Hai cercato la traduzione di legend seen on maps da Inglese a Tagalog

legend seen on maps
filipino

seen on tv
nakita ko ito sa tv news

as seen on your id
tulad ng sa iyong id

can be seen on his face
mababakas

what can be seen on the playground
ano ang makikita sa playground

what does it mean to be seen on facebook
ano ang ibig sabihin ng seen sa facebook

original and can only be seen on the dvd.
orihinal at makikita niyo lamang sa dvd.

streaky densities are seen on the left hilar area
streaky densities are seen on the left hilar area

do not focus on map when starting
huwag mag-focus sa mapa habang nag-sisimula

the day i saw you again for a long time at least one day away from home you can be seen on the day you're saddest i can't find my feeling my hidden love for you
yung araw na nakita kita ulit sa haba ng panahon kahit isang dipa lang ang layo ng iyong tirahan ay masilayan ka sa araw na pinaka malungkot mong di ko mawari ang aking mararamdaman .

the exploration of colonization discovery on maps and countries in imperialism asia on the topic about colonization about empires and whole full map about kingdoms and their states and national flags in south east asia by economy and how they usually leading the country and their voyage to the province from sailing to the sea and islands.
ang paggalugad sa kolonisasyon na pagtuklas sa mga mapa at bansa sa imperyalismo asia sa paksang tungkol sa kolonisasyon tungkol sa mga emperyo at buong buong mapa tungkol sa mga kaharian at kanilang mga estado at pambansang watawat sa timog silangang asya sa pamamagitan ng ekonomiya at kung paano sila karaniwang namumuno sa bansa at ang kanilang paglalakbay sa probinsiya mula sa paglalayag patungo sa dagat at mga isla.

lithospherethe word lithosphere is derived from the word sphere, combined with the greek word lithos, meaning rock . the lithosphere is the solid outer section of earth, which includes earth's crust (the "skin" of rock on the outer layer of planet earth), as well as the underlying cool, dense, and rigid upper part of the upper mantle. the lithosphere extends from the surface of earth to a depth of about 44–62 mi (70–100 km). this relatively cool and rigid section of earth is believed to "float" on top of the warmer, non-rigid, and partially melted material directly below. earth is made up of several layers. the outermost layer is called earth's crust. the thickness of the crust varies. under the oceans , the crust is only about 3–5 mi (5–10 km) thick. under the continents, however, the crust thickens to about 22 mi (35 km) and reaches depths of up to 37 mi (60 km) under some mountain ranges. beneath the crust is a layer of rock material that is also solid, rigid, and relatively cool, but is assumed to be made up of denser material. this layer is called the upper part of the upper mantle, and varies in depth from about 31–62 mi (50–100 km) below earth's surface. the combination of the crust and this upper part of the upper mantle, which are both comprised of relatively cool and rigid rock material, is called the lithosphere. below the lithosphere, the temperature is believed to reach 1,832°f (1,000°c), which is warm enough to allow rock material to flow if pressurized. seismic evidence suggests that there is also some molten material at this depth (perhaps about 10%). this zone which lies directly below the lithosphere is called the asthenosphere , from the greek word asthenes, meaning weak. the lithosphere, including both the solid portion of the upper mantle and earth's crust, is carried "piggyback" on top of the weaker, less rigid asthenosphere, which seems to be in continual motion. this motion creates stress in the rigid rock layers above it, forcing the slabs or plates of the lithosphere to jostle against each other, much like ice cubes floating in a bowl of swirling water . this motion of the lithospheric plates is known as plate tectonics , and is responsible for many of the movements seen on earth's surface today including earthquakes, certain types of volcanic activity, and continental drift. last update:2016-02-21 subject: science quality: excellent
lithospherethe word lithosphere is derived from the word sphere, combined with the greek word lithos, meaning rock . the lithosphere is the solid outer section of earth, which includes earth's crust (the "skin" of rock on the outer layer of planet earth), as well as the underlying cool, dense, and rigid upper part of the upper mantle. the lithosphere extends from the surface of earth to a depth of about 44–62 mi (70–100 km). this relatively cool and rigid section of earth is believed to "float" on top of the warmer, non-rigid, and partially melted material directly below. earth is made up of several layers. the outermost layer is called earth's crust. the thickness of the crust varies. under the oceans , the crust is only about 3–5 mi (5–10 km) thick. under the continents, however, the crust thickens to about 22 mi (35 km) and reaches depths of up to 37 mi (60 km) under some mountain ranges. beneath the crust is a layer of rock material that is also solid, rigid, and relatively cool, but is assumed to be made up of denser material. this layer is called the upper part of the upper mantle, and varies in depth from about 31–62 mi (50–100 km) below earth's surface. the combination of the crust and this upper part of the upper mantle, which are both comprised of relatively cool and rigid rock material, is called the lithosphere. below the lithosphere, the temperature is believed to reach 1,832°f (1,000°c), which is warm enough to allow rock material to flow if pressurized. seismic evidence suggests that there is also some molten material at this depth (perhaps about 10%). this zone which lies directly below the lithosphere is called the asthenosphere , from the greek word asthenes, meaning weak. the lithosphere, including both the solid portion of the upper mantle and earth's crust, is carried "piggyback" on top of the weaker, less rigid asthenosphere, which seems to be in continual motion. this motion creates stress in the rigid rock layers above it, forcing the slabs or plates of the lithosphere to jostle against each other, much like ice cubes floating in a bowl of swirling water . this motion of the lithospheric plates is known as plate tectonics , and is responsible for many of the movements seen on earth's surface today including earthquakes, certain types of volcanic activity, and continental drift.