Sie suchten nach: the deadly drug to be in love (Tagalog - Englisch)

you are the one i want to be in love
i wanna love you

i just want us to be in love
i just want us to be in love

how does it feel to be in love?
how does it feel to be in love

calling all the odds to be in my favor
may the odds be forever in your favor

you 're supposed to be crazy in love.
youre supposed to be crazy in love

i forgot what it feels like to be in love
i forgot what i feel like to be in love

better to be in silence.
better to be in silence

do you want to be in my bed?
you want be in my bed?

what would you like to be in the future
what do you like to be in the future

it happens to be that i like you and fallen in love with you already.
it happens to be that i like you and fallen in love with you already

you can never be happy to be in this life.
you can never be to happy in this life

will you love to be in a relationship with a friend of mine
will you love to be in a relationship with a friend of mine

i don 't want you to be your friend i want to be in you
i don't want you be your friend i want to be in you

where do i want to be in the next 3 months, 6 months, 1 year
where do i want to be in the next 3 months, 6 months, 1 year

your subject can divided into what happened in the the past,where you are today and where you hope to be in the future
impromptu speech in past, present,future

well, we haven't known each other long enough to be in love but i do like you a lot and could love you. easily
well, we haven't known each other long enough to be in love but i do like you a lot and could love you. easily

if people don 't make an effort in your life don' t try to be in theirs is not worth it.
if people don’t make an effort in your life don’t try to be in theirs is not worth it

if people don 't make an effort to be in your life don' t try to be in theirs it 's not worth it.
if people don’t make an effort to be in your life don’t try to be in theirs it’s not worth it

if for any reason, any section or provision of this appropriation ordinance is disallowed inif for any reason, any section or provision of this appropriation ordinance is disallowed in budget review or declared invalid by prop budget review or declared invalid by proper authorities, other sections or provisions hereof that are not affected thereby shall continue to be in full force and effect
if for any reasonif for any reason, any section or provision of this appropriation ordinance is disallowed inif for any reason, any section or provision of this appropriation ordinance is disallowed in budget review or declared invalid by prop budget review or declared invalid by proper authorities, other sections or provisions hereof that are not affected thereby shall continue to be in full force and effect , any section or provision of this appropriation ordinance is disallowed inif for any reason, any section or provision of this appropriation ordinance is disallowed in budget review or declared invalid by prop budget review or declared invalid by proper authorities, other sections or provisions hereof that are not affected thereby shall continue to be in full force and effect

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.
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