Internal/External Forces

Total Page:16

File Type:pdf, Size:1020Kb

Internal/External Forces Internal/External Forces Unit 1: Basics of Geography Internal Forces ○ Tectonic plates: enormous moving pieces that form the earth’s crust- continually being reshaped ○ Earthquakes/Volcanoes ○ Move 1 of 4 ways: ○ Spreading ○ Subduction (dive under another plate) ○ Collision ○ Sliding past each other Internal Forces ○ 3 types of boundaries that mark plate movements: 1. Divergent boundary- plates move apart/spread (b/w Saudi Arabia and Egypt) 2. Convergent boundary- plates collide (India crashing into Asia) 3. Transform boundary- plates slide apart (San Andreas Fault) Internal Forces ○ Folds/Faults- 2 plates meet- folding and cracking of rock -Occurs very slowly -Sometimes rock not flexible, cracks cause a fault ○ Earthquakes- Plates grind/slip past each other, causing an earthquake ○ Seismograph detects earthquakes ○ Focus- where an earthquake begins ○ Epicenter- point directly above the focus Internal Forces ○ Landslides, displacement of land, fires (broken gas lines) collapsed buildings ○ Aftershocks and smaller magnitude earthquakes ○ Richter Scale- 2 usually not noticed; 4.5 makes the news ○ Major is 7 or more- Largest reported 8.9 Kermadec Islands, So. Pacific Internal Forces ○ Tsunami- Giant wave in ocean caused by an earthquake up to 450 mph and 50-100 ft. waves ○ 2004 Tsunami hit Dec. 26 Indonesia, Thailand, Sri Lanka, Somalia ○ Waves about 33 feet high ○ 4th largest in world since 1900….9+ more than 150,000 casualties ○ Volcanoes- Found along tectonic plate boundaries -Magma, gases, and water from the lowest of the crust collect in underground chambers -Magma that reaches the earth’s surface is called lava Internal Forces □ Most dramatic volcano action-eruption- hot lava, gases, ash, dust, rocks explode out of vents in the earth’s crust (often a hill or mountain is formed by lava □ Volcanoes can be active for many years than stop. Can be inactive and become active. □ Ring of Fire- Zone around the rim of the Pacific Ocean- location of the vast majority of active volcanoes Internal Forces ○ 8 major tectonic plates meet in zone. Volcanic action and earthquakes occur frequently. ○ Hot spots- Hot springs and geysers- water heats up and rises to surface ○ Yellowstone- Old Faithful External Forces ○ Weathering- physical and chemical processes that change the characteristics of rock on or near the earth’s surface. Occurs slowly. ○ Creates sediment- smaller and smaller pieces of rock, mud, sand, or silt ○ Mechanical weathering- breaks rock into smaller pieces (construction, drilling, blasting, frost, plant roots External Forces ○ Chemical weathering- Decomposition (break up) Rock is changed into a new substance as a result of interaction b/w elements in the air. ○ Erosion- Weathered material is moved by the action of wind, water, ice or gravity. Glaciers, waves, blowing winds cause erosion; reshapes landforms ○ Water forms a delta (river enters ocean) Waves form beaches External Forces ○ Wind- transports/deposits sediment- sand dunes, rocks, loess (loh-uhs) are wind blown silt/clay sediment ○ Glaciers- large, long lasting mass of ice; cut valleys into the land; rocks left behind may form a ridge or hill; may be tunnels inside or under glacier ○ Soil- weathered rock, organic matter (humus), air, and water External Forces ○ Soil factors: Determine type of vegetation ○ Parent material- chemical composition of original rock ○ Relief- steeper slopes are eroded easily and do not produce soil quickly ○ Organisms- help loosen soil/supply nutrients ○ Climate- hot/cold wet/dry ○ Time- amount of time to produce soil varies (avg 2.5 cc/century).
