PAGBASA-BASA PUD ARON MAKAHIBALU TA OG DI TA MAGPABILIN NGA - TopicsExpress



          

PAGBASA-BASA PUD ARON MAKAHIBALU TA OG DI TA MAGPABILIN NGA IGNORANTE. FOR WHAT IS THIS LIFE WHEN WE DONT LEARN? ayg palabi og katapulan diha MR JUAN TAMAD!!! i dont know why i trouble myself when nobody really cares ....... IT IS GREAT WHEN YOU ARE A PERSON WITH A GOOD HEART; BUT A PERSON WITH A GOOD HEART AND WITH A LOT OF KNOWLEDGE, IS JUST AMAZING. A HEART THAT IS GOOD with an INTELLIGENT HEAD, is a HEART OF GOLD! TO change topic: ----------> Please READ (IMPORTANT!) THOSE LIVING near the coasts, especially when your area is very plain. you should get away from the place after an earthquake. there are some places like of the Mactan island, this city is very plain. the risk of the TSUNAMI is very high. Now, we have heard of the last TSUNAMI that took place not long ago in Japan, so you should take this very seriously. When the ocean disappears and you find it to be very strange, and when it is for you a not ORDINARY PHENOMENON be aware that the next thing that could happen would be the possible Tsunami to come. Imagine how high those giant waves are and how monstrous! So dont go out into the sea anymore but run to a higher place, far from the sea water and from the beach. It is not just because you think that there had not been any records of any TSUNAMI over in the Philippines, it does not mean that this can never happen. And sadly, it seems that the government have no programs or seminars to inform and educate the people about this kind of calamity. Remember, the Philippines is also built on one of those TECTONIC PLATES. This is a list of tectonic plates on Earth. Tectonic plates are pieces of the Earths crust and uppermost mantle, together. List of tectonic plates This is a list of tectonic plates on Earth. Tectonic plates are pieces of the Earths crust and uppermost mantle, together referred to as the lithosphere. The plates are around 100 km (62 mi) thick and consist of two principal types of material: oceanic crust (also called sima from silicon and magnesium) and continental crust (sial from silicon and aluminium). The composition of the two types of crust differs markedly, with basaltic rocks (mafic) dominating oceanic crust, while continental crust consists principally of lower density granitic rocks (felsic). See also Plate tectonics. Contents 1 Current plates 1.1 Primary plates 1.2 Secondary plates 1.3 Tertiary plates 2 Ancient continental formations 2.1 Ancient supercontinents 2.2 Ancient plates and cratons 2.2.1 African plate 2.2.2 Antarctica plate 2.2.3 Eurasian plate 2.2.4 Indo-Australian plate 2.2.5 North American plate 2.2.6 South American plate 3 References Current plates The following tectonic plates currently exist on the Earths surface with roughly definable boundaries. Primary plates These seven plates comprise the bulk of the continents and the Pacific Ocean. African Plate Antarctic Plate Eurasian Plate Indo-Australian Plate Nort American Plate ---> Pacific Plate South American Plate Secondary plates These smaller plates are generally not shown on major plate maps with the exception of the Arabian and Indian plates, as they do not comprise significant land area. Arabian Plate Caribbean Plate Cocos Plate Indian Plate Juan de Fuca Plate Nazca Plate Philippine Sea Plate Scotia Plate Tertiary plates Tertiary plates are grouped with the major plate that they would otherwise be shown as part of on a major plate map. Mostly these are tiny microplates, although in the case of the Nubian-Somalian and Australian-Capricorn-Indian plates these are major plates that are rifting apart. Some models identify more minor plates within current orogens like the Apulian, Explorer, Gorda, and Philippine Mobile Belt plates. The remainder of the tertiary plates are the dwindling remains of much larger ancient plates[examples needed].[citation needed] There may or may not be scientific consensus as to whether a tertiary plate is a separate plate yet[examples needed], is still a separate plate as with the Greenland and Malagasy Plates, or should be considered a separate plate, thus new research could change this list.[1][2][3][4] African Plate Lwandle Plate Nubian Plate Rovuma Plate Seychelles Plate Somali Plate Victoria Plate Antarctic Plate Kerguelen microcontinent Shetland Plate South Sandwich Plate Caribbean Plate Panama Plate Gonâve Microplate Cocos Plate Rivera Plate Eurasian Plate Adriatic or Apulian Plate Aegean Sea Plate (or Hellenic Plate) Amurian Plate Anatolian Plate Azores Microplate[5] Banda Sea Plate Burma Plate Iberian Plate Iranian Plate Molucca Sea Plate Halmahera Plate Sangihe Plate Okinawa Plate Pelso Plate Sunda Plate Timor Plate Tisza Plate Yangtze Plate Indo-Australian Plate Australian Plate Capricorn Plate Futuna Plate Indian Plate Kermadec Plate Maoke Plate Niuafoou Plate Sri Lanka Plate Tonga Plate Woodlark Plate Juan de Fuca Plate Explorer Plate Gorda Plate North American Plate Greenland Plate Okhotsk Plate Pacific Plate Balmoral Reef Plate Birds Head Plate Caroline Plate Conway Reef Plate Easter Plate Galapagos Plate Juan Fernandez Plate Kula Plate Manus Plate New Hebrides Plate North Bismarck Plate North Galapagos MicroPlate Solomon Sea Plate South Bismarck Plate PHILIPPINE SEA PLATE Mariana Plate Philippine Microplate South American Plate Altiplano Plate Falklands Microplate North Andes Plate
Posted on: Fri, 16 May 2014 08:40:22 +0000

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