Intro PHILIPPINES

Total Page:16

File Type:pdf, Size:1020Kb

Intro PHILIPPINES 1. SLIDES 1,2,3,4 The Philippines is a sovereign island country in Southeast Asia in the western Pacific Ocean. To its north across the Luzon Strait lies Taiwan. West across the South China Sea sits Vietnam. The Sulu Sea to the southwest lies between the country and the island of Borneo, and to the south the Celebes Sea separates it from other islands of Indonesia. It is bounded on the east by the Philippine Sea. Its location on the Pacific Ring of Fire and its tropical climate make the Philippines prone to earthquakes and typhoons but have also endowed the country with natural resources and made it a diverse country. The Philippines is the 73rd largest independent nation in the world covering almost 300,000 square kilometers (115,831 sq mi) and an archipelago comprising 7,107 islands, and is categorized broadly into three main geographical divisions: Luzon, Visayas, and Mindanao. 2. SLIDE 5 Multiple ethnicities and cultures are found throughout the islands. Because of early settlement, the islands are influenced by Malay, Hindu and Islamic societies. Later Chinese settlement introduced Chinese cultural elements. The arrival of Ferdinand Magellan in 1521 marked the beginning of the Spanish colonization. A Spanish colony for more than three centuries and named after a 16th century Spanish king – the Philippines was taken over by the US in the early 20th century after a protracted rebellion against rule from Madrid. Spanish and US influences remain strong, especially in terms of language, religion and government. Self-rule in 1935 was followed by full independence in 1946 under a US-style constitution 3. SLIDE 6 You will fly into Manila, the capital city and the second largest city of the Philippines. Manilla is 800 miles from mainland Asia. It is one of the sixteen cities (along with the municipality of Pateros) that make up the National Capital Region called Metro Manila that has a population of 12 million. Manila has a total population of 1.6 million according to the 2010 census and is the second most populous city in the Philippines, behind Quezon City. The populace inhabits an area of only 38.55 square kilometers, making Manila the most densely populated city in the world. Bustling commerce and some of the most historically and culturally significant iconic landmarks in the country, as well as the seat of the executive and judicial branches of the government are found in the city. Manila is also home to many scientific and educational institutions, numerous sport facilities, and other culturally and historically significant venues. 4. SLIDE 7,8 One of the more famous modes of transportation in Manila is the jeepney. Patterned after MacArthur’s U.S. army jeeps, these have been in use since the years immediately following World War II. They have become the ubiquitous symbol of the Philippine culture. Another popular mode of public transportation in the country are the Tricycles, they are a common means of passenger transport in the country especially on rural areas. There are 124,240 miles of roads of which only 20% are paved. However, the road system in Manila Metro area is adequate although crowded. Of course, there are private cars (smaller models) and taxis similar to the US. 5. SLIDE 9,10,11,12 Food shopping is much like the US. The shops will depend on the neighborhood, ranging from traditional markets to supermarkets and hypermarkets in urban areas. The local markets in a big city or regional town are time crowded and colorful. The sellers, young or older, will welcome foreigners in their stall. They are always prepared for a friendly talk, even if you don't buy. The Philippines is one of the developing countries where the sellers don't molest a foreigner in an attempt to sell. Most of the Filipinos speak English, so communication is not a problem. 