Pokhara valley extends, in the 'Oriental Realm', between the north parallels of 25⁰ 7’ and 28⁰ 10' and east meridians of 83⁰50' and 84⁰50'. Situated in the mountainous region of the southern Himalayas and trapped between the higher Himalayas in the north and Mahabharat range in the south, it occupies central position in the country. It valley spreads mainly over Kaski district and covers small portions of Tanahun and Syangja district from Pokhara, Tibetan border to the north is 72 kilometers and Indian border to the south is 78 kilometers. Within a small area the elevation ranges nearly from 500 meters to 3,000 meters in the Pokhara valley. 

Based on the administrative division on hierarchical order Pokhara lies in Western Development Region, Gandaki Zone and Kaski District. The valley includes Pokhara Sub‑Metropolitan City', Lekhnath Municipality, and some other Village Development Committees. The city is located in the central part of the valley.

ORIGIN OF POKHARA

The development of Pokhara valley and the origin of Annapurna range including the majestic peak Macchapuchhre is ascribed to Geological faulting in the 'Tertiary Period! (between 65‑25 million years ago from now). The convergence of Indian peninsula with Tibetan plate resulted into upsurge of Himalayas from the Tethys sea. After the upsurge of Annapurna range, due to the action of climatic components, glaciers started eroding mountains. The eroded materials ‑ limestone, gneiss and quartzite ‑were transported downwards depositing larger and coarser debris first and smaller as well as smoother debris later. Therefore the northern region of Pokhara has thicker layer of coarser and larger boulders but this thickness decreases southward and smoothness and size reduction occurs gradually. In this way, the tectonic valley was developed due to the hauling of debris as moraine and subsequent deposition as lake deposit.

GETTING INSIDE POKHARA

Pokhara, now‑a‑days, is linked to the major cities of Nepal by air and road transportation. Aeroplanes of different airlines fly several times a day from Kathmandu to Pokhara and many times a week from other major cities of the country. All the cities of Nepal where motoring has been possible so far, are linked to Pokhara by roads and regular bus services are available.

Pokhara is the only city in Nepal which is famous for the Himalayan Peaks and the Annapurna Himalayan Range. Some of the Famous Mountains that can be seen from Pokhara are Mt. Machhapuchree, Mt. Dhaulagiri, Mt. Annapurna, Mt. Hinchuli etc. it is the only City in Nepal that consist of seven beautiful lakes. Some of the famous lakes are Fewa Lake, Begnas Lake and Rupa Lake. It is the only City in Nepal that has excellent and breath taking caves. There are more then 5 caves within this city. Some of the most popular caves are Mahendra cave, Bat cave, Kali khola cave, Shiva cave etc.

Pokhara is the only City that has several rivers flowing within itself. Some of the major rivers that flow within this beautiful city are Seti, Yamdi, Mardi, Kali Khola, Madi etc. This City must be God's idea of heaven. Pokhara is so rich in Natural vegetation and excellent climatic conditions. It is neither too hot nor too cold. It seems to be a paradise.

CLIMATE

Pokhara experiences humid sub‑tropical to warm temperate climate. The climate of Pokhara valley is basically the influence of topography. Yearly mean temperature of the city (827m) is 20.8⁰C whereas monthly averages are ‑ maximum 25.5⁰C (During July and August) and minimum 13.2⁰C (during January). The deviation of temperature from mean value is also interesting: absolute maximum temperature is 37.4⁰C and absolute minimum temperature 2.4⁰C. Average annual rainfall recorded in Pokhara city is 3,755mm while 5,337mm is recorded in Lumle (a village nearby Pokhara city). Pokhara receives both monsoon and winter rains. It is important to note that profound effect of micro‑climatic elements on climatic parameters is clearly observable around Pokhara. Sunshine hours in Pokhara is estimated to be nearly six hours a day on an‑annual average. From June to August, monsoon clouds may create problems to view and photograph the mountains. Rest of the months are almost cloud free but November to March is the best time to avoid this problem. The annual average high wind speed recorded at Pokhara is 4 km per hour from February to June. The air is generally humid throughout the year with 80.16% relative humidity on yearly average. The relative humidity is found to be low in March and high in April.

The climate 'is neither too cold nor too hot Hence, from climatic point of view, Pokhara is enjoyable all year round. However, to visit higher Himalayas northern of Pokhara, especially for trekkers the best period is February to April.