the main, or central, idea of the passage is specific conditions in the cave of crystals led to the…

the main, or central, idea of the passage is specific conditions in the cave of crystals led to the development of the enormous crystal structures found there. how does the detail in bold develop the main idea? while excavating a tunnel under mexicos naica mountain, silver miners were stunned to discover a cavern full of luminous, elongated underground crystals. composed of the mineral gypsum, some of the crystals extended as far as thirty - six feet into the air. what accounted for these amazing mineral structures? millions of years ago, volcanic eruptions released a large amount of mineral - rich water into the cave, now known as the cave of crystals. one of those minerals was anhydrite, which slowly changes into gypsum when exposed to water. originally, the cave was too hot for this change to take place. eventually, however, the temperature cooled to about 136°f, and gypsum crystals began to form. this process continued as the temperature and other conditions in the cave remained constant for thousands of years. it identifies a condition that led to the formation of gypsum crystals. it challenges the influence of volcanic eruptions on the formation of gypsum crystals.

the main, or central, idea of the passage is specific conditions in the cave of crystals led to the development of the enormous crystal structures found there. how does the detail in bold develop the main idea? while excavating a tunnel under mexicos naica mountain, silver miners were stunned to discover a cavern full of luminous, elongated underground crystals. composed of the mineral gypsum, some of the crystals extended as far as thirty - six feet into the air. what accounted for these amazing mineral structures? millions of years ago, volcanic eruptions released a large amount of mineral - rich water into the cave, now known as the cave of crystals. one of those minerals was anhydrite, which slowly changes into gypsum when exposed to water. originally, the cave was too hot for this change to take place. eventually, however, the temperature cooled to about 136°f, and gypsum crystals began to form. this process continued as the temperature and other conditions in the cave remained constant for thousands of years. it identifies a condition that led to the formation of gypsum crystals. it challenges the influence of volcanic eruptions on the formation of gypsum crystals.

Answer

Answer:

It identifies a condition that led to the formation of gypsum crystals.

Brief Explanations:

El detalle en negrita menciona las erupciones volcánicas que liberaron agua rica en minerales, un factor que contribuyó a la formación de los cristales de yeso en la Cueva de los Cristales. No cuestiona la influencia de las erupciones volcánicas, sino que las presenta como una condición clave para el proceso de formación de los cristales.