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| Eshuis, H.J.. |
| The bogs of S. E. Groningen are part of the great peat-marshes extending from S. E. Drente as far as N.W. Germany inclusive. So far as the territory of Westerwolde is concerned, people have begun digging off very early. According to the map by Krayenhoff in 1816 nearly the whole peat-marsh westward from the line Blijham—Termaarsch had already been reclaimed, only a few parts still being covered with the original peat-layer (cf. map, fig. 1). The digging off east of the above line commences at the beginning of the 19th century on the borderland of Groningen and Drente. Borings were performed in three places and the samples pollenanalytically and stratigraphically examined. |
| Tipo: Article / Letter to the editor |
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| Ano: 1936 |
URL: http://www.repository.naturalis.nl/record/535191 |
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| Eshuis, H.J.. |
| As an introduction to a number of researches of his own the author wishes to give the following data: „Veen” has two meanings in Dutch: 1. in a petrographic sense (peat) Von Büllow’s definition was accepted: „Torf” ist zu deflnieren als ein meist dunkles, kohlenstoffreiches und ± saures Gemenge unvollständig spezifisch-zersetzter Pflanzenteile, das erdgeschichtlich jüngste Glied der Verwantschaftsreihe der Kohlen, dessen Bildung noch heute andauert.” 2. in a plant-sociological-geographic sense (bog) the following definition has been suggested: a bog is a plot, the surface of which consists of a layer of peat, either covered or not with vegetation, with which that layer is genetically connected. The classification of bogs according to their position with... |
| Tipo: Article / Letter to the editor |
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| Ano: 1946 |
URL: http://www.repository.naturalis.nl/record/535082 |
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