吉斯伯恩-东海岸地区的土壤及其放牧问题

H. Gibbs
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引用次数: 0

摘要

吉斯本-东海岸地区主要由陡峭的山地组成,山顶上有许多小块起伏的土地,山谷里有条状的梯田和河滩。丘陵地区延伸到500至1000英尺高的海岬海岸,中间有许多陡峭的山谷。除了大河,尤其是形成吉斯本平原的怀帕阿河及其支流,山谷都很狭窄。本区土壤种类较少,但变化频繁,格局复杂。土壤的格局和地形的高低起伏主要是由于东海岸的地质历史,这将在下面的段落中概述。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
SOILS OF THE GISBORNE-EAST COAST DISTRICT AND THEIR PROBLEMS FOR PASTORAL USE
The Gisborne-East Coast district consists mainly of steep hill country, with many small areas of rolling land on hilltops and strips of terrace and river flats in the valleys. The hill country extends to the coast in headlands 500 to 1,000 ft high separated by numerous valleys with steep sides. Valleys are narrow except those of large rivers, especially the Waipaoa River and associated tributaries which have formed the Gisborne Plains. The range of soils in the district is fairly small, but changes are very frequent and the pattern is complex. Both the pattern of soils and high relief of the landscape are due principally to the geological history of the East Coast, which is outlined in the following paragraphs.
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