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Until now, the kingdom of Ternate has existed for more than 750 years. In the age already so old, Sultanate of Ternate still standing, though its existence is no more than a mere symbol. Position sultan now has no authority, but remains influential in the community. Sultan of Ternate today are Drs. Hi. Mudaffar Sjah, BcHk. (Mudaffar II) who was crowned in 1975, and was the 49th sultan.
At the time of its inception, the power of the kingdom of Ternate only cover a few villages on the island of Ternate. Along with the development, the more advanced Ternate and reaches its apex in the 16th century. At that time, the power of the kingdom of Ternate covers an area of ​​ Maluku, North Sulawesi, East and Central, East Nusa Tenggara, South Filipinos Islands (Mindanao) and the Marshall Islands in the Pacific.
5. Governance Structure.
As described above, at its inception, the kingdom of Ternate is just a collection of several villages. At that time, the head kampungya called Momole. When the villages are united to form an empire, its leaders called Kolano (king). When Islam began to spread throughout the archipelago and the King of Ternate later converted to Islam, his Kolano replaced by the sultan. Kolano first took the title of Sultan Zainal Abidin is. Since then, the supreme leader is the sultan of Ternate. Furthermore, because the royal use of Islamic law, then, scholars also plays an important role.
To assist the Sultan perform royal duties, and also established the position Jogugu (prime minister) and the Advisory King called the Fala Raha (four houses). Fala Raha is a representation of the four noble clans who became the backbone of the Sultanate of Ternate. It could be said that, Fala Raha actually four momole replacement in the period before the arrival of Islam. Each led by a Kimalaha secret. Among Kimalaha are: Marasaoli, Tomagola Tomaito and Tamadi. The high court officials from four of these clans. If the sultan did not leave heirs, then his successor is selected from one of these four clans. Other positions are established to assist the task of the sovereign is Bobato Nyagimoi (Council 18), Sabua Raha, Capita Lau, Salahakan and Sangaji.
6. Social Life Culture.
Ternate is an area known for spice. The farming population are those who live in the hill area, they planted cloves, nutmeg, cinnamon and walnuts. Cloves from Ternate is famous for good quality. In areas rather low, people plant oil. People who live near the coast are also many who became a fisherman. In addition to farmers and fishermen, the people of Ternate also many became merchants. Ternate is the main meal of rice, sago or manioc (cassava), which is specially processed, known by the name huda, shaped like the slices of bread. Of cassava, people also make papeda Ternate. Rice is consumed by people originating from the island of Halmahera Ternate, Makassar and Manado.
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Prostitute in Tidore

The Global Volcanism Program has no activity reports for Tidore.
The Global Volcanism Program has no Weekly Reports available for Tidore.
The Global Volcanism Program has no Bulletin Reports available for Tidore.
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
Andesite / Basaltic Andesite.
Oceanic crust (< 15 km)
The Tidore volcanic complex consists of two dramatically different volcanic structures. The beautifully conical Kiematabu peak on the south end of Tidore Island is the highest volcano of the North Maluku island chain west of Halmahera. The broad, lower Sabale on the north side of the island is a caldera containing two cones. Maitara Island, 1 km off the NW coast, forms another volcanic construct. Tidore was mapped as Holocene by Apandi and Sudana (1980).
The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography.
Apandi T, Sudana D, 1980. Geologic map of the Ternate quadrangle, north Maluku. Geol Res Devel Centre Indonesia , 1:250,000 scale map and 9 p text.
Morris J D, Jezek P A, Hart S R, Gill J B, 1983. The Halmahera Island arc, Molucca Sea collision zone, Indonesia: a geochemical survey. In : Hayes D E (ed) The Tectonic and Geologic Evolution of Southeast Asia Seas and Islands, part 2, Amer Geophys Union, Geophys Monogr , 27: 373-387.
The Global Volcanism Program is not aware of any Holocene eruptions from Tidore. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Tidore page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

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