전문 번역가, 번역 회사, 웹 페이지 및 자유롭게 사용할 수 있는 번역 저장소 등을 활용합니다.
depth of
kaibuturan ng
마지막 업데이트: 2017-06-08
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depth of gratitude
depth of gratitude
마지막 업데이트: 2021-04-21
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the depth of thinking
ang lalim ng iniisip
마지막 업데이트: 2021-08-01
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example of field research
halimbawa ng field research
마지막 업데이트: 2022-03-27
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lack of depth of the respondent
lack of depth of the respondent
마지막 업데이트: 2024-01-03
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the depth of one's thinking
ang lalim ng iniisip ni tannie
마지막 업데이트: 2020-04-12
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tagalog translation of field personnel
field personnel
마지막 업데이트: 2023-06-25
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we measured the depth of the river.
sinukat namin ang kalaliman ng ilog.
마지막 업데이트: 2014-02-01
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thank you for the opportunity to work in this kind of field
마지막 업데이트: 2023-12-19
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there is a depth of felling in this cry from the heart.
there is a depth of feeling in this cry from the heart
마지막 업데이트: 2021-03-29
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eof before value of field `%.*s' (missing final newline)
eof nauna sa halaga ng saklaw `%.*s' (kulang ng kahulihang newline)
마지막 업데이트: 2014-08-15
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depths of the earth
kailaliman ng lupa
마지막 업데이트: 2017-06-22
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in the depths of the nigh
saksi ang buwan at bituwin
마지막 업데이트: 2022-09-17
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if only i could have come up with the right words to describe the depth of these feelings that i have for you,
마지막 업데이트: 2023-06-05
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i cannot express the depths of my gratitude
kabaitan at mapagbigay,
마지막 업데이트: 2021-01-15
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who are you talking to in the depths of the night
sino kausap mo sa kalaliman ng gabi
마지막 업데이트: 2020-09-07
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it was thought the water would freeze in the depths of the ice.
iniisip natin na ang tubig ay magyeyelo sa ilalim ng yelo.
마지막 업데이트: 2016-10-27
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in the depths of yout ribcage i want to be not a prisoner but an everlasting song the aubade in your ears when the morn is birthing the lullabies at night when your eyelids are closed the melody that clothes your body tge mellow ballads that move your bobes
마지막 업데이트: 2021-04-23
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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.
마지막 업데이트: 2016-02-21
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