Recommended publications
  • Biodiversity of the Kermadec Islands and Offshore Waters of the Kermadec Ridge: Report of a Coastal, Marine Mammal and Deep-Sea Survey (TAN1612)
    Biodiversity of the Kermadec Islands and offshore waters of the Kermadec Ridge: report of a coastal, marine mammal and deep-sea survey (TAN1612) New Zealand Aquatic Environment and Biodiversity Report No. 179 Clark, M.R.; Trnski, T.; Constantine, R.; Aguirre, J.D.; Barker, J.; Betty, E.; Bowden, D.A.; Connell, A.; Duffy, C.; George, S.; Hannam, S.; Liggins, L..; Middleton, C.; Mills, S.; Pallentin, A.; Riekkola, L.; Sampey, A.; Sewell, M.; Spong, K.; Stewart, A.; Stewart, R.; Struthers, C.; van Oosterom, L. ISSN 1179-6480 (online) ISSN 1176-9440 (print) ISBN 978-1-77665-481-9 (online) ISBN 978-1-77665-482-6 (print) January 2017 Requests for further copies should be directed to: Publications Logistics Officer Ministry for Primary Industries PO Box 2526 WELLINGTON 6140 Email: [email protected] Telephone: 0800 00 83 33 Facsimile: 04-894 0300 This publication is also available on the Ministry for Primary Industries websites at: http://www.mpi.govt.nz/news-resources/publications.aspx http://fs.fish.govt.nz go to Document library/Research reports © Crown Copyright - Ministry for Primary Industries TABLE OF CONTENTS EXECUTIVE SUMMARY 1 1. INTRODUCTION 3 1.1 Objectives: 3 1.2 Objective 1: Benthic offshore biodiversity 3 1.3 Objective 2: Marine mammal research 4 1.4 Objective 3: Coastal biodiversity and connectivity 5 2. METHODS 5 2.1 Survey area 5 2.2 Survey design 6 Offshore Biodiversity 6 Marine mammal sampling 8 Coastal survey 8 Station recording 8 2.3 Sampling operations 8 Multibeam mapping 8 Photographic transect survey 9 Fish and Invertebrate sampling 9 Plankton sampling 11 Catch processing 11 Environmental sampling 12 Marine mammal sampling 12 Dive sampling operations 12 Outreach 13 3.
    [Show full text]
  • I. Convergent Plate Boundaries (Destructive Margins) (Colliding Plates)
    I. Convergent plate boundaries (destructive margins) (colliding plates) 1. Plates collide, an ocean trench forms, lithosphere is subducted into the mantle 2. Types of convergence—three general classes, created by two types of plates —denser oceanic plate subsides into mantle SUBDUCTION --oceanic trench present where this occurs -- Plate descends angle average 45o a. Oceanic-continental convergence 1. Denser oceanic slab sinks into the asthenosphere—continental plate floats 2. Pockets of magma develop and rise—due to water added to lower part of overriding crust—100-150 km depth 3. Continental volcanic arcs form a. e.g., Andes Low angle, strong coupling, strong earthquakes i. Nazca plate ii. Seaward migration of Peru-Chile trench b. e.g., Cascades c. e.g., Sierra Nevada system example of previous subduction b. Oceanic-oceanic convergence 1. Two oceanic slabs converge HDEW animation Motion at Plate Boundaries a. one descends beneath the other b. the older, colder one 2. Often forms volcanoes on the ocean floor 3. Volcanic island arcs forms as volcanoes emerge from the sea 200-300 km from subduction trench TimeLife page 117 Philippine Arc a. e.g., Aleutian islands b. e.g., Mariana islands c. e.g., Tonga islands all three are young volcanic arcs, 20 km thick crust Japan more complex and thicker crust 20-35 km thick c. Continental-continental convergence— all oceaninc crust is destroyed at convergence, and continental crust remains 1. continental crust does not subside—too buoyant 2. two continents collide—become ‘sutured’ together 3. Can produce new mountain ranges such as the Himalayas II. Transform fault boundaries 1.
