Kitakami Mountains, range in northeastern Honshu, Japan, in the Tōhoku region. It parallels the Pacific Ocean coast and extends southward for about 155 miles (250 km) from southern Aomori prefecture, through Iwate and Miyagi prefectures, to terminate in the Oshika Peninsula. The range has a maximum breadth of about 50 miles (80 km) and is nearly wedge-shaped. The highest peak, Mount Hayachine, rises to an elevation of 6,280 feet (1,914 metres) in the centre of the range.
The mountains of the Kitakami range are generally regarded as dissected erosion surfaces in step formation, the highest step level being about 2,950 feet (900 metres). Mount Hayachine and other protruding peaks support some alpine vegetation.
The western margin of the range descends to the valley of the Kitakami River, which flows longitudinally between the Kitakami and Ōu ranges. The eastern side of the Kitakami Mountains presents two main configurations: in the north the mountains are fringed by marine terraces some 980 feet (300 metres) high, while in the south the mountains have been drowned to form a greatly embayed coast. The southern coast is liable to severe damage by tsunamis, as was the case in the disaster of March 2011.
The Kitakami Mountain region is often referred to as the “Tibet of Japan” and is regarded as one of the pioneer fringes of Honshu. Until the mid-20th century, relics of old agricultural practices survived, including the serflike system known as nago. Rice has now replaced millet as the major crop, and the valleys are used for breeding dairy cattle. The southern part of the range is crossed by two railways running from the Pacific coast to the main rail lines in the Kitakami River valley.