6. SLIDE 13,14,15 The climate in the area you are going to is very different than Wisconsin. There are are two seasons in the country, the wet season and the dry season, based upon the amount of rainfall. Based on temperature, the seven warmest months of the year are from March to October. May is the warmest month, and January, the coolest. The summer monsoon from the southwest brings heavy rains to most of the archipelago from May to October. Monsoon rains, although hard and drenching, are not normally associated with high winds and waves. The “trade winds” coming from the northeast dominates from December to May and bring little precipitation. At least 30 percent of the annual rainfall in the northern Philippines can be traced to tropical typhoons that occur in the period June- November. Relative humidity is high in the Philippines. A high amount of moisture or vapor in the air makes hot temperatures feel hotter. This quantity of moisture is due to different factors - the extraordinary evaporation from the seas that surrounds the country on all sides, to the different prevailing winds in the different seasons of the year, and finally, to the abundant rains so common in a tropical country. The least comfortable months are from March to May where temperature and humidity attain their maximum levels. The World Watch Institute (WWI) predicts that climate change will cause more heavy rainfall patterns and typhoons in the future. 7. SLIDE 16,17,18 One of the things in which a tropical country differs from countries of other climate zones, is housing. The architecture as well as the used construction materials, show a clear adjustment to the specific climate conditions. A more important aspect that influences the architecture is the financial position of the family. You can find living arrangements from the traditional Nipa hut (Bahay Kubo) of the indigenous people constructed of bamboo tied together and covered with a thatched roof of palm leaves. The Colonian Filipino house is a mixture of native Filipino, Spanish and Chinese influences. These stone houses had open ventilation and elevated apartments much like the Nipa hut. The Spanish colonial period brought with it the architecture of Europe along with the Roman Catholic religion. During the 20th century, the Americans constructed many Art Nouveaux Buildings in Manila. Today, the architecture is modern, although houses are considerably smaller than the US. Slumscan be found in all parts of the Philippines. SLIDE 19 A newly industrialized country, the Philippine economy has been transitioning from one based on agriculture to one based more on services and manufacturing. Of the country's total labor force of around 38.1 million, the agricultural sector employs close to 32% but contributes to only about 14% of GDP. Many citizens still live in rural areas and support themselves through agriculture. The country's agriculture sector is made up of 4 sub-sectors: farming, fisheries, livestock, and forestry. The main agricultural crops are rice, corn, coconut, sugarcane, bananas, pineapple, coffee, mangoes, tobacco, and abaca (a banana-like plant). The Philippines is the world’s largest producer of coconuts and pineapples and a large producer of sugar and rice. Secondary crops include peanut, cassava, camote (a type of rootcrop), garlic, onion, cabbage, eggplant, calamansi (a variety of lemon), rubber, and cotton. SLIDE 20, 21 Pork is the main animal product produced and consumed in the Philippines today. Like rice and chicken, it is one of the Philippines’s staple food products. Pork comprises about 59% of meat and poultry production in the Philippines. Imports account for less than 5% of consumption and are principally brought in to cover shortfalls in the local supply of lower-end and low-cost products for use by the food processing industry. Chicken is the second largest animal product . Cattle are for the most part Bos indicus type for meat, draft and milk although some dairies use European breeds. Caraboa, or water buffalo, are used for meat, draft and milk, They are well suited to the tropical environment. Duck meat and eggs are popular in the diet and account for 1.5% of the total animal production value. Dairy accounts for less than 1% of production and includes cattle, caraboa and goats. The Philippines has been identified as one of the next eleven by Goldman Sachs, as having a high potential of becoming the world’s largest economies in the 21st century. Currently the 45th largest economy in the world, the Philippines posted the highest GDP growth rates in Asia for the first two quarters of 2013. A youthful population, willing to adopt and develop new technology, bodes well for the future of the country. .
