Furry Feathered Friday – Birds with Benefits

Shallow Focus Photography of Gray and Orange Bird

Oh, the many (often unrealized) benefits to birding. Did you know birding:

  • Bird watching develops patience. …
  • Bird watching will get your children to go outside. …
  • Bird watching allows for introspection and contemplation. …
  • Bird watching can improve cardiovascular health. …
  • Bird watching gives you an excuse to travel. …
  • Bird watching builds a sense of community. …
  • Bird watching quickens reflexes.

One of my favorites, The mourning dove is a member of the dove family, Columbidae. The bird is also known as the American mourning dove or the rain dove, and erroneously as the turtle dove, and was once known as the Carolina pigeon or Carolina turtledove.

It is one of the most abundant and widespread of all North American birds. It is also a leading gamebird, with more than 20 million birds (up to 70 million in some years) shot annually in the U.S., both for sport and for meat. Its ability to sustain its population under such pressure is due to its prolific breeding; in warm areas, one pair may raise up to six broods of two young each in a single year. The wings make an unusual whistling sound upon take-off and landing, a form of sonation. The bird is a strong flier, capable of speeds up to 88 km/h (55 mph).  It is the national bird of the British Virgin Islands.

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1000 Piece Wooden Puzzle

Mourning doves are light grey and brown and generally muted in color. Males and females are similar in appearance. The species is generally monogamous, with two squabs (young) per brood. Both parents incubate and care for the young. Mourning doves eat almost exclusively seeds, but the young are fed crop milk by their parents.

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Yellow rail adults have brown upperparts streaked with black, a yellowish-brown breast, a light belly and barred flanks. The short thick dark bill turns yellow in males during the breeding season. The feathers on the back are edged with white. There is a yellow-brown band over the eye and the legs are greenish-yellow.

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Love the Sandhill Crane!  A species of large cranes of North America and extreme northeastern Siberia. The common name of this bird refers to habitat like that at the Platte River, on the edge of Nebraska’s Sandhills on the American Plains. This is the most important stopover area for the nominotypical subspecies, the lesser sandhill crane (Antigone canadensis canadensis), with up to 450,000 of these birds migrating through annually. (wiki)

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Gosky Prism Binoculars

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 National Geographic Birds 

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  Birds of the Midwest

Hike & Go Seek – Cooper Harbor

Aerial view of Copper Harbor

Looking for some of the funnest and most scenic trails around Michigan. Copper Harbor is your spot. It is an all-season resort town in northeastern Keweenaw County, Michigan located on the Keweenaw Peninsula which juts out from the Upper Peninsula of Michigan into Lake Superior. Due to its natural environment and surroundings it is a popular tourist destination within the Great Lakes region.

One popular spot for visitors is Hunter’s Island which is the name of a non-hilly point running out from the west into Lake Superior.  It was named for an early settler of the area named Mr. Hunter who owned a tract of land on what is now Hunter’s Point or Hunter’s Island.   Situated at the opening of the harbor itself is the historic Copper Harbor Lighthouse built in 1866, replacing an earlier lighthouse made in 1849.  It is only accessible via a short ride in a compact open vessel from the Copper Harbor marina.  Exhibits inside the lighthouse museum cover both the lighthouse history along with the local shipwreck culture of the area.

Copper Harbor is located in Michigan

 Another popular site known as “the most beautiful road in Michigan” is the Brockway Mountain Drive that is an 8.8 mile route that follows the backbone of a 753-foot-high ridge between the towns of Copper Harbor and Eagle Harbor and is the highest paved road between the Rocky Mountains to the west and the Allegheny Mountains to the east.  Constructed during the 30’s, this very picturesque road offers stunning views of Lake Superior and Keweenaw Penisula as well as the archipelago of Isle Royale.

wiki

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Snow shoes

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Columbia Waterproof Hiking Shoes

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Wild: From Lost to Found

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!

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.

