The Colored Pebbles of Lake McDonald
The Glacier National Park in the U.S. state of Montana, on the border with Canada, is home to more than 700 lakes, although only 131 of these lakes have names. Approximately 200 lakes are over five acres in size, and a dozen of them exceeds thousands of acres, which in unusual for mountain lakes. Additionally, the waters of the lakes are remarkably clear. This is owning to the year long low temperatures that prohibit the growth of planktons. It is not unusual to see details on the bottom of the lakes at depths of 30 feet or more.
One of the most striking feature of some of these lakes is the presence of a variety of colored rocks and pebbles just below the water surface and on the shores. The rocks range in color from dark red to maroon, and from green to blue. Colored pebbles are seen in abundance on the shores of Lake McDonald on the western side of the park. Lake McDonald is the largest of the lakes of Glacier National Park with a surface area of 6,823 acres. It is also the longest, at over 15 km, as well as the deepest lake at 141 meters.
The color of the rocks is determined by the presence or absence of iron. The bright red rocks found along the Grinnel Glacier trail were deposited in a shallow ocean environment where the iron was oxidized by the tidal exposure to the air. Rocks with this coloration often have old ripple marks or ancient mud crack lines.
The rich green-colored rocks were formed in deeper water than the red rocks. Although these rocks contain the same quantities of iron-bearing minerals, they did not have the same exposure to oxygen and the amount of oxidization was limited.
The green rocks can be seen at Otokomi Lake, while the dark-colored rocks found at the upper end of Lake McDonald, along McDonald Creek and around Trout Lake are the result of subjecting the red and green iron-rich rocks to heat and pressure.
These rocks are actually all around Glacier National Park, and were formed at different eras. When the glaciers came, it broke down the rocks into tiny fragments and the rivers washed them away. Many of these got deposited onto the lakes and “tarns” —lakes formed by filling the bottoms of ice-scoured amphitheaters. Water erosion then rendered them into smooth pebbles.