Recommended publications
  • The Plate Tectonics of Cenozoic SE Asia and the Distribution of Land and Sea
    Cenozoic plate tectonics of SE Asia 99 The plate tectonics of Cenozoic SE Asia and the distribution of land and sea Robert Hall SE Asia Research Group, Department of Geology, Royal Holloway University of London, Egham, Surrey TW20 0EX, UK Email: robert*hall@gl*rhbnc*ac*uk Key words: SE Asia, SW Pacific, plate tectonics, Cenozoic Abstract Introduction A plate tectonic model for the development of SE Asia and For the geologist, SE Asia is one of the most the SW Pacific during the Cenozoic is based on palaeomag- intriguing areas of the Earth$ The mountains of netic data, spreading histories of marginal basins deduced the Alpine-Himalayan belt turn southwards into from ocean floor magnetic anomalies, and interpretation of geological data from the region There are three important Indochina and terminate in a region of continen- periods in regional development: at about 45 Ma, 25 Ma and tal archipelagos, island arcs and small ocean ba- 5 Ma At these times plate boundaries and motions changed, sins$ To the south, west and east the region is probably as a result of major collision events surrounded by island arcs where lithosphere of In the Eocene the collision of India with Asia caused an the Indian and Pacific oceans is being influx of Gondwana plants and animals into Asia Mountain building resulting from the collision led to major changes in subducted at high rates, accompanied by in- habitats, climate, and drainage systems, and promoted dis- tense seismicity and spectacular volcanic activ- persal from Gondwana via India into SE Asia as well
    [Show full text]
  • Maritime Boundary Agreements 172 6.1 Introduction 172 6.2 Saudi-Bahrain 1958 Agreement 172 6.2.1 Historic Background 174 6.2.2 Boundary Delimitation 176
    Durham E-Theses Maritime boundary delimitation of the kingdom of Saudi Arabia a study in political geography Al-Muwaled, Faraj Mobarak Jam'an How to cite: Al-Muwaled, Faraj Mobarak Jam'an (1993) Maritime boundary delimitation of the kingdom of Saudi Arabia a study in political geography, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/10368/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk 2 MARITIME BOUNDARY DELIMITATION OF THE KINGDOM OF SAUDI ARABIA A STUDY IN POLITICAL GEOGRAPHY Fara.i Mobarak Jam'an AI-Muwaled The copyright of this thesis rests with the author. No quotation from it should be published without his prior written consent and information derived from it should be acknowledged. Thesis submitted for the Degree of Doctor of Philosophy in Social Science in the Department of Geography, Faculty of Social Sciences, University of Durham, U.K.
    [Show full text]
  • Geographic Names
    GEOGRAPHIC NAMES CORRECT ORTHOGRAPHY OF GEOGRAPHIC NAMES ? REVISED TO JANUARY, 1911 WASHINGTON GOVERNMENT PRINTING OFFICE 1911 PREPARED FOR USE IN THE GOVERNMENT PRINTING OFFICE BY THE UNITED STATES GEOGRAPHIC BOARD WASHINGTON, D. C, JANUARY, 1911 ) CORRECT ORTHOGRAPHY OF GEOGRAPHIC NAMES. The following list of geographic names includes all decisions on spelling rendered by the United States Geographic Board to and including December 7, 1910. Adopted forms are shown by bold-face type, rejected forms by italic, and revisions of previous decisions by an asterisk (*). Aalplaus ; see Alplaus. Acoma; township, McLeod County, Minn. Abagadasset; point, Kennebec River, Saga- (Not Aconia.) dahoc County, Me. (Not Abagadusset. AQores ; see Azores. Abatan; river, southwest part of Bohol, Acquasco; see Aquaseo. discharging into Maribojoc Bay. (Not Acquia; see Aquia. Abalan nor Abalon.) Acworth; railroad station and town, Cobb Aberjona; river, IVIiddlesex County, Mass. County, Ga. (Not Ackworth.) (Not Abbajona.) Adam; island, Chesapeake Bay, Dorchester Abino; point, in Canada, near east end of County, Md. (Not Adam's nor Adams.) Lake Erie. (Not Abineau nor Albino.) Adams; creek, Chatham County, Ga. (Not Aboite; railroad station, Allen County, Adams's.) Ind. (Not Aboit.) Adams; township. Warren County, Ind. AJjoo-shehr ; see Bushire. (Not J. Q. Adams.) Abookeer; AhouJcir; see Abukir. Adam's Creek; see Cunningham. Ahou Hamad; see Abu Hamed. Adams Fall; ledge in New Haven Harbor, Fall.) Abram ; creek in Grant and Mineral Coun- Conn. (Not Adam's ties, W. Va. (Not Abraham.) Adel; see Somali. Abram; see Shimmo. Adelina; town, Calvert County, Md. (Not Abruad ; see Riad. Adalina.) Absaroka; range of mountains in and near Aderhold; ferry over Chattahoochee River, Yellowstone National Park.
