Hike & Go Seek – 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!

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.

The once Historic Route 66, of the most famous roads in the United States that ran from Chicago, Illinois, through Missouri, Kansas, Oklahoma, Texas, New Mexico, and Arizona and ended  in Santa Monica in Los Angeles County, California, covered a total of 2,448 miles.  It has always been iconic for roadside stops….dinners…antiquing…and many historical sites.  Although it longer exists, you can still “get your kicks” on the path it took through the United States on other highways and roads.  In this series, I will highlight the many places you can stop to explore nature along this route….focusing on spots in the Midwest.  Looking for more stops….check out this guide.

Starved Rock State Park

 

And here are a few other great resources.

168268265X      

America’s Best Day Hikes       Great Hiking Trails of the World

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.

The once Historic Route 66, of the most famous roads in the United States that ran from Chicago, Illinois, through Missouri, Kansas, Oklahoma, Texas, New Mexico, and Arizona and ended  in Santa Monica in Los Angeles County, California, covered a total of 2,448 miles.  It has always been iconic for roadside stops….dinners…antiquing…and many historical sites.  Although it longer exists, you can still “get your kicks” on the path it took through the United States on other highways and roads.  In this series, I will highlight the many places you can stop to explore nature along this route….focusing on spots in the Midwest.  Looking for more stops….check out this guide.

Starved Rock State Park

 

And here are a few other great resources.

168268265X      

America’s Best Day Hikes       Great Hiking Trails of the World

 

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.

The once Historic Route 66, of the most famous roads in the United States that ran from Chicago, Illinois, through Missouri, Kansas, Oklahoma, Texas, New Mexico, and Arizona and ended  in Santa Monica in Los Angeles County, California, covered a total of 2,448 miles.  It has always been iconic for roadside stops….dinners…antiquing…and many historical sites.  Although it longer exists, you can still “get your kicks” on the path it took through the United States on other highways and roads.  In this series, I will highlight the many places you can stop to explore nature along this route….focusing on spots in the Midwest.  Looking for more stops….check out this guide.

Starved Rock State Park

 

And here are a few other great resources.

168268265X      

America’s Best Day Hikes       Great Hiking Trails of the World

Hike & Go Seek – Badlands

 

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South Dakota can generally be divided into three regions: eastern South Dakota, western South Dakota, and the Black Hills. The Missouri River serves as a boundary in terms of geographic, social, and political differences between eastern and western South Dakota. The geography of the Black Hills, long considered sacred by Native Americans, differs from its surroundings to such an extent it can be considered separate from the rest of western South Dakota. At times the Black Hills are combined with the rest of western South Dakota, and people often refer to the resulting two regions divided by the Missouri River as West River and East River.

Trekking The National Parks: The Family Board Game (Second Edition)

Trekking the National Parks Family Board Game

 

Badlands National Park

 

Eastern South Dakota generally features higher precipitation and lower topography than the western part of the state. Smaller geographic regions of this area include the Coteau des Prairies, the Dissected Till Plains, and the James River Valley. The Coteau des Prairies is a plateau bordered on the east by the Minnesota River Valley and on the west by the James River Basin.  Further west, the James River Basin is mostly low, flat, highly eroded land, following the flow of the James River through South Dakota from north to south.The Dissected Till Plains, an area of rolling hills and fertile soil that covers much of Iowa and Nebraska, extends into the southeastern corner of South Dakota. Layers deposited during the Pleistocene epoch, starting around two million years ago, cover most of eastern South Dakota.  These are the youngest rock and sediment layers in the state, the product of several successive periods of glaciation which deposited a large amount of rocks and soil, known as till, over the area.

 

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National Parks 18″ x 24″ Collector’s Series Puzzle 

 

Due to a higher elevation and level of precipitation, the Black Hills ecology differs significantly from the plains.  The mountains are thickly blanketed by various types of pines, including ponderosa and lodgepole pines, as well as spruces. Black Hills mammals include deer, elk (wapiti), bighorn sheep, mountain goats, pine marten, and mountain lions, while the streams and lakes contain several species of trout.

 

A Walk in the Woods by Bill Bryson

 

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Columbia Waterproof Hiking Shoes

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Bear Creek Lake Park — Linhart Photography – Hiking and Travel Adventures

Bear Creek Lake Park

Round-Trip Length:  3.64 miles
Start Elevation:  5,766’
High Point:  6,664’
Elevation Change:  204’
Skill Level:  Easy
Trailhead Location:   East of C470 at Morrison Road and S. Indiana Street (not the official park entrance).  Park along the shoulder of Morrison Road and S. Indiana Street.  The trail is on the south side of the road.

We decided to get out on this nice day and explore a trail close to home.  We were hoping this trail would not be too crowded and it wasn’t. Bear Creek Lake Park is a 2,624-acre park with 15 miles of multi-use trails.

