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Full-text - Norsk entomologisk forening

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202 A. Lillehammer<br />

parts of the area (Figs. 2 and 3), and it is<br />

only in the inner areas that the mean January<br />

temperature falls below 0° C. In the outermost<br />

areas the mean January temperature is<br />

more than +2° C (Fig. 3.1). The whole area<br />

experiences heavy precipitation between 1200<br />

mm and 2000 mm in the outer areas, and<br />

more than 2000 mm in the inner areas·<br />

On the coastal area of the Haugesund<br />

peninsula, west of Skjoldefjorden and Alfjorden,<br />

heights of more than 100 m a.s.l.<br />

are rare. In the central areas, east of Alfjorden<br />

and Skjoldefjorden, the mountains<br />

are higher, between 500 and 700 m a.s.!. in<br />

the outer parts and up to 1000 m a.s.l. in the<br />

inner parts (the area of Sandeid and Vikedal).<br />

In this area there are prominent valleys. In<br />

the inner areas, east of Vikedal, the mountains<br />

are even higher (up to 1600 m a.s.!. in<br />

the north-eastern parts) and the fjords cut<br />

deeply into the mountain massif.<br />

The vegetation of the area of the Haugesund<br />

peninsula consists mainly of bog and<br />

heath vegetation. Wooded areas total about<br />

8 0 /0. In the central area the wooded areas<br />

on average constitute about 24 % of the area.<br />

In the inner area, which is mainly mountainous,<br />

the wooded area totals about 8 %.<br />

River and stream descriptions<br />

In the inner areas, streams and rivers are<br />

abundant and the deep valleys contain some<br />

of the longest and largest rivers in Rogaland.<br />

The streams alternate between fast flowing<br />

and more slow flowing reaches. The stone<br />

size is very variable at all altitudes and<br />

the streams are generally fringed by dwarf<br />

willow up to about 7-800 m a.s.l.<br />

In the lowland areas there is often a<br />

dense fringe of alder, willow and birch along<br />

the rivers and streams, in which the substrate<br />

consists of different gravels and stones. Pollution<br />

is minimal and only occurs for a short<br />

distance near the fjords.<br />

In the central areas, the streams are of the<br />

same type as in the lowland inner areas. The<br />

vegetation is rich along the streams. The<br />

streams are seldom polluted to any noticeable<br />

degree, and if they are, they flow only a<br />

short distance before reaching the sea.<br />

The outer areas have very little wooded<br />

vegetation except in the shallow valleys.<br />

There is often a dense fringe of alder and<br />

other deciduous trees along the streams which<br />

on the whole are smaller and shorter than in<br />

the central and inner areas.<br />

Calcium hardness varied to some extent in<br />

the lowlands. Values up to 1. 7 mg Ca++/1<br />

were found in the coastal and central areas<br />

and up to 0.9 in the inland regions. Usually<br />

the values were much lower and below 1.0<br />

mg Ca++/1. In the highest areas up to<br />

0.4 mg Ca + +/1 was measured. Usually the<br />

values were much lower. The pH is around<br />

6.0 in the lowlands of the whole area, but on<br />

average it is a little higher at the coast than<br />

in the inner areas where the lowest pH value<br />

measured was 5.3.<br />

Stonefly fauna<br />

In this area 19 species were collected<br />

(Table Ill). Diura bicaudata were taken in<br />

lakes and their outlets at higher altitudes,<br />

and Dinocras cephalotes was taken in a stream<br />

at Suldal. The total number of species in the<br />

southern part of West Norway is 20, since<br />

lsoperla difformis was taken at Oltedal,<br />

]

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