    [Show full text]
  • Origin of Marginal Basins of the NW Pacific and Their Plate Tectonic
    Earth-Science Reviews 130 (2014) 154–196 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Origin of marginal basins of the NW Pacificandtheirplate tectonic reconstructions Junyuan Xu a,⁎, Zvi Ben-Avraham b,TomKeltyc, Ho-Shing Yu d a Department of Petroleum Geology, China University of Geosciences, Wuhan, 430074, China. b Department of Geophysics and Planetary Sciences, Tel Aviv University, Ramat Aviv 69978, Israel c Department of Geological Sciences, California State University, Long Beach, CA 90840, USA d Institute of Oceanography, National Taiwan University, Taipei, Taiwan article info abstract Article history: Geometry of basins can indicate their tectonic origin whether they are small or large. The basins of Bohai Gulf, Received 4 March 2013 South China Sea, East China Sea, Japan Sea, Andaman Sea, Okhotsk Sea and Bering Sea have typical geometry Accepted 3 October 2013 of dextral pull-apart. The Java, Makassar, Celebes and Sulu Seas basins together with grabens in Borneo also com- Available online 16 October 2013 prise a local dextral, transform-margin type basin system similar to the central and southern parts of the Shanxi Basin in geometry. The overall configuration of the Philippine Sea resembles a typical sinistral transpressional Keywords: “pop-up” structure. These marginal basins except the Philippine Sea basin generally have similar (or compatible) Marginal basins of the NW Pacific Dextral pull-apart rift history in the Cenozoic, but there do be some differences in the rifting history between major basins or their Sinistral transpressional pop-up sub-basins due to local differences in tectonic settings. Rifting kinematics of each of these marginal basins can be Uplift of Tibetan Plateau explained by dextral pull-apart or transtension.
    [Show full text]
  • The Borderlands of Southeast Asia Southeast of Borderlands the That Comforting Ambiguity Has Disappeared
    Edited by James Clad, Sean M. McDonald, and Bruce Vaughn s an academic field in its own right, the topic of border studies is experiencing a revival in university geography courses as well as in wider political commentary. Until recently, border studies in con- Atemporary Southeast Asia appeared as an afterthought at best to the politics of interstate rivalry and national consolidation. The maps set out all agreed postcolonial lines. Meanwhile, the physical demarcation of these boundar- ies lagged. Large slices of territory, on land and at sea, eluded definition or delineation. The Borderlands of Southeast Asia That comforting ambiguity has disappeared. Both evolving technologies and price levels enable rapid resource extraction in places, and in volumes, once scarcely imaginable. The beginning of the 21st century’s second decade is witnessing an intensifying diplomacy, both state-to-state and commercial, over offshore petroleum. In particular, the South China Sea has moved from being a rather arcane area of conflict studies to the status of a bellwether issue. Along with other contested areas in the western Pacific and south Asia, the problem increasingly defines China’s regional relationships in Asia—and with powers outside the region, especially the United States. Yet intraregional territorial differences also hobble multilateral diplomacy to counter Chinese claims, and daily management of borders remains burdened by a lot of retrospective baggage. The contributors to this book emphasize this mix of heritage and history as the primary leitmotif for contemporary border rivalries and dynamics. Whether the region’s 11 states want it or not, their bordered identity is falling into ever sharper definition—if only because of pressure from extraregional states.
