Frozen Waterfalls of Starved Rock

jpeg
jped
jep

Plan to be surprised and awed at the spectacular natural features found here at Starved Rock in Illinois.

Surrounded by the flat, seemingly endless fields of Illinois farm country, a totally different topography is found within the park. Starved Rock was formed thousands of years ago by the melting of glaciers releasing torrents of water. As the water rushed downstream it eroded and stripped away everything in its path except the resistant St. Peter sandstone. It is that sandstone that formed the steep rock walls and the cool dark valleys of the eighteen canyons. When conditions are right cascades of falling water spill down into these gorges, creating the waterfalls so many come here to enjoy.

WATERFALLS
Although you can technically see waterfalls in 14 of the 18 canyons, some of the most scenic waterfalls are found in St. Louis, French, Wildcat, Tonty, Ottawa and Kaskaskia canyons. The best times to see waterfalls are in the spring when the snow and ice melt or after a heavy rainfall.

ICEFALLS
Winter brings a whole new life to the canyons. The freezing and melting that happens during this time of year creates amazing ice sculptures in the canyons. Make sure you come back in the winter to see an icefall – they are spectacular!

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.

And here are a few other great resources.

168268265X

America’s Best Day Hikes

    Great Hiking Trails of the World

Hike & Go Seek – Wauponsee Glacial Trail

Image result for wauponsee glacial trail in winter

“Of all the paths you take in life, make sure one of them is dirt”  – John Muir (Essential Muir – A collection of Muir’s Writings)

The Wauponsee Glacial Trail of Illinois

Trail History

The 275-acre Wauponsee Glacial Trail was acquired between 2004 and 2016.

Prior to the District’s acquisition of the land, it was two abandoned railroads: Chicago, Milwaukee, St. Paul and Pacific from Joliet to Manhattan and the Wabash/Norfolk Southern from Manhattan to Custer Park.

The Trail

The Wauponsee Glacial Trail is a 22.42-mile paved/crushed limestone linear trail consisting of two segments.

The northern segment of the trail travels 2.80 miles from Sugar Creek Preserve north to Rowell Avenue in Joliet. This flat, paved segment of the trail travels through woodland, prairie and wetland.

The southern segment of the trail extends an additional 19.62 miles from Sugar Creek Preserve south to the Kankakee River. This flat, crushed limestone segment of the trail travels through prairie. It is ideal for the following activities:

You will cross bridges and  you might even see some wild turkeys…

Image result for wauponsee glacial trail
Image result for wauponsee glacial trail

https://www.reconnectwithnature.org/preserves-trails/trails/wauponsee-glacial-trail

For some great resources:

168268265X

America’s Best Day Hikes 

Great Hiking Trails of the World

Hike & Go Seek – Great Winter Spots to Visit

Don’t let a snowy forecast stop you from setting aside time for a enjoying the great outdoors.  Head to the woods for a peaceful hike, snow shoeing or cross country skiing.

Turkey Run State Park, Indiana For picturesque views!

download

You’ll marvel at the natural geologic wonders of this beautiful park as you hike along its famous trails. Nestled along State Road 47 southwest of Crawfordsville, the park offers the chance to explore deep, sandstone ravines, walk along stands of aged forests, and enjoy the scenic views along Sugar Creek.

Door County, Wisconsin

Sightseeing along frozen Lake Michigan

download (2)

Many people call Door County the Cape Cod of the Midwest, and that’s no less true in winter, when snow covers the picturesque northeast Wisconsin peninsula. Shops, galleries and inns stay open for visitors who come for cozy shopping and peaceful walks along frozen Lake Michigan beaches. Sleigh rides, trolley tours and wine tastings round out a romantic weekend.

Interstate State Park, Wisconsin and Minnesota

Hardy hikers can snowshoe on fresh white snow

5CF53E53-1DD8-B71B-0BC4DE60DE73ADF6

Interstate Park comprises two adjacent state parks on the Minnesota-Wisconsin border, both names Interstate State Park.  The staddle the Dalles of the beautiful St. Croix River, a deep basalt gorge with glacial potholes and other rock formations.

Southwest Lake Michigan shore

A stunning winter lighthouse road trip landscape!

images

Every winter, lake-effect storms leave southwest Michigan’s lighthouses and sand dunes cloaked in ice and snow.  From South Haven to New Buffalo and beyond winter is the perfect time to  take a road trip  along Lake Michigan, especially since the beautiful scenes of winter are in full force now.

B073RNG5QQ

Winter Hiking Boots

B08HYQMP46

Waterproof Thermal Fleece Hiking Coat

Starved Rock in Winter

jpegjped

jep

Plan to be surprised and awed at the spectacular natural features found here at Starved Rock in Illinois.

Surrounded by the flat, seemingly endless fields of Illinois farm country, a totally different topography is found within the park. Starved Rock was formed thousands of years ago by the melting of glaciers releasing torrents of water. As the water rushed downstream it eroded and stripped away everything in its path except the resistant St. Peter sandstone. It is that sandstone that formed the steep rock walls and the cool dark valleys of the eighteen canyons. When conditions are right cascades of falling water spill down into these gorges, creating the waterfalls so many come here to enjoy.

WATERFALLS
Although you can technically see waterfalls in 14 of the 18 canyons, some of the most scenic waterfalls are found in St. Louis, French, Wildcat, Tonty, Ottawa and Kaskaskia canyons. The best times to see waterfalls are in the spring when the snow and ice melt or after a heavy rainfall.

ICEFALLS
Winter brings a whole new life to the canyons. The freezing and melting that happens during this time of year creates amazing ice sculptures in the canyons. Make sure you come back in the winter to see an icefall – they are spectacular!

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.

And here are a few great resources for some great hikes!!

 Great Hiking Trails of the World

Here’s how to actually enjoy Hanging Lake without all the crowds — The best kept secret by The Denver Post

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.

Hanging Lake, Glenwood Springs, hiking,

via Here’s how to actually enjoy Hanging Lake without all the crowds — The Denver Post

Frozen Waterfalls of Starved Rock

Loyalsock Trail: High Knob and Falls — Appalachian Outdoor Journal

I was a bit apprehensive and excited about a winter trip this year. The ice has not fully left my bones. But it’s difficult to keep me away. It’s been three years since I spent multiple nights out in sub-freezing temperatures while hiking a trail section. And last time, it was -10 (F) for two […]

via Loyalsock Trail: High Knob and Falls — Appalachian Outdoor Journal