The interior features rugged mountains of volcanic origin. Volcanism is still quite evident on the island, the most popular examples being Dominica's Boiling Lake and "valley of desolation." The boiling lake (the world's second largest) is within a crater and is fed by a waterfall - the boiling is believed to be caused by the heat of a magma chamber beneath the lake. The valley of desolation is a sulfurous valley of volcanic vents and hot springs that inhibits significant plant growth - in stark contrast to the surrounding rain forest. Technically dormant today, this caldera last erupted in 1880. The area that exploded on 4 January 1880 was reported to be "fully nine square miles".