{दर्द}⭐===⭐ सभी इंसानों में है मगर कोई दिखाता है तो कोई छुपाता है {प्यार}⭐===⭐ सभी करते है मगर कोई दिल से करता है तो कोई दिमाग से करता है {जिन्दगी}⭐===⭐ सभी जीते है मगर कोई सब खुछ आने के बाद भी दुखी रहते है तो कोई लुटा के खुश रहते है {दोस्ती}⭐===⭐ सभी करते है मगर कुछ लोग निभाते है कुछ लोग अजमाते है {अहसास} ⭐===⭐सबको होता है मगर कोई महसूस करता है तो कोई समझ नही पता {हमसफर}⭐===⭐ सभी है मगर कोई साथ देता है तो कोई छोड़ देता है {रिश्ता} ⭐===⭐कई लोगो से होता है मगर कोई प्यार से निभाता है तो कोई नफरत से निभात है✞✞✞☽➪good night all friends

I don't know the language btw go to not .com k thanks

Explanation:

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what language is that??

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)

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