- published: 07 May 2013
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The Kaḷinga architectural style (Oriya: କଳିଙ୍ଗ ସ୍ଥାପତ୍ୟକଳା) is a style which flourished in the ancient Kalinga region or present eastern Indian state of Orissa and northern Andhra Pradesh. The style consists of three distinct types of temples: Rekha Deula, Pidha Deula and Khakhara Deula. The former two are associated with Vishnu, Surya and Shiva temples while the third is mainly with Chamunda and Durga temples. The Rekha Deula and Khakhara Deula houses the sanctum sanctorum while the Pidha Deula constitutes outer dancing and offering halls.
In Kalinga, the ancient land of Sakta cult, divine iconography existed since the mythological era. Present day research implies that idols (deities) were placed under auspicious Trees in the ancient days. And maybe today a Temple in general carries various minute details and the overall shape of some heritage tree. The various aspects of a typical Kalinga Temple include Architectural stipulations, Iconography, historical connotations and honoring the traditions, customs and associated legends.
Kalinga (Tagalog pronunciation: [kɐˈliŋɐ]) is a landlocked province of the Philippines in the Cordillera Administrative Region in Luzon. Its capital is Tabuk and borders Mountain Province to the south, Abra to the west, Isabela to the east, Cagayan to the northeast, and Apayao to the north. Prior to 1995, Kalinga and Apayao used to be a single province named Kalinga-Apayao, until they were split into two to better service the needs of individual native tribes in the provinces.
Kalinga is subdivided into 1 city and 7 municipalities. Tabuk was proclaimed a component city in 2007, but in November 2008 the Supreme Court of the Philippines ruled that its cityhood was unconstitutional. However, Tabuk had its city status reinstated by the Supreme Court on December 22, 2009.
The topography of Kalinga province is rugged and sloping with mountain peaks ranging from 1,500 to 2,500 metres (4,900 to 8,200 ft) in elevation. The province’s geographic feature on the western portion is characterized by sharp crested interlinking peaks of steep slopes, isolated flatlands, plateaus and valleys. The eastern portion is generally rolling and gradually sloping foothills.