Volcanic fire and glacial ice are natural enemies. Eruptions at glaciated volcanoes
typically destroy ice fields, as they did in 1980 when 70 of Mount Saint Helens
ice cover was demolished. During long dormant intervals, glaciers gain the upper hand
Line cutting deeply into volcanic cones and eventually reducing them to rubble. Only rarely
(5) do these competing forces of heat and cold operate in perfect balance to create a
phenomenon such as the steam caves at Mount Rainier National Park.
Located inside Rainier's two ice-filled summit craters, these caves form a labyrinth
of tunnels and vaulted chambers about one and one-half miles in total length. Their
creation depends on an unusual combination of factors that nature almost never brings
(10) together in one place. The cave-making recipe calls for a steady emission of volcanic
gas and heat, a heavy annual snowfall at an elevation high enough to keep it from
melting during the summer, and a bowl-shaped crater to hold the snow.
Snow accumulating yearly in Rainier's summit craters is compacted and compressed
into a dense form of ice called firm, a substance midway between ordinary ice and the
(15) denser crystalline ice that makes up glaciers. Heat rising from numerous openings (called
fumaroles) along the inner crater walls melts out chambers between the rocky walls
and the overlying ice pack. Circulating currents of warm air then melt additional openings
in the firm ice, eventually connecting the individual chambers and, in the larger of
Rainier's the crater's, forming a continuous passageway that extends two-thirds of the
(20) Way around the crater's interior.
To maintain the cave system, the elements of fire under ice must remain in equilibrium
Enough snow must fill the crater each year to replace that melted from below. If too
much volcanic heat is discharged, the crater's ice pack will melt away entirely and the
caves will vanish along with the snows of yesteryear. If too little heat is produced, the
(25) ice, replenished annually by winter snowstorms, will expand, pushing against the
enclosing crater walls and smothering the present caverns in solid firm ice.
The word "they" in line 2 refers to
(A) fields
(B) intervals
(C) eruptions
(D) enemies