What can I offer for the country where are mountains cover 93 percent of surface area? Of course the mountains!

Tajik National Park (2,611,674 ha in area) encompasses almost the entire Pamir Mountains, the third highest mountain ecosystem in the world after the Himalaya and Karakorum Mountains. The Pamir Mountains lie at the centre of the ‘Pamir Knot’, the term used by geographers to describe the tangle of the highest mountain ranges on the Eurasian continent. Huge tectonic forces stemming from the collision of the Indian-Australian plate with the Eurasian Plate have progressively thrown up the Himalaya, Karakoram, Hindu Kush, Kunlun and Tien Shan – all radiating out from the Pamir Mountains. Along with the Karakoram Mountains, the Pamir region is one of the most tectonically-active locations in the world.

Tajik National Park is one of the largest high mountain protected areas in the Palearctic Realm. The Fedchenko Glacier, the largest valley glacier of the Eurasian Continent and the world’s longest outside of the Polar Regions, is unique and a spectacular example at the global level. The visual combination of some of the deepest gorges in the world, surrounded by rugged glaciated peaks, as well as the alpine desert and lakes of the Pamir high plateaux adds up to an alpine wilderness of exceptional natural beauty. Lake Sarez and Lake Karakul are superlative natural phenomena. Lake Sarez, impounded behind the highest natural dam in the world, is of great geomorphic interest. Lake Karakul is likely to be the highest large lake of meteoric origin.

In 2008, the national park was submitted to UNESCO with a view to becoming a World Heritage Site. In 2013, the park was accepted as World Heritage

The three highest mountains in the Pamirs core are Ismoil Somoni Peak (known from 1932 to 1962 as Stalin Peak, and from 1962 to 1998 as Communism Peak), 7,495 m (24,590 ft); Ibn Sina Peak (still unofficially known as Lenin Peak), 7,134 m (23,406 ft); and Peak Korzhenevskaya (Pik Korzhenevskoi), 7,105 m (23,310 ft). In the Eastern Pamirs, China's Kongur Tagh is the highest at 7,649 m (25,095 ft).

Ismoil Somoni Peak is the highest mountain in Tajikistan. Because it was within the territory of the former Russian Empire and the former Soviet Union, it was the highest mountain in the Russian Empire and Soviet Union before Tajikistan became independent. The mountain is named after Ismail Samani, a ruler of the Samanid dynasty. It is located in the Pamir Range.

Lenin Peak or Ibn Sina (Avicenna) Peak, rises to 7,134 metres (23,406 ft) in Gorno-Badakhshan (GBAO) on the border of Tajikistan and Kyrgyzstan, and is the second-highest point of both countries. It is considered one of the less technical 7000 m peaks in the world to climb and it has by far the most ascents of any 7000 m or higher peak on Earth, with every year seeing hundreds of mountaineers make their way to the summit. Lenin Peak is the highest mountain in the Trans-Alay Range of Central Asia, and in the Pamir Mountains in Tajikistan it is exceeded only by Ismoil Somoni Peak (7,495 m). It was thought to be the highest point in the Pamirs in Tajikistan until 1933, when Ismoil Somoni Peak (known as Stalin Peak at the time) was climbed and found to be more than 300 metres higher. Two mountains in the Pamirs in China, Kongur Tagh (7,649 m) and Muztagh Ata (7,546 m), are higher than the Tajik summits.

Peak Ozodi (until 2020 Korzhenevskoi) is the third highest peak in the Pamir Mountains of Tajikistan. It is one of the five "Snow Leopard Peaks" in the territory of the former Soviet Union. It is named after Evgenia Korzhenevskaya, the wife of Russian geographer Nikolai L. Korzhenevskiy, who discovered the peak in August 1910.

The Pamir Mountains are a major centre of glaciation on the Eurasian continent and Tajik National Park illustrates within one protected area an outstanding juxtaposition of many high mountains, valley glaciers, and deep river gorges alongside the cold continental desert environment of the high Pamir Plateau landforms. An outstanding landform feature of the property’s geologically dynamic terrain is Lake Sarez. It was created by an earthquake-generated landslide of an estimated six billion tonnes of material and is possibly the youngest deep water alpine lake in the world. It is of international scientific and geomorphological hazard significance because of the on-going geological processes influencing its stability, and the sort of lacustrine ecosystem which will develop over time. Tajik National Park furthermore offers a unique opportunity for the study of plate tectonics and continental subduction phenomena thereby contributing to our fundamental understanding of earth building processes.