We headed south along the Ward Canal.  Views to the west of the foothills.

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A view looking back up from the direction we had come.

via Bear Creek Lake Park — Linhart Photography – Hiking and Travel Adventures

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Nikon Complete Kit

 

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Scratch off map – National Parks

Hiking Garden Of The Gods in Colorado USA

The Garden of the Gods, a registered National Natural Landmark, is located in Colorado Springs CO and is completely free to visit.  Set at the foothills of the Rocky Mountains, the main draw of the park is to marvel at the red sandstone rock formations scattered throughout.  There are 17 different formations altogether and many different hiking trails totalling 21 miles.  The Visitor Centre is a good place to start, you can pick up a free map which is helpful as there isn’t a huge amount of signage out on the trails.

Garden of the Gods Hiking

The Visitor Centre also has one of my favourite views in the park.  You can see North Gateway Rock, South Gateway Rock and Gray Rock in front of the Rocky Mountains.  I like the contrast of colours, from the orange/brown in the front to the green of the lower mountains and then the white of the snow capped Pikes Peak.

Garden of the Gods Colorado USA

via Hiking Garden Of The Gods in Colorado USA — Between England & Iowa

Trekking The National Parks: The Family Board Game (Second Edition)

Trekking the National Parks Family Board Game

 

 

National Parks Badges Puzzle 

 

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Nikon Complete Kit

 

Rewild through Birding

Shallow Focus Photography of Gray and Orange Bird

A rewilding, brought about first through neglect and now through intentional human effort, is occurring on all over the world and certainly here in the Midwest. Over the years, I have discovered unique beauties on ambling adventures along the Wisconsin and Michigan Shoreline, and even in the heart the city…downtown Chicago.

 

Even this time of year you can spot all types on many of the hiking trails the area has to offer.   But if you really want to view all types, try the Montrose Point Bird Sanctuary listed below.

One such spot… The Montrose Point Bird Sanctuary can be found by following Montrose Avenue east until crossing Lake Shore Drive and into Lincoln Park.  Visit the magic hedge, on the west side of the sanctuary, but stay on the trails as much as possible in order to not disturb the nesting and resting Birds. Make sure you take the path in One Direction and return in the opposite direction in order to navigate the whole area.

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Wren Home

 

Don’t forget to walk down to the pier where you will see rare ducks,  loons, and possibly peregrine falcons.

A small bird creeps out of a thicket and is greeted by flashing lights and muffled whispers. Welcome to the celebrity life of a bird along the “Magic Hedge.”

Focus Photography of Flying Hummingbird

A small finger curling out into the lake, Montrose Point Bird Sanctuary can boast in having over 300 species recorded, including some of the rarest birds ever recorded in the state.  A small stretch of low-lying bushes and small trees on the west side of the sanctuary in particular have been a magnet for migrating songbirds and rarities.  Some would say that the hedge seems to bring birds in like magic.  The nickname for this spot is fitting: “The Magic Hedge.”

 

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Birds of the Backyard

Everglades National Park: Mangrove Forest — National Parks With T

Welcome back to National Parks and other public lands with T!

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Everglades National Park has a number of videos on their website for the housebound to explore during the Covid-19 shutdown, including this video with Ranger Ally of the mangrove forest.

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In 2016, we took the Mangrove Wilderness tour with the only company licensed to do boat excursions inside the National Park boundaries. You can find them by clicking here.

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The tour was very similar to what is shown in the video, without the corny acting.  If you have 10 minutes to spare, I encourage you to watch the video. I enjoyed re-living this lovely journey through the Everglades.

via Everglades National Park: Mangrove Forest — National Parks With T

 

Trekking The National Parks: The Family Board Game (Second Edition)

Trekking the National Parks Family Board Game

 

 

National Parks Badges Puzzle 

 

B07PKL46PN

Nikon Complete Kit

 

 

National Park Week: Z I O N — Roamin Moens

National Parks really were “America’s Best Idea.” So many of my big life moments happened or were about national parks. I can remember moments exactly how they happened from the memories I have captured. Zion National Park will forever hold a special place in my heart because it was the first National Park I had […]

via National Park Week: Z I O N — Roamin Moens

 

National Parks Badges Puzzle 

 

Mind Travel: National Park Week and Earth Day — Jane Lurie Photography

Come celebrate nature with me.

“I wish that all of nature’s magnificence, the emotion of the land, the living energy of place could be photographed.”

~Annie Leibovitz

Landscape Photography, National Park, Earth Day, Inspiration, Travel

Landscape Photography, National Park, Earth Day, Inspiration, Travel

via Mind Travel: National Park Week and Earth Day — Jane Lurie Photography

 

Trekking The National Parks: The Family Board Game (Second Edition)

Trekking the National Parks Family Board Game

 

 

National Parks Badges Puzzle 

 

B07PKL46PN

Nikon Complete Kit