Şunu aradınız:: depths of despair (İngilizce - Tagalogca)

language of despair
talasalitaan ng pananamlay

depths of the earth
kailaliman ng lupa

in the depths of the nigh
saksi ang buwan at bituwin

lost in the depths of unspoken emotions
lost in the depths of unspoken emotions

i cannot express the depths of my gratitude
kabaitan at mapagbigay,

who are you talking to in the depths of the night
sino kausap mo sa kalaliman ng gabi

depth of
kaibuturan ng

depth of gratitude
depth of gratitude

the depth of thinking
ang lalim ng iniisip

the depth of your words
ang lalim ng mga salita

lack of depth of the respondent
lack of depth of the respondent

the depth of one's thinking
ang lalim ng iniisip ni tannie

we measured the depth of the river.
sinukat namin ang kalaliman ng ilog.

there is a depth of felling in this cry from the heart.
there is a depth of feeling in this cry from the heart

i do cherish you for the rest of my life if you're asking do i love you this much yes i do you don't have to think twice i will love you still from the depths of my soul it's beyond my control
minamahal kita sa buong panahon ng aking buhay hindi mo kailangang isiping dalawang beses mamahalin kita pa mula sa kalaliman ng aking kaluluwa ito ay lampas sa aking kontrol

with the rest of his strength, he swam with a swim to the depths of the sea. he also lured him to a floating timber-covered timber covered with thick sargassum. it served as a refuge and food for him - his home for a long time of adventure.
gamit ang natitira pa niyang lakas,lumangoy nang lumangoy si paeng patungo sa malalim na parte ng dagat. maswerte namang nakasakay siya sa isang palutang lutang na kahoy na nababalutan ng makapal na sargassum. ito ang nagsilbing kublihan at pagkain para sa kanya--ang kanyang tahanan sa loob ng mahabang panahon ng pakikipagsapalaran.

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.