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Kim Hy Proposed Nature Reserve - Frontier-publications.co.uk

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when heavy mists and, sometimes, hoar frost settles in the valleys early in the morning.<br />

At this time of year there tends to be a large difference between diurnal and nocturnal<br />

temperatures (reaching 20.8ºC during <strong>Frontier</strong>’s survey), and the temperature can fall to<br />

2ºC. Much of the precipitation <strong>co</strong>ndenses in the form of mist; during <strong>Frontier</strong>’s phase 2<br />

work, 26 <strong>co</strong>nsecutive days passed without any rain during November. These winter<br />

<strong>co</strong>nditions can seriously damage crops. Average temperature is 21.6ºC (maximum<br />

38.6ºC). Humidity averages 82% but can fall to 10%. Prevailing winds are north-easterly<br />

and south-westerly.<br />

2.2.2 Topography and <strong>Hy</strong>drology<br />

Much of the landscape of <strong>Kim</strong> <strong>Hy</strong> and An Tinh <strong>co</strong>mmunes, where most of the remaining<br />

forest lies, is strongly characterised by dramatic outcrops of limestone tower karst,<br />

forming a topographical patchwork of sheltered valleys and gorges interspersed with<br />

steep, rocky cliffs. Access over this terrain is extremely difficult, ac<strong>co</strong>unting for the<br />

relatively in tact forest block; slope angles on the karst are over 45º and most reach<br />

heights of 650-800m, the highest being Kuoi Coi at 985m. A number of caves, crevasses<br />

and subterranean gorges have formed in or under the limestone from erosion and<br />

chemical weathering, performing some important e<strong>co</strong>logical functions.<br />

To the north and east, mudstone–based hills with slope angles of around 20-25º and<br />

average heights of 400-500m source the tributaries of the Bac Giang river, which flows<br />

through An Tinh and Luong Thuong <strong>co</strong>mmunes, 5km to the north-east of Na Ri and into<br />

Ngan Son district. Between these hills the landscape is dominated by flooded rice<br />

paddies.<br />

There are virtually no over-ground water bodies within the main limestone area of <strong>Kim</strong><br />

<strong>Hy</strong> and An Tinh as most precipitation per<strong>co</strong>lates through the limestone and <strong>co</strong>llects in or<br />

below the limestone bedrock in deep underground ‘wells’, forming a well-developed<br />

subterranean drainage system marked by seasonal fluctuations in water level and<br />

sometimes spilling over to form small surface streams.<br />

2.2.3 Geology and Soil<br />

Geologically, <strong>Kim</strong> <strong>Hy</strong> and An Tinh <strong>co</strong>mmunes are dominated by Devonian-<br />

Carboniferous limestone of various depth of deposition and which have been influenced<br />

by denudation and karstic processes associated with fluctuations in sea level. The<br />

mudstone hills rest on beds of quartzite, sandstone and schist. No soil surveys were<br />

<strong>co</strong>nducted during the <strong>Frontier</strong> work phases: the information below is taken from surveys<br />

undertaken by FIPI in 1997. A map summarising distribution of the main soil types is<br />

held at the provincial FPD office.<br />

<strong>Frontier</strong> Vietnam Forest Research Programme Technical Report No.24. 21

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