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Oxygen is less dense.
if it sinks its more dense if it floats its less dense
== == Felsic lava has a higher silica content than mafic lava. Felsic lava is slower moving (high viscosity) than the less viscous mafic lava. Mafic lava is higher in dark minerals and higher in the elements iron and magnesium.
Gases are less dense than solids.
No, oil is less dense than saliva.
Less than 45%
no
Continental crust is made of granite, and forms the continents and areas of shallow seabed close to their shores. It is less dense than the material of the mantle, which consists of mafic rock. Continental crust is then less-dense than oceanic crust, which, due to sea-floor spreading, is hardened mantle/lithosphere.
Oxygen is less dense.
No, it is more dense. If it were less dense it would float.
Yes ammonia is less dense than air
if it sinks its more dense if it floats its less dense
it is less dense
== == Felsic lava has a higher silica content than mafic lava. Felsic lava is slower moving (high viscosity) than the less viscous mafic lava. Mafic lava is higher in dark minerals and higher in the elements iron and magnesium.
If more dense, it will sink when put into water; if less dense it floats.
its has more pressure
Gases are less dense than solids.