검색어: comprised of such extensions of the skin (영어 - 타갈로그어)

function of the skin
describe the uses of the skin

the white of the skin
nakaka puti ng balat

she said from the gourd of the skin
kurad

avoid the direct sunlight of the skin
tagalog

anung medicine pampa smoothness of the skin
anung gamot ang pampa kinis ng balat

extension of the cause
pagpapalawig

by the skin of the teeth
sa pamamagitan ng balat sa ngipin

stains on the skin of the face
mantsa sa balat ng mukha

what is the medicine for the skin of the lame tree
anong gamot sa balat na kamiring tree

any point on the surface of the skin that is particularly sensitive to stimuli producing the sensation of warmth.
anumang punto sa ibabaw ng balat na partikular na sensitibo sa mga stimuli na gumagawa ng sensasyon ng init.

the skin of the papaya will rot if it is left in a plastic container for a week
mabubulok ang balat ng papaya pag pinabayaan ito sa loob ng plastik na lalagyan ng isang linggo

the use of such a virus, be it inactive or dead, aims to elicit a prompt immune response of the human body to a new infection with covid-19.
ang paggamit ng nasabing mikrobyo, maging ito ay hindi aktibo o patay, ay naglalayon na magtamo ng isang maagap na immune response ng katawan ng tao sa isang bagong pagkahawa ng covid-19.

mass density is an extension of the concept of mass just as pressure is an measure of the concentration of force.
mass density ay isang extension ng ang konsepto ng mass tulad presyon ay isang sukatan ng ang konsentrasyon ng puwersa.

tools are defind as impliments used to modify raw materials for human use. tools can be considered as extension of the human hand thereby increasing its speed power and accuracy
ang mga tool ay defind bilang mga impliment na ginamit upang baguhin ang mga hilaw na materyales para sa paggamit ng tao. ang mga tool ay maaaring isaalang-alang bilang pagpapalawak ng kamay ng tao sa gayon ay pinatataas ang bilis ng lakas at katumpakan nito

a comparison of the use of such words as, as apparently, they are, seemingly or misleading, such as, likeness, and so forth.
simili-paghahambing na ginagamitan ng mnga salitang tulad ng, tulad wari,kapara,tila o mala,gaya ng, kawangis,at iba pa.

when a tender of payment is made in such a form that the creditor could have immediately realized payment if he had accepted the tender, followed by a prompt attempt of the debtor to deposit the means of payment in court by way of consignation, the accrual of interest on the obligation will be suspended from the date of such tender. but when the tender of payment is not accompanied by the means of payment, and the debtor did not take any immediate step to make a consignation, then the interes
kapag ang isang malambot ng pagbabayad ay ginawa sa tulad ng isang form na ang pinagkakautangan ay maaaring magkaroon ng agad na natanto pagbabayad kung siya ay tinanggap ang malambot, na sinusundan ng isang prompt pagtatangka ng may utang na magdeposito ng paraan ng pagbabayad sa hukuman sa pamamagitan ng paraan ng consignation, ang accrual ng interes sa obligasyon ay suspendido mula sa petsa ng naturang malambot. ngunit kapag ang malambot ng pagbabayad ay hindi sinamahan ng paraan ng pagbabayad, at ang may utang ay hindi gumawa ng anumang agarang hakbang upang makagawa ng isang consignation, pagkatapos ay ang interes

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.