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America’s Best Day Hikes

    Great Hiking Trails of the World

On Location – Glacier Park in Illinois

Although a bit barren in January, Glacial Park Conservation Area offers 3,432 acres of recreation including a wide array of prairies, wetlands and savannas.  There are over eight miles of hiking trails with a beautiful backdrop of hickory trees, oak trees. and wildflowers. It is the home for over 41 species of state endangered animals and plants. And a great spot for birding.

Trekking the Interpretive Nature Trail On this 2 mile trek, call  the edge, you will search for owls, deer, wood ducks and blue birds.  This “edge” offers the perfect combination of of both woodland and grassland which is exactly what these animals need.  Many types of berries, nuts and seeds are available.

Trekking the  Plant Community Interpretive Trial

This open woodland is a savanna, hosting plant both native and non native to the area.  Some of the plants include bottlebrush grass, joe pye weed, and mayapple.   The green plants here produce their own food by trapping the energy of the sun.  They then support a wide array of organisms throughout the savanna. Here there is a very healthy ecosystem and therefore a vast biodiversity.

Midwestern Birds: Backyard Guide - Watching - Feeding - Landscaping - Nurturing - Indiana, Ohio, Iowa, Illinois, Michigan, Wisconsin, Minnesota, ... Dakota (Bird Watcher's Digest Backyard Guide)

Midwestern Birds 

National Geographic Field Guide to the Birds of North America, 7th Edition

  National Geographic Birds

Geology of Glacial Park

12,000 years ago glaciers were in this park.  After leaving they left the land shaped into unique land forms and bringing rocks and till from Canada.   Because of so much till, the bedrock was buried and after breaking down, plants were able to grow in this new fertile soil.  This area then became of the top regions for agriculture.

Here are a few other great resources.

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America’s Best Day Hikes     

 Great Hiking Trails of the World

Hike & Go Seek – Castle Rock State Park

 Located in the Rock River Hills region of Illinois you will find 2000 acres of rolling topography. Awesome rock formations and ravines abound as well as unique northern plant associations.

Enjoy six miles of trials and you will encounter woodland animals and birds inhabiting the park. Bring your camera!

How did it get it’s name? A sandstone bluff along the river. Castle Rock is a bluff of exposed St. Peter Sandstone from the Middle Ordovician period. Newly exposed sections are white quartz, while older areas have browner tints from the formation of limonite. The bluff is along the axis of the Sandwich Fault Zone, separating Ordovician exposures from those of the Cambrian period.

Castle Rock State Park was one of eleven state parks slated to close indefinitely on November 1, 2008 due to budget cuts by former Illinois governor Rod Blagojevich. After delay, which restored funding for some of the parks, a proposal to close seven state parks and a dozen state historic sites, including Castle Rock, went ahead on November 30, 2008. After the impeachment of Illinois Governor Blagojevich, new governor Pat Quinn reopened the closed state parks in February.  In March 2009 Quinn announced he is committed to reopening the state historic sites by June 30, 2009.

https://en.wikipedia.org/wiki/Castle_Rock_State_Park_(Illinois)

1732352224

Nature’s Silent Message 

Hike & Go Seek – Kankakee River State Park

Kankakee River State Park, a treasured and historical area for centuries, is an Illinois state park on 4,000 acres. Originally, 35 acres (14 ha) of land was donated by Ethel Sturges Dummer for the creation of the state park in 1938. Another 1,715 acres (694 ha) was donated by Commonwealth Edison in 1956, which again donated more land in 1989. The area includes three amazing river islands.

There are plenty of hiking trails throughout the park that go through different ecosystems and different park features. While some go along the Kankakee River, with places to sit along the river, others go into the forests or along Rock Creek, a tributary of the Kankakee River that cuts through the ground, creating a gorge with cliffs. The trails are very diverse. The site is very good for mushroom hunting.

