Frozen Waterfalls, Icefalls & Canyons of the Midwest USA

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Who says you cannot enjoy the Midwest in the Winter. 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.

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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.

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PARKS

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Whispers in the Wilderness

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Wild: From Lost to Found

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Nature’s Silent Message 

Winter Hiking – The Blue Water River Walk – Michigan, USA

As snow and ice cover hiking trails in wintertime, sometimes a hike along a river walk so long as it’s not too winter, is an ideal option.

The Blue Water River Walk is a one mile stretch of land that runs along the St. Clair River in Port Huron, Michigan.  It has it’s own unique naturalized shoreline that is made up from natural rocks, pebbles and boulders while also consisting of many native plants, flowers, trees and shrubs that grow in their own natural landscape and habitat onshore.  The River Walk provides for a place where the natural habitat can thrive and visitors can take a walk along the shoreline and enjoy looking for turtles, watch the freighters or enjoy a nice outdoor picnic.

The River Walk provides for a place where the natural habitat can thrive and visitors can take a walk along the shoreline and enjoy looking for turtles, watch the freighters or enjoy a nice outdoor picnic.

Pedestrian Trial


A very unique and noticeably different feature of the new St. Clair river shoreline along the Blue Water River Walk is the huge boulder and stone structures sticking up from the water just offshore.  These are huge offshore reefs that extend downwards almost 15 feet into the river bottom.  These large boulders weigh as much as 4,000 pounds and are resting on two other layers…recycled slabs of cement on the very bottom and a middle layer of smaller boulders.  All together over 8,000 tons of rock, stone, cement and boulders were used to build these reefs.


Perhaps the most striking different aspect of the new St. Clair River shoreline along the Blue Water River Walk is the huge stone and boulder structures sticking up from the water just offshore. These huge offshore reefs extend down almost 15 feet into the river bottom. The large boulders seen on the surface weigh as much as 4,000 pounds. They are resting on two other layers; recycled slabs of cement on the very bottom and a middle layer of smaller boulders. All together, over 8,000 tons of rock, stone, cement and boulders were used to build these reefs.

These offshore reefs are a critical element to the overall naturalization of the St. Clair River shoreline.  The reefs are there to serve two purposes:  first, they help to knock down the incredibly strong wave energy caused by passing boats and if left unchecked those waves can create serious damage and erosion to the new shoreline.  Secondly, they create new shallow water habitats between the reefs and the shoreline which is critical to the growth and development of small fish, reptiles and amphibians.  

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VIEW ALL SALE ITEMS ON ESTY

Frozen Waterfalls of Starved Rock

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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!

KEEP WARM THIS WINTER

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Midwest Birds

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Beautiful Birds of the Midwest 

The every popular Western Meadowlark.  The western meadowlark has distinctive calls described as watery or flute-like, which distinguish it from the closely related eastern meadowlark. The western meadowlark is the state bird of six states: Montana, Kansas, NebraskaNorth Dakota, Oregon, and Wyoming.

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The Hooded and Common Merganser.  In most places, the common merganser is as much a frequenter of salt water as fresh water. In larger streams and rivers, they float down with the stream for a few miles, and either fly back again or more commonly fish their way back, diving incessantly the whole way. In smaller streams, they are present in pairs or smaller groups, and they float down, twisting round and round in the rapids, or fishing vigorously in a deep pool near the foot of a waterfall or rapid. When floating leisurely, they position themselves in water similar to ducks, but they also swim deep in water like cormorants, especially when swimming upstream. They often sit on a rock in the middle of the water, similar to cormorants, often half-opening their wings to the sun. To rise from water, they flap along the surface for many yards. Once they are airborne, the flight is strong and rapid. They often fish in a group forming a semicircle and driving the fish into shallow water, where they are captured easily. Their ordinary voice is a low, harsh croak, but during the breeding season, they (including the young) make a plaintive, soft whistle. Generally, they are wary, and one or more birds stay on sentry duty to warn the flock of approaching danger. When disturbed, they often disgorge food before moving. Though they move clumsily on land, they resort to running when pressed, assuming a very upright position similar to penguins, and falling and stumbling frequently.

