Hanging Lake is one of Colorado’s most popular hiking trails in the summer. But the local secret is that it’s best done in the winter.
GLENWOOD CANYON — Long fangs of ice drape from the famous waterfall above Hanging Lake. Water plunges into the turquoise pond, creating a soothing sound, as patches of snow dapple the soaring cliffs that surround one of the most picturesque spots in Colorado.
Hanging Lake is a place so special that it was being loved to death until the U.S. Forest Service partnered with Glenwood Springs last year to control access and limit crowds from May to October — a policy that will be in place again this year — but there’s no need for crowd control in the winter. When we made the 1.2-mile climb of 1,000 vertical feet to the lake recently we saw maybe 30 people, only a dozen or so while we were at the lake itself.
On that hike, we uncovered Hanging Lake’s biggest secret: It is even more beautiful and intoxicating in the winter than in the summer. And it’s a lot less complicated — not to mention less crowded.
via Here’s how to actually enjoy Hanging Lake without all the crowds — The Denver Post
600 million years ago Northern Illinois was part of a broad upland that was undergoing extensive erosion. The erosion wore
the land down to near sea level. Erosion that forms a near sea
level surface is called a peneplain. This peneplain was submerged several times by sea water and several layers of sediment were laid on the surface.
Starved Rock State Park was once covered with 3000-5000
feet of glacial ice on and off over a course of 700,000 years.
Glacial ice can move forwards never backwards. When a glacier is said to be retreating, it is actually melting faster than it is
moving forward. As glacial ice can only move forward, it picks
up rocks and carries them in the ice. When the ice melts, these
rock particles are dropped at the point of melting. All dropped
rock material is called drift. Drift found at the point of melting is
called till. Till is unsorted glacial drift. When the glacier is stagnant, the drift accumulates into a pile called an end moraine.
After the glacier has retreated, it leaves a range of irregular hills
which are the end moraine. The melt waters of the glacier were
so great that they would accumulate behind the moraines and
form vast lakes. The streams that drain these lakes were gigantic compared to today’s streams. The Illinois Valley was
formed by one of these streams.
15,000 years ago during the Wisconsinan Glacial Age, the glacial meltwater of a large lake overtopped the Marseilles Moraine and formed Lake Ottawa behind the Farm Ridge Moraine
that ran north to south along what we call Starved Rock State
Park today. This lake drained when it overtopped the Farm
Ridge Moraine cutting a channel that became the Illinois River.
Repeated meltwater floods of the Kankakee Torrent poured
through the channels cut through the Marseilles and Farm
Ridge Moraines establishing the drainage for the Illinois, Fox,
and Vermillion Rivers. This repeated drainage also cut the outcrops , overlooks, and 18 canyons that you see today.