The minimum number of seismic stations needed to determine the location of an earthquake's epicenter is THREE.
The minimum number of seismic stations needed to determine the location of an earthquake's epicenter is THREE.
You would die before you got very far. The earth's crust is 124 miles thick. After that you come upon the mantle (which is about 100-250 miles thick), which consists of molten rock (more commonly known as magma) and is split into three layers: Upper mantle, Mantle, Inner Mantle, each ranging between 600-900 degrees Celsius (or 1,112-1,652 degrees Fahrenheit). Once through the Mantle, you come upon the Inner core which is 1,400 miles thick and made up of Iron and Nickel and has a temperature of 6,692 degrees Fahrenheit. Then you have the inner core which is 750 miles thick and made of solid iron and nickel and has a temperature of about 13,000 degrees Fahrenheit (THAT"S HOTTER THAN THE SUN!) So as you can see, you would be dead before you reach the center of the earth.
About three musicians. Why make things complicated?
Three things that produce heat are a light bulb, fire, and the sun
Viscousity, Pressure, and Chemical composition of the magma.
The properties of the three types of magma depend with viscosity, density and temperature. This is usually determine by heat and how far the molten rock are far from the surface of the earth.
Silica-rich thick magma is called rhyolite. It contains high levels of silica, making it very viscous and typically light in color. Rhyolite is associated with explosive volcanic activity due to the build-up of pressure caused by the slow movement of its thick lava.
Igneous intrusions form when magma cools and solidifies before it reaches the surface. Three common types of intrusion are sills, dykes, and batholiths
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The factor the gebulkdje and the habut
One factor that influences a volcanic eruption is the composition of the lava; the thicker the lava, the more explosive the eruption. Another factor is the level of pressure that forces magma up a pipe or vent; the higher the pressure, the more violent the eruption.
Silica content: Magma with high silica content tends to be more viscous and therefore thicker. Temperature: Hotter magma is usually less viscous and flows more easily. Gas content: The presence of dissolved gases, such as water vapor and carbon dioxide, can affect the viscosity of magma, making it thicker.
Magma is composed of three main components: liquid (molten rock), solid crystals, and gases (such as water vapor and carbon dioxide). The composition of magma varies depending on factors like temperature, pressure, and chemical composition of the rock melting to form it.
Three Million gallons of magma
Your place on the earth, The brightness of the star, Its distance.
When magma is cooled and hardened, it is an igneous rock. That being said, there's only three left and those three are the three types of rocks. Igneous, metamorphic, and sedimentary.