    [Show full text]
  • PHILIPPINES 2018 Highlights of Events Page 1 of 5
    PHILIPPINES 2018 Highlights of Events Page 1 of 5 TROPICAL CYCLONES SEISMIC ACTIVITIES Twenty-one tropical cyclones entered the The country, which lies along the Pacific Ring of Fire, is constantly Philippine Area of Responsibility in 2018, of which frequented by seismic and volcanic activity each year. In 2018, seismic 21 8 made landfall. Five of these were Tropical monitoring by the Philippine Institute of Volcanology and Seismology entered the Depressions (TD). Notable was Typhoon (PHIVOLCS) recorded more than 5,800 seismic events. Around 95% of Philippine Area Mangkhut (Ompong) which made landfall in these events were Magnitude 4.0 and below, and therefore barely felt. of Responsibility September. It was the lone Category 4 typhoon Even with over 250 seismic events with Magnitude 4.0 and above, there that left a trail of damages, and displacement was no significant damage or casualties reported throughout the country. 8 made landfall mostly in northern part of Luzon. Majority of the However, the Magnitude 7.2 offshore quake that rocked Davao Oriental Tropical tropical cyclones that made landfall were province on 29 December 2018 created a 5 Depression Magnitude 4.0 LUZON characterized by heavy and prolonged rainfall, scare in the coastal communities in the & above (257) Tropical affecting 38 provinces which suffered repeated region after PHIVOLCS issued a Tsunami 1 Storm displacements topped by Eastern Visayas region Advisory, which was lifted a few hours later 1 Category 2 (4 out of the 6 provinces). 769 Barangays / Villages after only minor sea level disturbance. 5,868 experienced rain-induced flooding, while landslides 1 Category 4 Magnitude 4.0 Manila were also reported.
    [Show full text]
  • Deep Sea Drilling Project Initial Reports Volume 22
    16. STRATIGRAPHIC-SEISMIC SECTION CORRELATIONS AND IMPLICATIONS TO BENGAL FAN HISTORY David G. Moore, Naval Undersea Research and Development Center Joseph R. Curray, Russel W. Raitt, and Frans J. Emmel, Scripps Institution of Oceanography, La Jolla, California ABSTRACT Two drilling sites were proposed in the Bay of Bengal (Sites 217 and 218) in areas of anomalously thin section as determined by earlier seismic work. Although possibilities for characterizing the sediments in the normal thick section of the Bengal Fan were precluded, these holes were, nevertheless, successful in determin- ing the ages of two unconformity-refracting horizons which had been traced throughout the entire bay. These horizons, which subdivide the sedimentary section into three units, probably mark times of both plate-edge and mid-plate deformation. The oldest sediments in the Bay of Bengal were deposited on new sea floor formed after rifting of India from Antarctica and Australia, probably as a Cretaceous and Paleocene passive continental rise up to 12 km thick. First collision of India with the subduction zone lying off the southern margin of Asia occurred at the end of the Paleocene, causing both uplift of ancestral mountains in the eastern Himalayan region and defor- mation and unconformity across the bay. The first phase of Bengal Fan deposition was from middle Eocene into uppermost Miocene. At this time important further tectonism occurred, causing uplift of the modern Himalayas, deformation of the sea floor, and changes in sedimentation in the bay. Subsequent deposits of the modern Bengal Fan are largely undeformed. INTRODUCTION unconformably on apparently older deformed fan and pelagic deposits, and these in turn unconformably overlay The international Indian Ocean expeditions of 1960 to still older deposits of unknown origin.
