The Magma is rising fast!
Angry Magma builds up in secret, far,
When the Magma reaches the surface,
Magma contains vesicles and volcanic edifices are often eroded.
The Magma that surrounds us… turns this place into pretty
That's right. The Magma that surrounds us… turns this place into pretty
are Magmatic eruptions, which involve the decompression of gas within Magma that propels it forward.
The extremely shallow earthquakes(example
1 km) are normally triggered by stress and certainly not by Magma intrusion.
The AVCAN map below shows the"road" the Magma is following while pressurizing the below the island tunnels.
Lava cools fastest at the earth's surface, while Magma, which cools more slowly,
can form larger mineral crystals.
Magma"- this company has been active since 2005,
proving every year that it has rightfully earned its place.
driven by the compression of gas within Magma, the direct opposite of the process powering Magmatic activity.
Once they are active they can let gas,
ash and warm Magma escape in occasionally violent and spectacular eruptions.
At this present stage, potentially eruptible Magma has already been intruded and continues
to be intruded beneath the edifice.
A seismic crisis began at 0300 on 3 April, and along
with deformation, indicted Magma migration towards the surface.
When the conditions in the Magma change, the crystals respond
and produce distinct growth zones that record these changes.".
An orange glow was later observed around the crater at night,
confirming that fresh Magma had indeed reached the surface.
The El Julan coast where the Magma seems to have been blocked(last recorded
group of listed earthquakes)- image Joke Volta.
Roughly every half hour, like volcanic clockwork, Santiaguito's active Caliente lava dome expands,
filling with gas from depressurizing Magma below.
When the Magma reaches the surface,
it often builds a volcanic mountain, such as a shield volcano or a stratovolcano.
When the Magma is not able to expand anymore,
stronger earthquakes will show up(at least in the present activity stage).
While these two words are very similar,
the difference is that the Magma is stuck underground and lava flows above ground.
The Magma seem to be imprisoned very well
at a depth of 18 to 21 km, so no concern there neither.
What an extraordinary action today and not only steam, but also many earthquakes showing the restless power of the Magma.
The first image below shows a detected volcano-tectonic event,
a little quake generated as Magma tries to break through bedrock underground.
Moreover, the crystallized mafic Magma is possibly feeding fluids at shallower
depths for causing the swarm-type earthquake activities in this region.
This does not mean that there should be a higher risk now, only that the Magma pressure is gradually getting higher.
The tectonic plates
are regions that are floating on top of the Magma of the Earth and can move against each other.
It is also an important
fact that this kind of atmosphere is available near the Magma below the ground floor of Bhuprapati.
Scientists have revised amount of Magma coming up to 250 m3/s-
the lava is flowing NE at a rate of 1/2-1 m/minute.