Geology of Indonesia active volcanoes formed Sumatra, Java, Bali, and Nusa Tenggara islands, most of which, particularly Java and Bali, emerged within the last 2–3 million years. The Pacific and Australian plate movements controlled the tectonics of the eastern portion of Indonesia. The tectonics processes in Indonesia formed major structures in Indonesia. The most prominent fault in the west of Indonesia is the Semangko Fault or the Great Sumatran Fault, a dextral strike-slip fault along Sumatra Island (about 1900 km). The formation of this fault zone is related to the subduction zone in the west of Sumatra. Palu-Koro fault is another major structural
Foreign aid to Indonesia Foreign aid to Indonesia US: $43 billion in International Monetary Fund (IMF) aid in 2004 was sent as foreign aid to Indonesia, and this assistance has traditionally been an important part of the central government’s budget. From 1967 to 1991, most aid was coordinated through the Inter-Governmental Group on Indonesia (IGGI) founded and chaired by the Netherlands; since 1992, without the Netherlands, the organization has been known as the Consultative Group on Indonesia (CGI). Although Indonesia terminated its IMF aid program in December 2003, it still receives bilateral aid through the CGI, which pledged US$2.8 billion in grants and loans