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The Ruffed Grouse.  Ruffed grouse have two distinct morphs: grey and brown. In the grey morph, the head, neck and back are grey-brown; the breast is light with barring. There is much white on the underside and flanks, and overall the birds have a variegated appearance; the throat is often distinctly lighter. The tail is essentially the same brownish grey, with regular barring and a broad black band near the end (“subterminal”). Brown-morph birds have tails of the same color and pattern, but the rest of the plumage is much more brown, giving the appearance of a more uniform bird with less light plumage below and a conspicuously grey tail. There are all sorts of intergrades between the most typical morphs; warmer and more humid conditions favor browner birds in general.

Displaying male

The ruffs are on the sides of the neck in both sexes. They also have a crest on top of their head, which sometimes lies flat. Both genders are similarly marked and sized, making them difficult to tell apart, even in hand. The female often has a broken subterminal tail band, while males tend to have unbroken tail bands, though the opposite of either can occur. Females may also do a display similar to the male. Another fairly accurate sign is that rump feathers with a single white dot indicate a female; rump feathers with more than one white dot indicate a male.

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The red-necked grebe is a migratory aquatic bird found in the temperate regions of the northern hemisphere. Its wintering habitat is largely restricted to calm waters just beyond the waves around ocean coasts, although some birds may winter on large lakes. Grebes prefer shallow bodies of fresh water such as lakes, marshes or fish-ponds as breeding sites.

The red-necked grebe is a nondescript dusky-grey bird in winter. During the breeding season, it acquires the distinctive red neck plumage, black cap and contrasting pale grey face from which its name was derived. It also has an elaborate courtship display and a variety of loud mating calls. Once paired, it builds a nest from water plants on top of floating vegetation in a shallow lake or bog.

The barred owl, also known as northern barred owl or hoot owl, is a true owl native to eastern North America. Adults are large, and are brown to grey with barring on the chest. Barred owls have expanded their range to the west coast of North America, where they are considered invasive.

The common loon or great northern diver is a large member of the loon, or diver, family of birds. Breeding adults have a plumage that includes a broad black head and neck with a greenish, purplish, or bluish sheen, blackish or blackish-grey upperparts, and pure white underparts except some black on the undertail coverts and vent. Non-breeding adults are brownish with a dark neck and head marked with dark grey-brown. Their upperparts are dark brownish-grey with an unclear pattern of squares on the shoulders, and the underparts, lower face, chin, and throat are whitish. The sexes look alike, though males are significantly heavier than females.

Traveling Tuesday – White Pines Forest State Park

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White Pines Forest State Park is an Illinois state park in Ogle County, Illinois, which is a 385 acre park that contains the southernmost remaining stand of native white pine trees in the state of Illinois designated an Illinois Nature preserve in 2001.  The park contains two freshwater streams, dolomite rock formations and a variety of activities generally associated with Illinois state parks.
Among the park’s most distinctive and well known features are the vehicular river crossings.  At three places, crossing Pine Creek, fords were constructed instead of bridges.  The fords offer visitors a chance to actually drive through the creek, though high water frequently closes the crossings.  Hikers are relegated to pedestrian bridges or stepping stones in the creek to cross the stream.  Floods are frequent enough on Pine Creek, a large watershed to the north of the park, that there is an emergency exit from the campground.  When high water closes the fords, the campground is cut off and the emergency exit is the only way out.
The banks of Pine Creek and Spring Creek are lined with large rock and cliff formations that provide habitat to plants ranging from large trees to moss to hanging vines.  The forest undergrowth provides small mammal habitats and among the mammals that can be seen include red squirrels, raccoons, deer and chipmunks.  The creeks are populated with smallmouth bass, rock bass, channel catfish and , when they are stocked by the IDNR, rainbow trout.
The park is Illinois’ third oldest and has become one of the state’s most visited parks hosting over 350,000 visitors each year.  During the warmer months picknicking, camping, lodging, hiking and fishing are available.  The lodge and cabins are listed on the U.S. National Register of Historic Places.

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MORE GREAT PLACES TO VISIT

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Hike & Go Seek – Starved Rock

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All year round, 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.

168268265X

America’s Best Day Hikes     

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OTHER PLACES TO VISIT!!

A030, Theodore Roosevelt National Park, North Dakota, USA, 2001.jpg

Theodore Rooselvelt National Park

This image has an empty alt attribute; its file name is 220px-Temperance_River_State_Park_SHT_Bridge.jpg

Superior Hiking Trail

Maquoketa Caves 02.jpg

Maquoketa Cave State Park