Halimbawang sitwasyon na nagpapakita ng gamit ng wika sa lipunan

Tinutulungan tayo ng wika na ipahayag ang aming damdamin at saloobin - natatangi ito sa aming species sapagkat ito ay isang paraan upang maipahayag ang mga natatanging ideya at kaugalian sa loob ng iba`t ibang kultura at lipunan. ... Ang wika ay tumutulong sa pagpapanatili ng mga kultura, ngunit pinapayagan din kaming malaman tungkol sa iba at mabilis na kumalat ng mga ideya.

Explanation: markahan mo ako ng utak utak!

(i speak english btw)

step 1. boil eggs

step 2.eat eggs

step 3. get your hot poonts ready

the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)