How to protect yourself from social media abuse​

The Internet is an integral asset for correspondence. Figure out how to utilize the Internet, keep your eyes open for great and troublemakers, and take advantage of what the Internet offers. Keep your own data separate from your expert job. Utilize various personas for various jobs. Eliminate area information from pictures and recordings prior to posting. Mood killer application admittance to area. Try not to uncover your area openly posts. They're more valuable than any gems. Shield them from both physical and advanced altering. Use encryption and solid access qualifications. Discover partners and set up an arrangement for managing on the web badgering, doxing and different types of misuse. Try not to take care of the savages! They don't merit your consideration. Try not to let cyberbullies sabotage what you are doing. Show them you are not apprehensive. Others will remain with you. Request help. Post for stick phishers. Check prior to associating with another person. In the event that something appears to be unrealistic, don't confide in it.

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)