Lakki Marwat (, ) is a district in Bannu Division of Khyber Pakhtunkhwa province in Pakistan. It was created as an administrative district on July 1, 1992, prior to which it was a tehsil of Bannu District. Geography The district is located in the southern part of Khyber Paktunkhwa. It borders Karak, Bannu and South Waziristan districts to the north, Tank district to the west, Dera Ismail Khan district to the south, and Mianwali district of Punjab to the west. The district is a combination of hills and sandy plains. The hilly areas are along the boundaries of the district especially in the east, southeast, southwest and northwest. In the southeast, the Marwat range separates Lakki Marwat from Dera Ismail Khan District while in the east the Karak Niazi range separates it from Mianwali District. It is surrounded by Baittani range on the west and southwest, which separates it from Tank District and South Waziristan Agency. The Marwat range culminates and Baittani ranges starts near Sheikh Badin. The general elevation of these hills ranges from 500 to 1000 meters above sea level. The land beyond these hills gradually slopes to the central part, which looks like a basin. A large number of streams flow from the surrounding hills, the Kurram river flows through the district from North West to the south east and joins the Indus River south of Isakhel town. One of its important tributary is Gambila River, also known as the Tochi. The major part of this basin is an alluvial plain. The northern portion of this plain is situated chiefly in the Kurram Gambila Doab and irrigated by Kurram River. It is a flat sandy area. The southern part is made up of undulating dunes of sand, furrowed at regular intervals by deep torrent beds which carry the drainage of the Marwat and Baittani ranges to the Gambila. It is good for cultivation, water table is quite deep below the soil surface. In the western portion of the district, the soil is fairly stiff clay covered by a layer of stones at the foot of the hills. The whole district is intersected by numerous hill torrents and deep ravines. The general elevation of the plain area is about 200 to 300 meters above sea level. Climate The region has all the characteristics of a desert due to its sand dunes, scorching heat and dry weather. Summers are