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Hajla Guide

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Use this Region Guide to easily find and compare Crags.

Table of contents

1. Hajla 0 routes in Region

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Mt Hajla is situated in the very east of Montenegro within the municipality of Rožaje. In the broader geographical sense Mt Hajla can be regarded as the part of the north-eastern Prokletije; it spreads along the boarder of Serbia (Kosovo and Metohia) and Montenegro, more precisely, it lies between the source of the Ibar River and Rugovska klisura(gorge) in Kosovo. The relief is characterised by numerous peaks with the elevation of over 2000masl, canyons and gorges of the mountain rivers, numerous and picturesque coniferous forests and mountain pastures. The highest peak of Mt Hajla, 2403masl, is situated at the bare rocky ridge. In terms of height and beauty, a prominent peak is Ahmica Peak(2271masl )as well. Mt Hajla, although one of the fairly high mountains in Montenegro, until the last few years hasn't been widely known and visited. Only with activation of mountaineering associations in Rožaje working on promotion of this gorgeous mountain, among other things, a mountain hut has been built, Hajla has become widely known and visited. On this mountain there are outstanding terrains for ski touring.

How to Get There and Accommodation

As the best starting point for a visit to this mountain we can recommend the town of Rožaje in the very east of Montenegro. Rožaje can be reached from the south, from the direction of Podgorica, along the main road towards Bijelo Polje, further on towards Berane where one should turn left to Rožaje. From Rožaje one should head towards the Bandžov katun at 1460 masl, where there is a mountain hut of the PAK Jelenčica(Mountaineering and Alpine Climbing Club). It is 9 kms away from Rožaje and in the summer it is possible to reach it by passenger car, too. Mountain hut Bandžov can be reached along the road Rožaje - Berane towards the west, after the suburb Suho polje to the first bridge (Dimiskin bridge) over the Ibar River, across the bridge to the left along the gravel road leading to the source of the Ibar River. When you reach the fifth bridge, you'll come across the information board Bandžov, across the bridge on the left. After a kilometre, on the left side you'll come across another small bridge over the stream flowing into the Ibar River, you'll cross it and continue further on to Bandžov. The hut is open all the time during the summer, while in the winter months you must inform them about your visit in advance. It has about thirty beds. There are electricity and water in the hut. It is possible to pitch tents here. Within the katun it is also possible to rent some of the privately owned wooden cottages or log cabins.

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1.1. North rock face of Mt.Hajla ridge 0 routes in Crag

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North rock face of Mt Hajla ridge is the biggest mountaineering/rock climbing potential on this mountain. The rocky ridge stretches almost 2 kms in width, while its height in the section below the highest peak is around 500 m. Due to its ruggedness, numerous steep and grassed gullies and couloirs it can be an attractive destination for winter alpine climbing, in particular, if one take into account that there are no ascended routes.

Approach and Descent.

The details of reaching the mountain hut at Bandžov have been already described. A marked mountain trail through the forest leads from the hut to the locality Grope - a meadow below the north rock face at around 1800 masl. Starting from the hut, it takes about 1.30 hours of moderate hike to reach Gropa, in which the abandoned katun is located. Descent is possible along the ridge following mountain markations in the direction of the east to the first ridge, and then one should descend from the ridge going towards Grope in the direction of the north.

Accommodation.

At above-mentioned mountain hut, or if you want to be closer to the crag in the tents on the meadows below the crag. The mountaineers from Rožaje have started building the new hut at Grope. The hut should be built by the end of 2009. By the abandoned 'flats'(cottages) where the new hut will be located there is a tapped (captured) karst spring-head called Studenac.

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