    [Show full text]
  • Plate Tectonics Says That Earth’S Plates Move Because of Convection Currents in the Mantle
    Bellringer Which ocean is getting smaller and which ocean is getting bigger due to subduction and sea floor spreading? Plate Tectonic Theory Notes How Plates Move • Earth’s crust is broken into many jagged pieces. The surface is like the shell of a hard-boiled egg that has been rolled. The pieces of Earth’s crust are called plates. Plates carry continents, oceans floors, or both. How Plates Move • The theory of plate tectonics says that Earth’s plates move because of convection currents in the mantle. Currents in the mantle carry plates on Earth’s surface, like currents in water carry boats on a river, or Cheerios in milk. How Plates Move • Plates can meet in three different ways. Plates may pull apart, push together, or slide past each other. Wherever plates meet, you usually get volcanoes, mountain ranges, or ocean trenches. Plate Boundaries • A plate boundary is where two plates meet. Faults form along plate boundaries. A fault is a break in Earth’s crust where blocks of rock have slipped past each other. Plate Boundaries • Where two plates move apart, the boundary is called a divergent boundary. • A divergent boundary between two oceanic plates will result in a mid-ocean ridge AND rift valley. (SEE: Sea-Floor Spreading) • A divergent boundary between two continental plates will result in only a rift valley. This is currently happening at the Great Rift Valley in east Africa. Eventually, the Indian Ocean will pour into the lowered valley and a new ocean will form. Plate Boundaries • Where two plates push together, the boundary is called a convergent boundary.
    [Show full text]
  • My Friend, the Volcano (Adapted from the 2004 Submarine Ring of Fire Expedition)
    New Zealand American Submarine Ring of Fire 2007 My Friend, The Volcano (adapted from the 2004 Submarine Ring of Fire Expedition) FOCUS MAXIMUM NUMBER OF STUDENTS Ecological impacts of volcanism in the Mariana 30 and Kermadec Islands KEY WORDS GRADE LEVEL Ring of Fire 5-6 (Life Science/Earth Science) Asthenosphere Lithosphere FOCUS QUESTION Magma What are the ecological impacts of volcanic erup- Fault tions on tropical island arcs? Transform boundary Convergent boundary LEARNING OBJECTIVES Divergent boundary Students will be able to describe at least three Subduction beneficial impacts of volcanic activity on marine Tectonic plate ecosystems. BACKGROUND INFORMATION Students will be able to explain the overall tec- The Submarine Ring of Fire is an arc of active vol- tonic processes that cause volcanic activity along canoes that partially encircles the Pacific Ocean the Mariana Arc and Kermadec Arc. Basin, including the Kermadec and Mariana Islands in the western Pacific, the Aleutian Islands MATERIALS between the Pacific and Bering Sea, the Cascade Copies of “Marianas eruption killed Anatahan’s Mountains in western North America, and numer- corals,” one copy per student or student group ous volcanoes on the western coasts of Central (from http://www.cdnn.info/eco/e030920/e030920.html) America and South America. These volcanoes result from the motion of large pieces of the AUDIO/VISUAL MATERIALS Earth’s crust known as tectonic plates. None Tectonic plates are portions of the Earth’s outer TEACHING TIME crust (the lithosphere) about 5 km thick, as Two or three 45-minute class periods, plus time well as the upper 60 - 75 km of the underlying for student research mantle.
    [Show full text]
  • Patterns of Prehistoric Human Mobility in Polynesia Indicated by Mtdna from the Pacific Rat (Rattus Exulans͞population Mobility)
    Proc. Natl. Acad. Sci. USA Vol. 95, pp. 15145–15150, December 1998 Anthropology Patterns of prehistoric human mobility in Polynesia indicated by mtDNA from the Pacific rat (Rattus exulansypopulation mobility) E. MATISOO-SMITH*†,R.M.ROBERTS‡,G.J.IRWIN*, J. S. ALLEN*, D. PENNY§, AND D. M. LAMBERT¶ *Department of Anthropology and ‡School of Biological Sciences, University of Auckland, P. B. 92019 Auckland, New Zealand; and §Molecular Genetics Unit and ¶Department of Ecology, Massey University, P. B. 11222 Palmerston North, New Zealand Communicated by R. C. Green, University of Auckland, Auckland, New Zealand, October 14, 1998 (received for review July 20, 1998) ABSTRACT Human settlement of Polynesia was a major Recent genetic research focusing on Polynesian populations event in world prehistory. Despite the vastness of the distances has contributed significantly to our understanding of the covered, research suggests that prehistoric Polynesian popu- ultimate origins of this last major human migration. Studies of lations maintained spheres of continuing interaction for at globin gene variation (2) and mtDNA lineages of modern least some period of time in some regions. A low level of genetic Polynesians (3, 4) and studies of ancient DNA from Lapita- variation in ancestral Polynesian populations, genetic admix- associated skeletons (5) may indicate that some degree of ture (both prehistoric and post-European contact), and severe admixture with populations in Near Oceania occurred as more population crashes resulting from introduction of European remote biological ancestors left Southeast Asia and passed diseases make it difficult to trace prehistoric human mobility through Near Oceania. An alternative hypothesis is that the in the region by using only human genetic and morphological biological ancestors of these groups were one of a number of markers.
