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The shrinkage in distribution of closed canopy forest in Costa Rica from 1940 to the present. Only the volcano slopes within the area of Guanacaste National Park (northwestern Costa Rica) contained enough pristine forest to be recorded in this map in 1983 (Rodas 1985). Note that the relative rate and thoroughness of forest removal has been substantially greater in the dry western habitats than in the mountainous rainforest habitats.

This article text was automatically generated and may include errors. View the full page to see article in its original form.I whakaputaina aunoatia ēnei kuputuhi tuhinga, e kitea ai pea ētahi hapa i roto. Tirohia te whārangi katoa kia kitea te āhuatanga taketake o te tuhinga.
Permanent link to this item
Hononga pūmau ki tēnei tūemi

https://paperspast.natlib.govt.nz/periodicals/FORBI19891101.2.26.7

Bibliographic details
Ngā taipitopito pukapuka

Forest and Bird, Volume 20, Issue 4, 1 November 1989, Page 26

Word count
Tapeke kupu
69

The shrinkage in distribution of closed canopy forest in Costa Rica from 1940 to the present. Only the volcano slopes within the area of Guanacaste National Park (northwestern Costa Rica) contained enough pristine forest to be recorded in this map in 1983 (Rodas 1985). Note that the relative rate and thoroughness of forest removal has been substantially greater in the dry western habitats than in the mountainous rainforest habitats. Forest and Bird, Volume 20, Issue 4, 1 November 1989, Page 26

The shrinkage in distribution of closed canopy forest in Costa Rica from 1940 to the present. Only the volcano slopes within the area of Guanacaste National Park (northwestern Costa Rica) contained enough pristine forest to be recorded in this map in 1983 (Rodas 1985). Note that the relative rate and thoroughness of forest removal has been substantially greater in the dry western habitats than in the mountainous rainforest habitats. Forest and Bird, Volume 20, Issue 4, 1 November 1989, Page 26

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