If you heated them in a microwave, the moist inside heats much faster than the drier crust does. The inside can get very hot while they are still not too hot to the touch on the outside.
Lithosphere
The Earth's crust is brittle due to the cool temperatures and high pressures near the surface. These conditions cause rocks to be in a solid state and fracture easily when subjected to stress. The brittle nature of the crust allows for the formation of faults and earthquakes when the stress becomes too great.
The lithosphere, i am suggesting, it's otherwise known as "crust". Crust is the top layer of Earth. Everything beneath it is hot, unlike the crust, the crust is cool making it the temperature for our feet not to burn.
The Earth cooled for the first time around 4.5 billion years ago when it formed from a cloud of gas and dust in space. As the planet continued to cool, the surface eventually solidified to form the crust we know today.
The thin cool skin of Earth is called the lithosphere. It consists of the outermost layer of the Earth's crust and a portion of the upper mantle, where tectonic plates are located and move around.
its solid and cool because the outside cools faster than the inside
To use an egg tart mold for baking delicious egg tarts, first prepare the tart dough and filling according to your recipe. Grease the mold with butter or cooking spray to prevent sticking. Press the dough into the mold, making sure to create a thin and even crust. Fill the crust with the egg tart filling and bake according to the recipe instructions. Allow the tarts to cool before removing them from the mold. Enjoy your delicious homemade egg tarts!
To create perfect tarts using a tart mold, follow these tips: Ensure the tart dough is chilled before pressing it into the mold. Press the dough evenly into the mold to create a uniform crust. Blind bake the crust before adding the filling to prevent sogginess. Use a non-stick tart mold or grease it well to prevent sticking. Allow the tarts to cool completely before removing them from the mold for best results.
When magma cools inside the crust, intrusive igneous rocks are formed. These rocks will have larger crystal fragments or pores as an effect of their slow rate of cooling. The rocks will cool slower underneath the crust due to pressure and heat, rather than on the crust. An example of an intrusive igneous rock is granite. When rocks cool on or above the crust they are called extrusive igneous rocks. An example of an extrusive igneous rock is basalt. Granite and basalt are good examples of the comparison between intrusive and extrusive igneous rock because of their significant difference in crystal or fragment sizes. While granite has larger crystals, basalt barely has any at all.Michael Sacco
Intrusive activity is when magma in the mantle or crust starts to cool and crystallize. Igneous rock forms from the crystallization.
It would have to be melted into the earths magma and cool down as either intrusive (inside the earth) or extrusive (on the Earth's crust) igneous rock.
It would have to be melted into the earths magma and cool down as either intrusive (inside the earth) or extrusive (on the Earth's crust) igneous rock.
Igneous rocks that cool quickly beneath earth's crust are known as intrusive rocks. These rocks will form from magma which will cool and solidify quickly.
The lithosphere includes the crust and the very top of the mantle. The lithosphere is cool and brittle.
Water does cool lava, but not instantly. For one thing, lava is a poor conductor of heat, so when lava erupts underwater the outside cools fairly quickly to form solid crust, but the inside remains molten. Second, the water in contact with the lava or crust (which is still quite hot) boils and forms an insulating layer of steam.
the temperture varies
The inner core and the outermost layer of the Earth, called the crust, are completely solid. The inner core is solid due to high pressure, while the crust is solid because it is relatively cool compared to the layers beneath it.