| 41. | According to the analysis of earthquake data in 2013, the magma chamber is long and wide.
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| 42. | It is an exposed magma chamber that formed beneath the surface causing surface swelling to occur.
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| 43. | A magma chamber may lie beneath the volcano.
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| 44. | At high pressures within the magma chamber, gases are dissolved in the melt and are soluble.
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| 45. | During these events a large magma chamber emerged.
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| 46. | Some rocks may have been influenced by the interaction with calcium carbonate in the magma chambers.
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| 47. | The magmas forming this field formed in deep magma chambers with little modification in shallower magma chambers.
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| 48. | The conditions at the magma chamber may be comparable to these under which epithermal mineral deposits form.
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| 49. | The magmas forming this field formed in deep magma chambers with little modification in shallower magma chambers.
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| 50. | Low solubility of carbon dioxide means that it starts to release bubbles before reaching the magma chamber.
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