Lava that contains a greater amount of silica will flow slower and more sluggishly. The silica affects the viscosity of the lava making it thicker and therefore moving at a slower pace.
A page flow is a directory of web application files which work together to implement a user interface feature.
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There are several different types of flow charts. The main function of a flowchart is to see the steps and process of something from the beginning to the end.
No dumb-as5
They don't have one. They go with the flow.
Water gas a greater influence. Regardless of the amount of silica present, an eruption cannot be explosive if there is no gas present, and the chief gas is water vapor. Magma that is high in silica but low in gas content will be slowly extruded to form a lava dome or a very thick lava flow.
If the basalt flow contains air bubbles and pockets and there is a spring that contains silica then the silica can deposit into the air bubbles (the air bubbles are known as Amygdaloidal basalt or vesicles) If the silica deposits slowly and the conditions are correct then precious opal can form. Two examples of this would be in California at the Nowak and the Barnett mines.
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.
it is normally intermediate flow because of the silica content.
it is normally intermediate flow because of the silica content.
It determines high silica or low silica. It will determine if it is sticky or not, or if it flows fast or slow. *high in silica~Sticky, and slow. Will not flow easily. *low in silica~Fact, not sticky. Will flow easily.
it is normally intermediate flow because of the silica content.
A holocene volcano is a volcano that is made up of several different particles of holocene (Chemical gases) that come from basaltic silica or granitic silica. A quiet flow makes a slow and steady amount of various amounts of holocene, while the granitic flow, the explosive flow, makes a fast amount. High viscosity and low viscosity are also parts and particles of placements of holocene.
The amount of silica and water affect the viscosity of the magma. The more viscous the magma, the slower the flow rate and the shorter and the thicker the flows. Silica makes for a more viscous magma.
The thickness of magma may be indicated by its measured temperature, its color, and the speed of its flow.
Silica will determine if the lava is hot and runny or thick and slow!
Lava with high silica content will erupt explosively, if it has low silica content it will flow.