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RELIEF REPRESENTATION
- 13-1-2010
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Figure 4. Most eastern part of Java. Map extracts of a: ‘Nederl. Oost-Indië’, by R. Bos and K. Zeeman, 1928, 3rd edition, published by P. Noordhoff, 108 x 136 cm, scale 1 : 3.500.000; b: ‘Java en Madoera’, 1923, published by Topografische Inrichting, 87 x 224 cm, scale 1 : 500.000; c: ‘Eenvoudige Wandkaart van Nederlandsch Oost-Indië’, by R. Noordhoff and H. Niehaus, 1915, published by J.B. Wolters, 182 x 219 cm, scale 1 : 2.750.000.
Every now and then nonprofessionals also produced relief representations that were of surprisingly high quality. Schoolmaster R. Noordhoff (not to be confused with one of the leading publishers of school wall maps P. Noordhoff) emphasized in his writings [5] the importance of the physical character of the landscape, and examined several techniques of relief representation. In 1902 he was strongly against hypsometric layers (“de schaduwzijde der Höhenschichten, made in Germany” according to the multilingual Noordhoff). However, he was an advocate of oblique hill shading, and on his school wall maps he put his opinions into practice (see map extract in Figure 4c). The fact that this schoolmaster’s representation of the volcanos of Java can compete with that of the ‘Topografische Inrichting’ (Figure 4b) is quite amazing.
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