as the snow accumulates in the high mountains, it stacks up and begins to slide down the mountain side as a glacier. as the glacier continues to get pushed from behind (from more incoming snow), it becomes packed into a very dense ice and can travel decades across the country side. sometimes they end by finally giving way to the heat, and turn into a stream of icy cold water. other times they end by crumbling into an ocean like this one.

looking straight down toward the tops of foliage and a simple dirt (mud) road.

Indiana wetlands

hiking through Waimea canyon on Kauai

the American side of Niagara Falls

Sierra Nevada Mountains in late spring as the snow begins to melt at this elevation

This is a highly concentrated salt lake in eastern California that is known for its unique calcareous rock formations (tufas). These structures range from a couple feet to perhaps 15 feet tall and are quite rigid. Most of these structures form on the ground near the shore, but I really enjoyed this grouping when surrounded by water. Plus, the winds coming over a nearby mountain range, produce complex clouds rolling over this area and are usually quite interesting and often stormy in appearance.

northern Indiana