    [Show full text]
  • Santa Monica Mountains National Recreation Area Geologic Resources Inventory Report
    National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Santa Monica Mountains National Recreation Area Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2016/1297 ON THE COVER: Photograph of Boney Mountain (and the Milky Way). The Santa Monica Mountains are part of the Transverse Ranges. The backbone of the range skirts the northern edges of the Los Angeles Basin and Santa Monica Bay before descending into the Pacific Ocean at Point Mugu. The ridgeline of Boney Mountain is composed on Conejo Volcanics, which erupted as part of a shield volcano about 15 million years ago. National Park Service photograph available at http://www.nps.gov/samo/learn/photosmultimedia/index.htm. THIS PAGE: Photograph of Point Dume. Santa Monica Mountains National Recreation Area comprises a vast and varied California landscape in and around the greater Los Angeles metropolitan area and includes 64 km (40 mi) of ocean shoreline. The mild climate allows visitors to enjoy the park’s scenic, natural, and cultural resources year-round. National Park Service photograph available at https://www.flickr.com/photos/ santamonicamtns/albums. Santa Monica Mountains National Recreation Area Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2016/1297 Katie KellerLynn Colorado State University Research Associate National Park Service Geologic Resources Division Geologic Resources Inventory PO Box 25287 Denver, CO 80225 September 2016 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics.
    [Show full text]
  • Active Continental Margin
    Encyclopedia of Marine Geosciences DOI 10.1007/978-94-007-6644-0_102-2 # Springer Science+Business Media Dordrecht 2014 Active Continental Margin Serge Lallemand* Géosciences Montpellier, University of Montpellier, Montpellier, France Synonyms Convergent boundary; Convergent margin; Destructive margin; Ocean-continent subduction; Oceanic subduction zone; Subduction zone Definition An active continental margin refers to the submerged edge of a continent overriding an oceanic lithosphere at a convergent plate boundary by opposition with a passive continental margin which is the remaining scar at the edge of a continent following continental break-up. The term “active” stresses the importance of the tectonic activity (seismicity, volcanism, mountain building) associated with plate convergence along that boundary. Today, people typically refer to a “subduction zone” rather than an “active margin.” Generalities Active continental margins, i.e., when an oceanic plate subducts beneath a continent, represent about two-thirds of the modern convergent margins. Their cumulated length has been estimated to 45,000 km (Lallemand et al., 2005). Most of them are located in the circum-Pacific (Japan, Kurils, Aleutians, and North, Middle, and South America), Southeast Asia (Ryukyus, Philippines, New Guinea), Indian Ocean (Java, Sumatra, Andaman, Makran), Mediterranean region (Aegea, Cala- bria), or Antilles. They are generally “active” over tens (Tonga, Mariana) or hundreds (Japan, South America) of millions of years. This longevity has consequences on their internal structure, especially in terms of continental growth by tectonic accretion of oceanic terranes, or by arc magmatism, but also sometimes in terms of continental consumption by tectonic erosion. Morphology A continental margin generally extends from the coast down to the abyssal plain (see Fig.
