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geographia - Studia

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V. SOROCOVSCHI, W. SCHREIBER, ŞT. BILAŞCO, CS. HORVATH<br />

The altitudes increase from the Someş Valley (the 200 m contour penetrates till<br />

Răstoci) to the Southern and Southwestern watersheds, where they remain at 500-600 m, only<br />

in some areas overpassing 600 m (Nadiş, 644 m, Mărului, 622 m, Râpa Şimişnei, 612 m etc.).<br />

The relatively high altitudes and especially the fragmentation density(52,7% from<br />

the total surface is described by values between 1,3 and 3 km/km 2 ) and depth (with dominant<br />

values between 100 and 150 m – 45,7% from the total surface and between 150 and 200 m –<br />

30,6%), determined a particular way to organize the geographic space.<br />

The radial-divergent orientation of the<br />

river network has repercussions on the road<br />

network configuration and on the settlements<br />

distribution in this subunit. The population<br />

density is reduced (20-30 inhab./km 2 ) and<br />

the settlements are situated along the main<br />

river valleys and rarely on the watersheds.<br />

Dejului Hills represent the central<br />

compartment of the studied area, lying<br />

between the watersheds of the Şimişna -<br />

Vad rivers, respectively Olpret to the North<br />

and Luna - Borşa to the South. To the East<br />

and Northeast it is bordered by the Someşul<br />

Mic Corridor, continued with the Someş<br />

valley between Dej and Vad, while to the<br />

West they come into contact with the central<br />

compartment of the Almaş – Agrij Depression.<br />

Within these boundaries, Dejului Hills<br />

occupy more than 34,9 % of the studied<br />

area. The maximal altitudes correspond to<br />

the structural remains preserved on the Dej<br />

tuff layers (the Hills of Bobâlna, 693 m,<br />

Fig. 1. The Geographic Subunits of the Southern<br />

Part of the Someşan Plateau.<br />

Făgetul, 602 m, Horgău, 595 m).<br />

The presence of the volcanic tuff is<br />

also underlined by the narrowing of some<br />

valleys (Lujerdiu, Mărului, Olpretului etc.),<br />

upstream of which different sized depressions have developed, facilitating the apparition of<br />

many small-sized settlements. From the Northern central part, the peaks decrease in altitude<br />

to East and Southeast where they remain frequently between 350 and 400 meters. The 350-<br />

450 altitudinal interval occupies almost half of the subdivisions (45,7 %) area.<br />

The main valleys are directed towards East and South, and the watersheds are<br />

larger than those in the Şimişna-Surduc Hills. The horizontal fragmentation values are reduced,<br />

grading between 0,5 and 2 km/km 2 (58,8 %). The vertical fragmentation values are also<br />

reduced, not exceeding 150 m in more than three quarters (83,4 %) of the subdivisions area.<br />

Clujului Hills, situated in the Southeast of the Someşan Plateau, develop between<br />

the Luna and Nadăş Valleys and represent 40,3 % of the studied area. The altitudes are<br />

generally decreasing from West to East and from South to North. The highest peaks, over<br />

600 m, correspond to the cuesta that dominates the Nadăş Valley (Lomb 682 m, Morunu,<br />

647 m, GurgueŃu Mare, 639 m).<br />

16

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