Characteristics of the voi mep massif’s altitudinal belt differentiation
The Voi Mep massif of the Truong Son range, havingthe highest peak in the Quang Tri area (1739m), is composed of granite and granodiorite intrusive rocks in Ben Giang-Que Son complex. This massif is fairly isometric with characteristic landforms comprising: remnants of old pediment surfaces, mount...
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| Format: | Article |
| Language: | English |
| Published: |
VNU
2014
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| Subjects: | |
| Online Access: | http://repository.vnu.edu.vn/handle/11126/4528 |
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| Institution: | Vietnam National University, Hanoi |
| Language: | English |
| Summary: | The Voi Mep massif of the Truong Son range, havingthe highest peak in the
Quang Tri area (1739m), is composed of granite and granodiorite intrusive rocks in Ben Giang-Que Son complex. This massif is fairly isometric with characteristic landforms comprising: remnants of old pediment surfaces, mountain slopes and valleys with steep profiles. The massif area has a regular altitudinaldifferentiation manifested in the formation of two climatic belts: tropical humid climatic belt, subtropical humid climatic belt; two
altitudinal soil belts: red yellow soil belt and red yellow humus soil belt; four altitudinal
vegetation cover types: evergreen broadleaf closed forest, mixed broadleaf/needleleaf
forest, needleleaf forest and association of Arundinaria sat. The combination and interaction of natural components led to the formation of two altitudinal landscape belts: mountain foot tropical landscape belt and medium montane subtropical landscape belt. |
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