    [Show full text]
  • Copyright © by SIAM. Unauthorized Reproduction of This Article Is Prohibited. 82 PHILIPPE GUYENNE and DAVID P
    SIAM J. SCI. COMPUT. c 2007 Society for Industrial and Applied Mathematics Vol. 30, No. 1, pp. 81–101 A HIGH-ORDER SPECTRAL METHOD FOR NONLINEAR WATER WAVES OVER MOVING BOTTOM TOPOGRAPHY∗ † ‡ PHILIPPE GUYENNE AND DAVID P. NICHOLLS Abstract. We present a numerical method for simulations of nonlinear surface water waves over variable bathymetry. It is applicable to either two- or three-dimensional flows, as well as to either static or moving bottom topography. The method is based on the reduction of the problem to a lower-dimensional Hamiltonian system involving boundary quantities alone. A key component of this formulation is the Dirichlet–Neumann operator which, in light of its joint analyticity properties with respect to surface and bottom deformations, is computed using its Taylor series representation. We present new, stabilized forms for the Taylor terms, each of which is efficiently computed by a pseu- dospectral method using the fast Fourier transform. Physically relevant applications are displayed to illustrate the performance of the method; comparisons with analytical solutions and laboratory experiments are provided. Key words. gravity water waves, bathymetry, pseudospectral methods, Dirichlet–Neumann operators, boundary perturbations AMS subject classifications. 76B15, 76B07, 65M70, 35S30 DOI. 10.1137/060666214 1. Introduction. Accurate modeling of surface water wave dynamics over bot- tom topography is of great importance to coastal engineers and has drawn considerable attention in recent years. Here are just a few applications: linear [16, 33] and nonlinear wave shoaling [25, 24, 28, 27], Bragg reflection [35, 15, 36, 14, 30, 33, 4], harmonic wave generation [3, 17, 18], and tsunami generation [37, 22].
    [Show full text]
  • Obsidian from Macauley Island: a New Zealand Connection
    www.aucklandmuseum.com Obsidian from Macauley Island: a New Zealand connection Louise Furey Auckland War Memorial Museum Callan Ross-Sheppard McGill University, Montreal Kath E. Prickett Auckland War Memorial Museum Abstract An obsidian flake collected from Macauley Island during the Kermadec Expedition has been analysed to determine the source. The result indicates a Mayor Island, New Zealand, origin, supporting previous results on obsidian from Raoul Island that Polynesians travelled back into the Pacific from New Zealand. Keywords obsidian; Pacific colonisation; Pacific voyaging; Macauley Island. INTRODUCTION The steep terrain meant there were only a few suitable habitation places confined to flat areas of limited size on The Kermadec Islands comprise Raoul Island, the largest the south and north coasts. The only landing places were of the group, the nearby Meyer Islands and Herald adjacent to these flats. Botanical surveys have recorded Islets, and 100–155 km to the south are Macauley, the presence of Polynesian tropical cultigens including Curtis and Cheeseman iIslands, and L’Esperence Rock. candlenut (Aleurites monuccana) and ti (Cordyline Raoul is approximately 1000 km to the northeast of fruticosa) (Sykes 1977) which are not endemic to the New Zealand. During the 2011 Kermadec Expedition, island and it is assumed they were transported there by samples of naturally occurring obsidian were obtained Polynesian settlers. Polynesian tuberous vegetables such from Raoul, the Meyer Islands, and from the sea floor off as taro (Colocasia esculenta) and kumara (Ipomoea Curtis Island. These are now in the Auckland Museum batatas) were also recorded but their introduction collection. More importantly however was the single attributed to later 19th century immigrants.
    [Show full text]
  • Plate Tectonics Passport
    What is plate tectonics? The Earth is made up of four layers: inner core, outer core, mantle and crust (the outermost layer where we are!). The Earth’s crust is made up of oceanic crust and continental crust. The crust and uppermost part of the mantle are broken up into pieces called plates, which slowly move around on top of the rest of the mantle. The meeting points between the plates are called plate boundaries and there are three main types: Divergent boundaries (constructive) are where plates are moving away from each other. New crust is created between the two plates. Convergent boundaries (destructive) are where plates are moving towards each other. Old crust is either dragged down into the mantle at a subduction zone or pushed upwards to form mountain ranges. Transform boundaries (conservative) are where are plates are moving past each other. Can you find an example of each type of tectonic plate boundary on the map? Divergent boundary: Convergent boundary: Transform boundary: What do you notice about the location of most of the Earth’s volcanoes? P.1 Iceland Iceland lies on the Mid Atlantic Ridge, a divergent plate boundary where the North American Plate and the Eurasian Plate are moving away from each other. As the plates pull apart, molten rock or magma rises up and erupts as lava creating new ocean crust. Volcanic activity formed the island about 16 million years ago and volcanoes continue to form, erupt and shape Iceland’s landscape today. The island is covered with more than 100 volcanoes - some are extinct, but about 30 are currently active.
