Results for to be too busy forgetful as well translation from English to Tagalog

i used to be too
dati na rin akong naging

don't be too busy
wag ka na magbigay ng regalo

don't wait for it to be too late
huwag nating hintayin maging huli ang lahat

human ace2 was found to be a receptor for sars-cov-2 as well as sars-cov.
ang human ace2 ay natagpuan na isang receptor para sa sars-cov-2 pati na rin sa sars-cov.

when you're that hot, you don't have to be too good at anything.
kung ganyan ka ba naman kasarap, hindi mo kailangan maging magaling sa kung ano-ano.

student learners are rely on teacher to tell them what is important as well as what needs to be done
umaasa sa mga nag - aaral

meranda right is a set of instructions that are required to be given to a person taken into costumy on suspicion of having committed a criminal act before be can be question by police.purpose of the meranda rights is to ensure such individual are made aware of their right to not make any statement that incriminates themselves as well as their right to have an anttoney
meranda right is a set of instructions that are required to be given to a person taken into costumy on suspicion of having committed a criminal act before be can be questioned by police.purpose of the meranda rights is to ensure such individual are made aware of their right to not make any statement that incriminates themselves as well as their right to have an anttoney

i chose him because of his talented and skilled artist and one of his favorite artworks is "grand old man of philippine art". because apart from the fact that he did it well. that we filipinos have something to be proud of as well
napili ko siya dahil sa galing at husay niyang artist at isa sa mga nagustuhan kung artworks niya ay ang "grand old man of philippine art".kasi bukod sa maganda na maayos pa ang pagkakagawa niya nito.sa tingin ko kaya ginawa niya ito para maipakita na tayong mga pilipino ay may ipapagmalaki rin

because the person who knows how to be grateful possesses respect for himself and for the person who appreciates him as well. because it brings joy to the person you thanked who did the good thing again. because the value of gratitude is simply returning to the good she has accomplished and avoiding the resentment of one another that will bring about a good relationship with each other.
dahil ang taong marunong magpasalamat ay nagtataglay ng respeto sa kanyang sarili at sa taong kanya rin pinasasalamatan. dahil nagbibigay ito ng galak sa taong iyong pinasalamatan na gumawa ulit ng kabutihan. dahil ang halaga ng pasasalamat ay simpleng pagbalik sa mga kabutihan niyang nagawa at maiiwasan ang sama ng loob sa isa't isa na magdadala sa magandang relasyon ng bawat isa.

in summary, i conclude that when we collect and gather information for the someone we want to be monitor is we should able to be patience, be observant and record all that information that we gathered weather it a small or big facts it will be very important to us to configure as well as to pattern what is their day to day activities for the someone we being monitored. additional to that, it would be better to accomplished this tasks if we trace their location first to establish our objective
sa buod, tapusin ko na kapag kinokolekta namin at tinipon ang impormasyon para sa isang taong nais nating masubaybayan ay dapat nating maging mapagpasensya, maging mapagmasid at itala ang lahat ng impormasyon na natipon natin sa panahon ito ay maliit o malaking katotohanan na ito ay magiging napaka mahalaga sa amin upang i-configure pati na rin sa pag-pattern kung ano ang kanilang mga gawain sa araw-araw para sa isang taong sinusubaybayan namin. karagdagan iyon, mas mahusay na maisakatuparan ang mga gawaing ito kung susuriin natin ang kanilang lokasyon upang maitaguyod ang aming layunin

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.