The three things that determine how thick or thin magma is temperature, silica content, and gas content.
because it is thin and thick
i dont know
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 three types of magma, named for the rock they form are basaltic, rhyolitic and andesitic. Rhyolitic magma is rich in silica and water vapor.
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, Water and carbon dioxide.
The thickness of magma may be indicated by its measured temperature, its color, and the speed of its flow.
magma can be generated from solid rock by three things:1. decress in PRESSURE2. increase in TEMPATURE3. addition of VOLATILES
The three elements that determine viscosity in magma are:TemperatureSilicaOxides (gases)Viscosity changes the way in which magma will flow. Magma with low viscosity will flow much more easily than high viscosity magma.
Mineral crystals, gases and a slushy mix of molten rock
Igneous intrusions form when magma cools and solidifies before it reaches the surface. Three common types of intrusion are sills, dykes, and batholiths
punk
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.