    [Show full text]
  • Presentation on Pacific Plate and Associated Boundaries
    PACIFIC PLATE AND ASSOCIATED BOUNDARIES The Pacific Plate • Pacific Plate is the largest plate and an oceanic plate. • It shares its boundaries with numerous plates namely; North American Plate.(Convergent and transform fault) Philippine Plate.(Convergent) Juan de Fuca Plate.(Convergent) Indo – Australian Plate.(Convergent, Transform Fault) Cocos Plate.(Divergent) Nazca Plate.(Divergent) Antarctic Plate.(Divergent,Transform Fault) Types of Plate Boundaries • Convergent Boundary: Subduction zones where two plates converges. Eg; Aleutian Islands(Alaska) • Divergent Boundary: Spreading centres where two plates move away from each other. Eg; East Pacific Rise (MOR, Pacific Ocean). • Transform Faults: Boundary where two plates slide past each other. For Eg. ; San Andreas Fault. BOUNDARY WITH ANTARCTIC PLATE DIVERGENT BOUNDARY • Pacific – Antarctic Ridge TRANSFORM FAULT • Louisville Seamount Chain Pacific – Antarctic Ridge Pacific – Antarctic Ridge(PAR) is located on the seafloor of the South Pacific Ocean. It is driven by the interaction of a mid oceanic ridge and deep mantle plumes located in the eastern portion of East Pacific Ridge. Louisville Seamount Chain It is the longest line of seamount chain in the Pacific Ocean of about 4,300 km, formed along the transform boundary in the western side between Pacific plate and Antarctic plate. It was formed from the Pacific Plate sliding over a long – lived centre of upwelling magma called the Louisville hotspot. BOUNDARY WITH PHILIPPINE PLATE CONVERGENT BOUNDARY • Izu – Ogasawara Trench • Mariana Trench Izu – Ogasawara Trench It is an oceanic trench in the western Pacific Ocean. It stretches from Japan to northern most section of Mariana Trench. Here, the Pacific Plate is being subducted beneath the Philippine Sea Plate.
    [Show full text]
  • Code Sequence
    Code Sequence PART II: CODE SEQUENCE Discontinued codes are identified by a hyphen preceding the first letter in the code string. a Asia a-ccp Bo Hai (China) a-af Afghanistan a-ccs Xi River (China) a-ai Armenia (Republic) a-ccy Yellow River (China) a-aj Azerbaijan a-ce Sri Lanka a-ba Bahrain a-ch Taiwan a-bg Bangladesh a-cy Cyprus a-bn Borneo a-em East Timor a-br Burma a-gs Georgia (Republic) a-bt Bhutan -a-hk Hong Kong a-bx Brunei a-ii India a-cb Cambodia a-io Indonesia a-cc China a-iq Iraq a-cc-an Anhui Sheng (China) a-ir Iran a-cc-ch Zhejiang Sheng (China) a-is Israel a-cc-cq Chongqing (China) a-ja Japan a-cc-fu Fujian Sheng (China) a-jo Jordan a-cc-ha Hainan Sheng (China) a-kg Kyrgyzstan a-cc-he Heilongjiang Sheng (China) a-kn Korea (North) a-cc-hh Hubei Sheng (China) a-ko Korea (South) a-cc-hk Hong Kong (China) a-kr Korea a-cc-ho Henan Sheng (China) a-ku Kuwait a-cc-hp Hebei Sheng (China) a-kz Kazakhstan a-cc-hu Hunan Sheng (China) a-le Lebanon a-cc-im Inner Mongolia (China) a-ls Laos a-cc-ka Gansu Sheng (China) -a-mh Macao a-cc-kc Guangxi Zhuangzu Zizhiqu a-mk Oman (China) a-mp Mongolia a-cc-ki Jiangxi Sheng (China) a-my Malaysia a-cc-kn Guangdong Sheng (China) a-np Nepal a-cc-kr Jilin Sheng (China) a-nw New Guinea a-cc-ku Jiangsu Sheng (China) -a-ok Okinawa a-cc-kw Guizhou Sheng (China) a-ph Philippines a-cc-lp Liaoning Sheng (China) a-pk Pakistan a-cc-mh Macao (China : Special a-pp Papua New Guinea Administrative Region) -a-pt Portuguese Timor a-cc-nn Ningxia Huizu Zizhiqu (China) a-qa Qatar a-cc-pe Beijing (China) a-si Singapore
    [Show full text]