Plasticity allows the brain to cope better with the indirect effects of brain damage resulting from inadequate blood supply following a stroke. Fundamentally, the nervous system needs to rearrange itself in order to adapt to the unfolding situation that it faces.

Neuroplasticity – or brain plasticity – is the ability of the brain to modify its connections or re-wire itself. For example, there is an area of the brain that is devoted to movement of the right arm. Damage to this part of the brain will impair movement of the right arm.

Neural plasticity, also known as neuroplasticity or brain plasticity, can be defined as the ability of the nervous system to change its activity in response to intrinsic or extrinsic stimuli by reorganizing its structure, functions, or connections.

1 : the quality or state of being plastic especially : capacity for being molded or altered. 2 : the ability to retain a shape attained by pressure deformation.

For example, rolling steel into a particular shape (like rebar for construction) involves plastic deformation, since a new shape is created. Plastic wrap is an example of plasticity. After stretched—it stays stretched. Most materials have an amount of force or pressure for which they deform elastically.

Plasticity, ability of certain solids to flow or to change shape permanently when subjected to stresses of intermediate magnitude between those producing temporary deformation, or elastic behaviour, and those causing failure of the material, or rupture (see yield point).

Plasticity in a crystal of pure metal is primarily caused by two modes of deformation in the crystal lattice: slip and twinning. Slip is a shear deformation which moves the atoms through many interatomic distances relative to their initial positions.

(plăs-tĭs′ĭ-tē) The ability to change and adapt, especially the ability of the central nervous system to acquire alternative pathways for sensory perception or motor skills.

mantle

Inner core

core

If we subdivide the Earth based on rheology, we see the lithosphere, asthenosphere, mesosphere, outer core, and inner core. However, if we differentiate the layers based on chemical variations, we lump the layers into crust, mantle, outer core, and inner core.

Our planet sits in a small corner of the Milky Way galaxy, 25,000 light-years from the galactic center and 25,000 light-years away from the rim, according to Universe Today.

crust

There are three main sources of heat in the deep earth: (1) heat from when the planet formed and accreted, which has not yet been lost; (2) frictional heating, caused by denser core material sinking to the center of the planet; and (3) heat from the decay of radioactive elements.

The Earth’s inner core is thought to be slowly growing as the liquid outer core at the boundary with the inner core cools and solidifies due to the gradual cooling of the Earth’s interior (about 100 degrees Celsius per billion years).

Your ‘down’ trip would have gravity increasing your speed every second as you are pulled towards the core, propelling your way through Earth until you reached the center. Once there, gravity would begin acting as a buffer against you, making your ‘up’ trip increasingly slower.

The Earth’s core same temperature as the surface of the sun. It’s a mystery that has puzzled generations of scientists: At the very center of our planet, within a liquid outer core, is a Pluto-sized orb of solid iron. That’s right, solid — even though it’s nearly the same temperature as the surface of the sun.

Supernova

The corona is the outer atmosphere of the Sun. It extends many thousands of kilometers (miles) above the visible “surface” of the Sun, gradually transforming into the solar wind that flows outward through our solar system. The material in the corona is an extremely hot but very tenuous plasma.

At its surface (called the “photosphere”), the sun’s temperature is a whopping 10,000° F! That’s about five times hotter than the hottest lava on Earth. A temperature of 27 million degrees Fahrenheit is more than 12,000 times hotter than the hottest lava on Earth!

copper

Bow Tie Nebula

When geologists refer to magma, they’re talking about molten rock that’s still trapped underground. If this molten rock makes it to the surface and keeps flowing like a liquid, it’s called lava. They’re also the hottest variety of magma, reaching temperatures between 1,800 degrees to 2,200 degrees Fahrenheit.

You get burned, because lava has a really high temperature. Now if you touch it through an insulator, it’s still really hot but you might not get burned if you pull away fast enough. The lava is kind of viscous, so it’d be like stepping on really springy play dough.

While lava can be as hot as 2200 F, some flames can be much hotter, such as 3600 F or more, while a candle flame can be as low as 1800 F. Lava is hotter than a typical wood or coal-buring fire, but some flames, such as that of an acetylene torch, is hotter than lava.

Most lava is very hot—about 2,000 degrees Fahrenheit. At those temperatures, a human would probably burst into flames and either get extremely serious burns or die. Unlike a lake, people won’t immediately sink into lava.

The lava torture won’t be much of a problem then. However, heat transfer will still take place, which would mean an excruciating amount of pain. One’s body temperature will rise off the charts and one will feel one’s whole body burning for a few seconds.

Soldier survives 70-foot fall into active Hawaiia’s Kilauea volcano. A 32-year-old soldier attempting to get a better view inside of Hawaii’s Kilauea volcano fell in Wednesday night, authorities said. He was seriously injured, but survived after falling 70 feet into the volcano’s crater.

While your lungs would almost undoubtedly be irrevocably charred from the hot air above the lava (assuming relatively static air conditions over the lava), it takes about 80 seconds for the average human to fall unconscious from lack of oxygen, and I highly doubt your body will last that long.