Results for is the image large enough to suit... translation from English to Tagalog

is the image large enough to suit your purpose?
sapat ba ang laki ng larawan upang umangkop sa iyong layunin?

the man is the image of god
ang tao ay kawangis ng diyos

what is the central message of the image
tagalog

the only solution to this difficulty is the effort and cooperation of our family. accompanied by strong, unwavering faith in the lord and love for each other is enough to get out of adversity
ang tanging solusyon sa paghihirap na ito ay ang pagsisikap at pagtutulungan ng aming pamilya. sinamahan ng matibay, hindi natitinag na pananampalataya sa panginoon at pagmamahal sa isa't isa ay sapat na upang makaahon sa kahirapan

what do you think is the connection among the images..
ano sa palagay mo ang koneksyon sa mga larawan ..

our company is developed to offer or provide ample opportunity to supply a wide variety of products to suit your business needs. we provide as little or as much as we help to, extend your life expectancy in the fastest and broadest possible way, to identify with future generations
ang aming kumpanya ay binuo upang mag alok o magbigay ng malawak na oportunidad upang mag supply ng ibat ibang uri ng produkto na naayon sa kakailanganin ng inyong negosyo . kami ay nagbibigay ng kaunti o bultuhang bilang tumutulong kami upang ,apalawak ang inyong hanap buhay sa pinaka mabilis at malawak na pagunlad , makilala sa mga susunod pang henerasyon

artistic skill in sculpture is the art of molding welding or producing work of art in three dimension young rizal impressed his professor and classmate when he curved the image of the virgin mary on the piece of the philipines hard wood batikuling with a pocket knife the professors were amazed at the beuty and the finish of the image because of this sculpture talent father leonard request rizal to curved from him the image of the sacred heart of jesus the old jesuit priest was very much pleased and expressed his profound appreciation to the young sculpture his attention was to take with him the image of when he went back to spain but unfortunately he forgot the image was placed on the door of the dormitory of the ateneo and remained theme for almost twenty years
ang masining na kasanayan sa iskultura ay ang sining ng paghubog ng hinang o paggawa ng gawa ng sining sa tatlong sukat na batang si rizal ay humanga sa kanyang propesor at kaklase nang hubugin niya ang imahe ng birhen mary sa piraso ng pilipinas matapang na kahoy na batikuling na may isang kutsilyo ng bulsa ang mga propesor ay namangha sa beuty at pagtatapos ng imahe dahil sa iskultura na ito ng talento ng tatay na si leonard na humiling kay rizal na hubugin mula sa kanya ang imahe ng sagradong puso ni jesus ang matandang pari ng hesus ay labis

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.