    [Show full text]
  • Philippines, March 2006
    Library of Congress – Federal Research Division Country Profile: Philippines, March 2006 COUNTRY PROFILE: PHILIPPINES March 2006 COUNTRY Formal Name: Republic of the Philippines (Republika ng Pilipinas). Short Form: Philippines (Pilipinas). Term for Citizen(s): Filipino(s). Capital: Manila. Click to Enlarge Image Major Cities: Located on Luzon Island, Metropolitan Manila, including the adjacent Quezon City and surrounding suburbs, is the largest city in the Philippines, with about 12 million people, or nearly 14 percent of the total population. Other large cities include Cebu City on Cebu Island and Davao City on Mindanao Island. Independence: The Philippines attained independence from Spain on June 12, 1898, and from the United States on July 4, 1946. Public Holidays: New Year’s Day (January 1), Holy Thursday (also called Maundy Thursday, movable date in March or April), Good Friday (movable date in March or April), Araw ng Kagitingan (Day of Valor, commonly called Bataan Day outside of the Philippines, April 9), Labor Day (May 1), Independence Day (June 12), National Heroes Day (last Sunday of August), Bonifacio Day (celebration of the birthday of Andres Bonifacio, November 30), Eid al Fitr (the last day of Ramadan, movable date), Christmas Day (December 25), Rizal Day (the date of the execution by the Spanish of José Rizal in 1896, December 30). Flag: The flag of the Philippines has two equal horizontal bands of blue (top) and red with a white equilateral triangle based on the hoist side; in the center of the triangle is a yellow sun with eight primary rays (each containing three individual rays), and in each corner of the triangle is Click to Enlarge Image a small yellow five-pointed star.
    [Show full text]
  • The Country Report of the Republic of the Philippines: Technical Seminar on South China Sea Fisheries Resources
    The country report of the Republic of the Philippines: Technical seminar on South China Sea fisheries resources Item Type book_section Publisher Japan International Cooperation Agency Download date 30/09/2021 10:06:36 Link to Item http://hdl.handle.net/1834/40440 3.3 Other areas catch rate in waters shallower than 50 meters which are 3.3.1 East Malaysia fairly well exploited, and with a potential yield of 3.0 tons An estimate of potential yield is made for demersal and per square nautical mile. semipelagic species only based on the results of a single Unless very efficient gear, such as pair trawling, can be demersal trawl survey in the coastal waters up to about 50 employed to exploit successfully this sparse resource it is meters. The estimate is 183,000 tons but is more likely to not expected that major fishery can be developed. be between 91,500 to 137,250 tons. The potential yield (b) East coast of West Malaysia and East Malaysia per square nautical mile of 10.6 tons is similar to that of The estimate of potential yield is comprehensively the east coast of West Malaysia, 10.3 tons. dealt with by Shindo (IPFC/72/19) and as the average 3.3.2 Deeper waters density is low, though in some areas it is higher than (a) West coast of West Malaysia others, the problem of developing major fisheries for these In waters deeper than 50 meters the average catch rate demersal fish stocks is similar to the one discussed above of about 92.0 kg per hour was lower, about 64% of the for the west coast of West Malaysia.
    [Show full text]
  • Celebes Sea by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO
    An Atlas of Oceanic Internal Solitary Waves (February 2004) Celebes Sea by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO Celebes Sea Overview The Celebes Sea is located in the western Pacific Ocean north of the Indonesian Island of Celebes and south of the Sulu Sea and the Philippines (Figure 1). It is a deep-water sea, roughly circular with several exits to the Sulu Sea (to the north), the Makassar Strait (to the south), and the Phillipine and Molucca Seas (to the east). Figure 1. Bathymetry of the Celebes Sea. [Smith and Sandwell, 1997] Observations Like the Sulu Sea to the north, the Celebes Sea has a depth of over 4000 meters. It is surrounded by a shallow water regime along the edges of the adjacent landmasses and islands. The water depth in the northern region changes rapidly, from over 4000 m in Sulu Sea to approximately 100 m in the area across the Sulu Archipelago, returning to over 4000 m in the Celebes Sea. These bathymetric changes take place over approximately 150-km of horizontal distance. A similar situation takes place at the eastern end among the Kepulauan Sangi Islands. Both of these areas appear to be the sources of the internal waves observed in the Celebes Sea. There has been very little scientific research on the internal waves in the Celebes Sea. Satellite imagery indicates the internal waves are similar in character to those observed in the Sulu Sea. Internal waves are expected to occur all year round in the Celebes Sea, similar to other regions of the tropical Pacific (Table 1).
