Philippines History

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History of the Philippines and United Kingdom

History of the Philippines

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ASEAN, international organization established by the governments of Indonesia, Malaysia, the Philippines, Singapore, and Thailand in 1967 to accelerate economic growth and promote peace and security in Southeast Asia. Brunei joined in 1984, followed by Vietnam in 1995, Laos and Myanmar in 1997, and Cambodia in 1999. East Timor has been granted observer status and is expected to become a full member in 2025. The ASEAN region has a population of more than 700 million, covers a total area of 1.7 million square miles (4.5 million square km), and had a combined gross domestic product of $3.62 trillion as of 2022. Since its establishment, ASEAN has substantially enhanced security and stability throughout Southeast Asia, while also promoting economic growth and cooperation on international issues. Yet certain regional issues remain divisive within ASEAN, such as Myanmar’s civil war, which has proved challenging for the bloc to address uniformly, and relations with China, particularly with regards to economic ties and territorial disputes in the South China Sea. ASEAN’s history ASEAN's 50th Summit ASEAN's 50th SummitDelegates from Southeast Asian nations gather at the 50th ASEAN Summit in Melbourne, March 2024. ASEAN’s origins can be traced back to earlier regional organizations such as the Southeast Asia Treaty Organization (SEATO), founded in 1954, and the Association of Southeast Asia (ASA), established in 1961. These early efforts, however, were limited in scope and membership. In 1967 ASEAN was established by Thailand, Indonesia, Malaysia, the Philippines, and Singapore with the signing of the ASEAN Declaration in Bangkok. The initial aim was to encourage regional cooperation and create a collective front against the spread of communism in Asia, reflecting the geopolitical concerns of the era. Lee Kuan Yew Lee Kuan YewPrime Minister Lee Kuan Yew of Singapore at the Third ASEAN Summit, 1987, in Manila. The organization gained a new level of cohesion in the mid-1970s following the Vietnam War. ASEAN’s first summit meeting, held in Bali, Indonesia, in 1976, resulted in several significant agreements, including the signing of the Treaty of Amity and Cooperation. The end of the Cold War and increased regional development and stability saw ASEAN expand its membership, incorporating Brunei, Vietnam, Laos, Myanmar, and Cambodia by the end of the 1990s. This period also marked a shift toward deeper economic integration, exemplified by the establishment of the ASEAN Free Trade Area (AFTA) in 1992 and the response to the 1997 Asian financial crisis with the Chiang Mai Agreement. The adoption of the ASEAN Charter in 2007 provided a legal and institutional framework defined by three core pillars: the ASEAN Economic Community, the ASEAN Political-Security Community, and the ASEAN Socio-Cultural Community. This structure has helped promote increased cooperation and mutual understanding, despite enormous differences in the political structures, cultural backgrounds, and development levels of member states.

People of Southeast Asia By the late 20th century, Southeast Asia’s population (including Indonesia and the Philippines) was approaching a half billion, or about one-twelfth of the world’s total. This population, however, was unevenly distributed within the region. By far the nation with the largest population was Indonesia, with about two-fifths of the regional total; in contrast, Brunei’s population was only a tiny fraction of that. Nearly half of the regional population was accounted for by the mainland states, with Vietnam and Thailand being the most populous. Settlement patterns Southeast Asia is predominantly rural: three-fourths of the people live in nonurban areas. Moreover, population is heavily clustered in fertile river valleys and especially in delta areas, such as those of the Mekong and Irrawaddy rivers. Historical, cultural, and environmental influences also have affected the settlement patterns. Java and other core areas such as the Bangkok (Thailand), Hanoi, and Manila metropolitan areas contain high population densities. While the rate of urbanization in Southeast Asia is relatively low compared with those of other developing regions, it is increasing rapidly. Singapore is unique in that it is essentially totally urban. In addition, the Philippines has a much higher than average level of urbanization, in part because of its Spanish and American colonial history. The largest cities—Jakarta (Indonesia), Bangkok, and Manila—are among the world’s most populous. The growth of cities of all sizes is being fueled primarily by natural increase, but rural-urban migration also is a significant contributor. Rural dwellers continue to be attracted by the promise of employment and other opportunities, but for many migrants the informal (undocumented) economic sector in these large cities is the only hope for some form of employment. Settlement patterns in rural areas tend to be associated with agricultural practices. Shifting cultivation is still common in some parts of the region (notably the remote interior areas of Myanmar, Vietnam, and the island of Borneo), although the amount of land so utilized is gradually shrinking. The village is the unit of settlement and often functions collectively, and typically it is moved from time to time. By contrast, wet-rice cultivation, the dominant form of agriculture in Southeast Asia, is sedentary and results in relatively large rural agglomerations with well-developed village life and customs. Dry and upland farming often produces scattered homesteads. Population resettlement to provide agricultural employment and access to land is important in some Southeast Asian countries, notably Indonesia, Malaysia, and Vietnam. By far the largest program has been conducted in Indonesia, where more than four million people have been voluntarily resettled from Java and Bali to the less populated islands. Despite considerable success, the program has been plagued by such problems as improper site selection, environmental deterioration, migrant adjustment, land conflicts, and inadequate financing. A program in Malaysia also has been quite successful, in part because it has set much smaller resettlement targets and has been better funded. Vietnamese development policy also has utilized the resettlement of people in an effort to revitalize areas outside the major population centres.

Volcanic Eruptions Earthquakes are sometimes used in predicting volcanic eruptions. An earthquake alerts the authorities to observe a nearby volcano. When a volcano shows signs of eruption, evacuation of the nearby villages should be immediately implemented Active volcanoes are the ones that are usually closely monitored by volcanologists These are commonly located along plate boundaries specifically along the Pacific Ring of Fire. The Philippines is one of the countries that have a lot of volcanoes. The Pacific Ring of Fire is a region in the Pacific where most active volcanoes are located. The dots in the figure represent the active volcanoes in the world. Active volcanoes are those that have a recorded volcanic eruption in their history. There are two types of volcanic eruptions depending on the magma composition: the explosive type and the Hawaiian or nonexplosive type. The types of eruptions depend on the viscosity and amount of dissolved gases in a magma. Explosive eruptions have magma that is highly viscous and contains large amounts of dissolved gases. On the other hand, the Hawaiian type or nonexplosive eruptions have magma that has low viscosity and low amount of dissolved gases. Viscosity determines the ability of magma to flow. The lower the viscosity, the easier it is for the magma to flow. This viscosity of the magma is affected by silica content and temperature. Low-temperature magma with high silica content are highly viscous, high-temperature magma with low silica content has low viscosity. Therefore, in explosive eruptions, the magma could not easily get out of the vent. This impedes the remaining magma below, causing an increase of pressure. Once the pressure is released. an explosive eruption occurs. Volcanic Hazards Explosive volcanic eruptions release pyroclastic flows and materials that are considered to pose the greatest threat. The pyroclastic flows often render people in a shock state since they become overwhelmed with what they are seeing Too much pyroclastic material (eg., tephra), may bury people and severely damage the agricultural land and livestock. Damaged agricultural land could lead to famine. After an eruption, pyroclastic materials that have settled along the slope of the volcano get mixed with rainwater. This would start a mudflow or lahar moving at high speed, destroying everything along its path. Poisonous gases are also released by volcanoes. These gases can be lethal to people, animals, and plants. Just like earthquakes, violent volcanic eruptions may also happen underwater, which can trigger a tsunami.

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