Dush Cave

In Mirusha Canyon special forms have been created: deepening, caves, rock cuts, deposition of materials, lakes etc. In addition to the characteristic formations of waterfalls and lakes, there are also caves of various shapes and sizes. Some of the most interesting caves are the Great Cave and the Little Church Cave, the Cave on the Tenth Lake, the Cave on the Ninth Lake divided into two channels (left channel and right channel), the cave behind the Ninth Lake, and the Cave on the 9th. Shower etc. The Cave of Dush is the most interesting and important about the natural values ​​in the whole area of ​​Mirusha Park. The permeable cave length is 180 m. It should also be mentioned that the cave has two secondary channels of 40 m, so with the secondary channels the total length of the cave goes to 260 m. The entrance to the cave is quite impressive with a width of 10 m and a height of 15 m. Inside the cave up to 72 meters, in the north direction lies the canal about 40 m long, while in the south-east direction the cave is passable through the meandrin channel up to 180 meters. At 180 meters, the secondary channel connects to the main cave channel and the other secondary channel to the southwest. Here too the cave ends in the form of "S" and is not passable. Inside the cave there are six small lakes created during erosive activity and waterfalls up to 2-5 m high. It is rich in stalactites, stalagmites and columns of various shapes and sizes, with a large number of sticks living inside.

Livoq Lake

Livoq Lake  is a small artificial lake in eastern Kosovo. Livoqi Lake lies west of the town of Gjilan and near the Gollak Mountains. The lake is supplied with water from a small Morava branch of Binça (South Morava). It is the second largest lake, east of Kosovo, after Prilepnica Lake.

Badovc Lake

Badovc Lake is located 2 km from settlements such as Hajvalia and Gracanica and 5 km from Pristina. This lake is an artificial reservoir supplied by the Gracanica River. It is one of the main reservoirs in Kosovo for the use of potable water and which supplies Pristina and its surroundings with water.

Radoniq Lake

Radoniq Lake is an artificial lake in Gjakova municipality. Created in the 1980s, the lake received the name of the village which was reversed for its creation. Radoniqi supplies about 214,000 inhabitants of the cities of Gjakova / Djakovica and Rahovec / Orahovac as well as surrounding villages. It is also used for irrigation of 10,500 ha of land. With an area of ​​5.62 km2, Radoniqi occupies the second place in Kosovo in terms of surface area. The dam's capacity is 113 million m3, which currently allows for reasonable water supply throughout the year.

Ujmani Lake

Gazivoda Lake or Gazivode Lake, is an artificial lake in Serbia and Kosovo. Gazivoda Lake has an area of 11.9 km² of which 9.2 km² reside in Kosovo's territory and 2.7 km² in Serbia's territory. The lake is formed by the damming of the Ibar River, which flows into the lake.  

Batllava Lake

Batllava Lake is an artificial lake built in the 70's. This lake is located in the village of Batllava, Podujevo municipality. The function of this lake is the supply of potable water to Pristina and Podujeva municipality. This is also Kosovo's main water supply. Today this lake is also used for summer vacations, refreshments, fishing, relaxation in various restaurants etc.      

Radavc Cave

The cave is located near the village of Radac, near the source of the White Drin, about 11 kilometers from the town of Peja, to the left of Peja-Rozaje Road. The cave entrance is oriented north-east with dimensions of 2.80 m high and 2.20 m wide with a narrow tunnel-shaped corridor of 2.50 m long. The cave is illuminated by a natural window located at the top of it. The entrance of the cave is located at an altitude of 578 m. Radac cave is also distinguished in the "architectural" aspect because it is presented as a residential object created by nature. The first announcement of this cave was made by the researcher J. Petrovic. Archaeologist M. Garashanin considers this cave as a safe place for the Paleolithic era. The cave is of particular importance, as there are indications of the Paleolithic period, so there should be a special treatment because traces of the stone age, namely the Paleolithic, have not yet been confirmed in our country.

Marble Cave

Marble Cave is located in Gadime village near Lipjan, Kosovo it is 1500 meters long. But for tourists it is only possible to see the first 1,300 meters of the cave, since the rest of the cave is not yet accessible. During the summer the temperature inside the cave is constant 13 degrees Celsius and in winter it is 11-13 degrees.

Kopaonik

Kopaonik (known as Kopaonik Mountain) is a high mountain mass that extends from northwest to southeast with a length of about 75 km, reaching between about 40 km in the territory of Serbia and northern Kosovo. the lowest peak of the Kopaonik is the Panchic Peak (Argentine Peak) with 2017 m altitude, which is also the northernmost point of the territory of Kosovo.

Karadag Mountains

The Karadag Mountains, often known as the Skopje Karadag, extend from the Kacanik Gorge, namely the Lepenc River to the west and the Koncul Gorge to the Morava e Binca River in the south-east, about 50 km long, between Anamorava. to the north, the Presevo Valley to the south-east and the Skopje Plain to the south. The relief structure is quite fragmented. This is done by the river valleys as the lower parts and the peaks of the mountains as the highest parts of the relief. New sediments in the west, mesozoic in the middle and old paleozoic in the east indicate a variety in geological construction. The flow of the rivers that gave this part a broken structure has been influenced by the formation of the relief. Descending from the high areas, they have deepened their beds and carried eroded material with them. The most important rivers of this province are: Golemareka, Letnica, Karadak, Lashtica, Pasjani, Llapushnica etc. They all spill into the Morava of Binca.

Pashtrik

Pashtrik , is a mountain located in Kosovo and Albania. Its highest peak is located on their mutual border, it is also called Paštrik and it is 1,986 m (6,516 ft) high. The White Drin river passes along by it. Two-thirds of the mountain belongs to Albania. It is located in north-eastern Albania. The village of Krumë is positioned next to it. One-third of the mountain is in Kosovo. It is located in south-western Kosovo. The village of Gjonaj is positioned next to the mountain. It was built from Paleozoic core, covered by Mesozoic limestone, mostly under the vegetation. Small mammals living in the mountain include the common vole, northern white-breasted hedgehog, balkan mole, and european mole. The blind mole occurs in the grasslands in old growth stands of beech forest.

Sharr Mountains

They lies in the South-East of Kosovo starting from the vicinity of Prizren and go steeply with peaks or rows of pyramids lined up one after another or as it was called from antiquity the Illyrian people, the peaks of the saw, of resemblance to the saws, form consecutive characteristic images in the heart of the Balkans. The Sharr Mountains have been known since antiquity in documents of various authors, since the 5th century BC. named after Mont Skardus, of Herodotus, who also describes the Illyrian tribes and their restrictions.