    [Show full text]
  • Celebes Sea and Sulu Sea, Leg 124, Sites 767 and 7681
    Silver, E. A., Rangin, C., von Breymann, M. T., et al., 1991 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 124 30. SUBSIDENCE AND SEDIMENTATION ANALYSIS OF MARGINAL BASINS: CELEBES SEA AND SULU SEA, LEG 124, SITES 767 AND 7681 Zehui Huang,2 Felix M. Gradstein,2 and Keith E. Louden3 ABSTRACT Based on the chronostratigraphy and porosity of the sediments recovered from ODP Sites 767 and 768 drilled in the Celebes Sea and Sulu Sea, respectively, we examine the decompacted sedimentation and basement subsidence rates using a quantitative method. The results of this study help us to recognize several important tectonic events in these two marginal basins which improve understanding of the regional tectonic development. Among the recognized events are: (1) a pronounced increase in decompacted sedimentation rate in the Celebes Sea at 23.4 Ma, indicating basin transformation from a larger, more open oceanic setting to a marginal basin; (2) an increased basement subsidence rate in both basins between 10.8 and 8.9 Ma associated with the initiation of the Sulu Trough and the Sulawesi Trough; (3) appearance of a decompacted sedimentation rate peak between 10.0 and 8.9 Ma in both basins, indicating the combined effect of tectonic uplift in the source area and a sea-level drop; (4) uplift of the basement since 2.0 Ma, first in the Celebes Sea and then in the Sulu Sea, probably occurring as the result of collision events. INTRODUCTION strike-slip fault system that cuts through Sulawesi, which is a Neogene volcanic arc. The Molucca Sea collision zone, which is The Sulu and Celebes Seas are two small marginal basins in nearing completion and features incipient thrusting on its west- the west Pacific region, a complicated geotectonic region ern boundary, lies to the southeast of the Celebes Sea (Hamilton, marked by dynamic arc-arc and arc-continent collision zones, 1977; Moore and Silver, 1982).
    [Show full text]
  • RIOP09, Leg 2 [Final] Report
    RIOP09, Leg 2 [final] Report Regional Cruise Intensive Observational Period 2009 RIOP09 R/V Melville, 27 February – 21 March 2009 Arnold L. Gordon, Chief Scientist Leg 2 [final] Report Manila to Dumaguete, 9 March to 21 March 2009 “Pidgie” RIOP09 Leg 2 Mascot, Dumaguete-Manila Preface: While this report covers RIOP09 leg 2, it also serves as the final report, thus the introductory section of the leg 1 report is repeated. For completeness within a single document the preliminary analysis [or better stated: first impressions of the story told by the RIOP09 data set] included in the leg 1 report are given in the appendices section of this report. Other appendices describe specific components of RIOP09: CTD-O2; LADCP; hull ADCP; PhilEx moorings; the Philippine research program: Chemistry/Bio- optics; and sediment trap moorings. I Introduction: The second Regional IOP of PhilEx, RIOP09, aboard the R/V Melville began from Manila on 27 February. We return to Manila on 21 March 2009, with an intermediate port stop for personnel exchange in Dumaguete, Negros, on 9 March. This divides the RIOP09 into 2 legs, with CTD-O2/LADCP/water samples [oxygen, nutrients]; hull ADCP and underway-surface data [met/SSS/SST/Chlorophyll] on both legs, and the recovery of: 4 PhilEx, 2 Sediment Trap moorings of the University of Hamburg, and an EM-Apex profiler, on leg 2. The general objective of RIOP09, as with the previous regional cruises is to provide a view of the stratification and circulation of the Philippine seas under varied monsoon condition, as required to support of PhilEx DRI goals directed at ocean 1 RIOP09, Leg 2 [final] Report dynamics within straits.
    [Show full text]