What is the area of Balikpapan?

What is Balikpapan's population?

The population of Balikpapan is 639,031.

When was Persiba Balikpapan created?

Persiba Balikpapan was created in 1950.

Where is the dawn service in balikpapan?

Currently at Chevron complex..with gunfire breakfast at Novetel

Average sunlight a year in Balikpapan?

Probably around 30 and 20 degrees Celsius

Where is Balikpapan Indonesia in relation to Bali Indonesia?

Balikpapan is a city in Kalimantan ( Borneo ) Island, the largest island in Indonesia archipelago, while Bali is the name of Bali Island . Indonesia is archipelago country. Both Bali and Kalimantan are parts of Indonesia

Balikpapan, Indonesia?

Once a rural fishing village, Balikpapan, Indonesia, has experienced explosive growth in recent years due to the petroleum industry, and is now an economic center and a hub of travel for the entire region. From here it is possible to travel into deeply forested regions where indigenous people live a traditional life. Along the way, travelers can also see the wildlife of Borneo in its natural setting. North of the city lies the Sungai Wain Protection Forest containing many wild species unique to Borneo. From Balikpapan, travelers can take a cruise down the Mahakam River to see untouched corners of the island, and only a short drive from Balikpapan is the Samboja Lodge Project, where native plants and animals grow in lush profusion. Balikpapan is also the starting point for forest treks that allow visitors to stay at local homes and see a lifestyle unchanged for centuries. Balikpapan is the gateway to the wilds of Borneo, land full of wonders.

When was Cees Fasseur born?

Cees Fasseur was born on December 11, 1938, in Balikpapan, Indonesia.

When was Marisa Haque born?

Marisa Haque was born on October 15, 1962, in Balikpapan, Indonesia.

When was Jodi Ann Paterson born?

Jodi Ann Paterson was born on July 31, 1975, in Balikpapan, Indonesia.

Where is balikpapan?

Balikpapan is a seaport city on the eastern coast of the island of Borneo, Indonesia, in the East Kalimantan province, a resource-rich region well known for its timber, mining, and petroleum export products. Two harbors, Semayang and Kariangau (a ferry harbour), and the Sepinggan International Airport are the main transportation ports to the city.

How far is it from Jakarta Indonesia to balikpapan Indonesia?

The distance between Jakarta, Indonesia and Balikpapa, Indonesia is about one and a half hours or two hours if you go there by plane. According to Tiket2, Garuda, Citilink and other Indonesian airlines make it in 2h 5m.

Balikpapan coal formation and other coal formation caparision?

East Kalimantan GeologyNumerous Tertiary, hydrocarbon bearing basins occur around the periphery of Borneo (Hutchison, 1989). A large portion of East Kalimantan is covered by the Kutei Basin. The Kutei Basin is the largest (160000 square kilometres) and deepest (12000 to 14000 metres) Tertiary basin in Indonesia.Formations of the Kutei Basin are essentially a succession of eastward prograding deltas. The stratigraphic succession around the tenement area is summarised in below Tables. Formations developed within the tenement area are highlighted in yellow.Stratigraphy of the Samarinda QuadrangleAgeFormationLithologyThicknessUpper Middle MioceneBalikpapan Formation (Tmbp)Alternating quartz sandstone, silty claystone and shale with intercalations of marl, limestone and coal. Deposited in a littoral to shallow marine environment. Conformably overlies the Paulua Balang Formation.800 mMiddle MiocenePaulau Balang Formation (Tmpb)Alternating quartz sandstone, sandstone and claystone with intercalations of coal seams. Deposited in a shallow sublittoral environment. Conformably overlies the Bebuluh Formation.900 mEarly MioceneBebulu Formation (Tmbl)Limestone with intercalations of claystone and marl. Shallow marine environment.Late Oligocene to Middle MiocenePamaluan Formation (Tomp)Claystone and shale intercalated with marl, sandstone and limestone. Deposited in deep sea environment.1500 - 2500 mEarly EoceneKuaro Formation (Tek)Sandstone and conglomerate. Intercalations of coal, shale, marl and limestone. Shallow marine environment.700 mLate CretaceousHaruyan Group (Kvh)Lava, breccia and tuff. Lava basaltic.Early CretaceousPintap Formation (Ksp)Flysch deposits. Alternating sandstone, claystone, siltstone, shale, limestone and basaltic lavas. Deposited in arc trench gap area.