.35, no.4, pp.159-168, 1983 (Released:2010-04-30)

参考文献数

4

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In the western part of Ibaraki prefecture, there is a slender zone of paddy fields which is located in between Mitsukaido City and Sanwa Town. It is called ‘Iinuma-Shinden’. This zone had been a shallow lake until 1725 (the 10th Year of Kyoho). The lake was reclaimed by Tokugawa Shogunate which accepted the villagers' petition of the reclamation.The writer has studied this zone, and clarified where the former lacustrine shoreline was existed (Figs. 4, 8, etc.). The data for deciding upon the shoreline are as follows; a) the large scale maps published after 1965 (Figs. 8, 9, etc.), b) the map of district baundaries of former towns and villages in this zone (Fig. 6.), and c) the old map of this zone made in 1724 (Figs. 1, 7, etc.).From these data, the writer has estimated the surface level of the former lake was 10.7 meter in height and made clear that the farmers' settlements were distributed around the paddy fields made by reclamation. Furthermore, the writer has clarified that the place of their settlements was on the topset flat of the former delta (of the “lake days”), and consisted of soft silt and sand from 20 to 40 meter thick.

著者

籠瀬 良明

出版者

日本地理教育学会

雑誌

新地理 (ISSN:05598362)

巻号頁・発行日

vol.26, no.3, pp.1-28, 1978-12-25 (Released:2010-02-26)

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“Fjord are best developed on the coasts of British Columbia, southern Alaska, southern Chile, eastern Canada, Greenland, Norway, Iceland and Spitsbergen, the south-west of South Island (New Zealand); and finally Antarctica-Embleton & King (1968): Glacial and Periglacial Geomorphology p. 234”“fjord, or FIORD, long narrow arm of the sea, commonly extending far inland, that results from marine inundation of a glaciated valley. Many fjords are astonishingly deep-The New Encyclopaedia Britannica, 1968”There are 56 fjords in Denmark. The fjords in east-Jylland are the result of marine submergence of the deepest parts of the tunnel valleys, good examples are given by Vejle Fjord, Mariager Fjord. Sidinge fjord and Lamme fjord in Sjælland are central depressions under sea level. Maximum extent of the Stone Age Sea, and Ringkø bing Fjord, Nissum Fjord in west-Jylland are lagoons.

著者

籠瀬 良明

出版者

Japan Cartographers Association

雑誌

地図 (ISSN:00094897)

巻号頁・発行日

vol.1, no.3, pp.30-33, 1963-10-31 (Released:2011-07-19)

著者

籠瀬良明著

出版者

古今書院

巻号頁・発行日

1995

著者

籠瀬 良明

出版者

日本地図学会

雑誌

地図 (ISSN:00094897)

巻号頁・発行日

vol.6, no.2, pp.21-28, 1968

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□昭和37年以来, 日本のほとんどの市 (および一部の町村) で, 町界・町名・住居表示の番地についての, 根本的な改変調整事業が進められている。その改変の度合い, 全国的統一性からいって, ある意味では大化改新頃の, 条里制の実施にも匹敵する大事業といっても過言ではない。□従来の町割形態を, 旧城下町に卓越する路線式のものと, 道路などで取囲まれた街画式のものに大別する。その場合, 条里区画の発達する地域では, その区画がどの程度町界に反映するか。□住居表示案内図の構成とルール

著者

籠瀬 良明

出版者

日本地図学会

雑誌

地図 (ISSN:00094897)

巻号頁・発行日

vol.16, no.1, pp.30-31, 1978

著者

籠瀬 良明

出版者

一般社団法人 人文地理学会

雑誌

人文地理 (ISSN:00187216)

巻号頁・発行日

vol.3, no.3, pp.63-68, 1951-07-30 (Released:2009-04-28)

参考文献数

4

著者

籠瀬 良明

出版者

日本地図学会

雑誌

地図 (ISSN:00094897)

巻号頁・発行日

vol.16, no.1, pp.30-31, 1978-03-31 (Released:2011-07-19)