Oh, dude, a non-example of lava would be like... ice cream! Yeah, lava is hot molten rock flowing from a volcano, but ice cream is definitely not that. So, next time you're at a volcano, don't expect to find any ice cream flowing out of it.
Viscous lava is very sticky and thick and is more felsic (ie it contains more silica) than non-viscous lava. This type of lava makes for a very explosive volcano, because it's so sticky that it sticks to itself and can't exit the volcano until it explodes violently. Non-viscous lava is more runny and is more mafic (has more iron, less silica). Volcanoes with non-viscous lava are less explosive because the lava just runs out slowly and no pressure builds. The Hawaiian islands are formed from volcanoes with non-viscous lava.
Lava flows in Hawaii are an example of Mafic Lava. Mafic Lava is composed of Basaltic rocks of which tend to have high levels of iron and magnesium.
Acid lava comes from composite cones,is slowly moving and viscous while basic lava comes from shield volcanoes,is non viscous, runny and flows faster
mud volcanos
A non-example of magma would be any solid rock found on the Earth's surface or within the Earth's crust. Magma is molten rock located beneath the Earth's surface, whereas solid rocks like granite, basalt, or sandstone are not examples of magma. Additionally, substances such as water, air, or metals are also not examples of magma, as they do not have the same chemical composition or physical properties as molten rock.
Lava flow.
Thick, highly viscous lava.
Viscous lava is very sticky and thick and is more felsic (ie it contains more silica) than non-viscous lava. This type of lava makes for a very explosive volcano, because it's so sticky that it sticks to itself and can't exit the volcano until it explodes violently. Non-viscous lava is more runny and is more mafic (has more iron, less silica). Volcanoes with non-viscous lava are less explosive because the lava just runs out slowly and no pressure builds. The Hawaiian islands are formed from volcanoes with non-viscous lava.
Lava
Lava flow.
Lava flow.
A volcanic eruption is a living example of a lava lamp, where molten lava rises to the surface, cools, and solidifies. The cycle repeats as new lava continues to flow, resembling the movement of the liquid wax in a lava lamp.
Basic lava is low in viscosity.
Lava flows in Hawaii are an example of Mafic Lava. Mafic Lava is composed of Basaltic rocks of which tend to have high levels of iron and magnesium.
It depends on what you need, but a fire staff is the most expensive for non member. There are no two types of staffs together for non-member. Sorry
A geologic event. An example of an igneous rock formation.
Acid lava comes from composite cones,is slowly moving and viscous while basic lava comes from shield volcanoes,is non viscous, runny and flows faster