Rock Creek on Kankakee River2.jpg

The park’s trails stretch along both sides of the river. Hiking, biking and cross-country ski trails are on the river’s north side. Horse and snowmobile trails can be found on the south. A 3-mile route along Rock Creek lets hikers take in the beauty of limestone canyons and a waterfall. A bicycle trail begins at Davis Creek Area and travels 10.5 miles of trails in the form of a linear trail along the river and a loop in the west end of the park.

https://en.wikipedia.org/wiki/Kankakee_River_State_Park

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Whispers in the Wilderness

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READ FOR FREE

Wilderness Wednesday

See the source image

COVERING FIVE STATES (IL, IA, NE, UT, WY)

Explore the Mormon Pioneer National Historic Trail across five states to see the 1,300-mile route traveled by Mormons who fled Nauvoo, Illinois, to the Great Salt Lake Valley in 1846-1847

Martins Cove, Wyoming

A Brief History

The story of the Mormon Trail is rooted in the beginnings of a unique American religion. In 1827, 21-year-old Joseph Smith announced that he had unearthed a set of golden plates, inscribed with the tenants of God’s true church. Smith said that he had been directed to the plates by an angel named Moroni, who also had given him divine tools for translating the ancient inscriptions into English. Smith used these to produce new Scripture called the Book of Mormon. In 1830, in western New York, he organized a legal entity that would become The Church of Jesus Christ of Latter-day Saints. His followers, who regarded Smith as a prophet, became known as Mormons.

Important differences between mainstream Christianity and Mormon doctrine quickly emerged, but it was primarily hostilities over land, business, and politics that caused Smith repeatedly to move church headquarters. Driven out of Missouri in 1838, the Mormons finally settled along a bend of the Mississippi River in Illinois. There they established a community they called Nauvoo, a Hebrew word meaning “beautiful place.” It was at Nauvoo that Smith cautiously began introducing the Old Testament practice of “plural marriage,” or polygamy, among select church leaders.

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READ FOR FREE

Thousands of converts flocked to Nauvoo, soon making it the largest town in Illinois. Neighbors initially welcomed the orderly, industrious settlers despite their religious differences. But relations gradually soured, with complaints centering on Mormons’ clannish business practices, accusations of theft, their electoral sway, and Smith’s political aspirations. Meanwhile, dissent emerged within the church as rumors leaked of secret plural marriages. After an opposition newspaper publicly accused the prophet and other leaders of polygamy, Nauvoo’s city council and Smith declared the paper a public nuisance and Smith ordered destruction of its press. For that he and others were arrested and jailed at Carthage, Illinois. On June 27, 1844, a mob broke into the jail and murdered Joseph Smith and his brother Hyrum. Other vigilantes attacked Mormon farms around Nauvoo in an attempt to expel them.

Brigham Young stepped up as Smith’s successor and began planning an orderly, spring 1846 evacuation of some 15,000 faithful to the Great Basin, Mexican-held territory beyond the Rocky Mountains. However, as anti-Mormon violence heated, Young decided to organize a vanguard of church leaders to depart in late winter, hoping that would pacify the vigilantes until the main body of Mormons could start west in April. On February 4, 1846, the first wagons ferried across the Mississippi to Iowa. This group halted after five miles and set up camp at Sugar Creek for a lengthy wait as Young and his associates concluded business at Nauvoo. Meanwhile others, anxious not to be left behind, drifted over to join the Sugar Creek camp. Young’s vanguard company unexpectedly swelled from his intended 1,800 emigrants to around 3,000—many without their own wagons and provisions.

https://www.nps.gov/mopi/index.htm

0996962662

Whispers in the Wilderness

B005CRQ4XI

Wild: From Lost to Found

1732352224

Nature’s Silent Message 

Starved Rock in Winter

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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

Hike & Go Seek – White Pines Forest State Park

White Pines Forest State Park Pine Stand2.JPG

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.

Books you might like:

A Walk in the Woods by Bill Bryson

B005CRQ4XI

Wild: From Lost to Found

0996962662

Whispers in the Wilderness

 Lost 

And just released last month by Scott Stillman…Nature’s Silent Message

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Nature’s Silent Message