Newgrange VIII

The Newgrange facade and kerbstones consists of stones from various locations, believed to be transported by sea and river.

The Newgrange façade and entrance of today is a creation from the large quantity of small stones unearthed and conserved during excavation given form by a steel-reinforced concrete retention wall. 

The brilliant white quartz cobblestones were collected from the Wicklow Mountains, 31 miles to the south.  Our guide called them “sunstones” for the way they reflect sunlight. In the following photograph is white quartz, the same excavated 1967-1975 from the Newgrange site and incorporated into the facade, I collected from “Miners Way” along R756 (above Glendalough).

You can also see in these photographs dark rounded granodiorite cobbles from the Mourne Mountains, 31 miles to the north.  Dark gabbro cobbles from the Cooley Mountains and banded siltstone from the shore at Carlingford Lough both locations on the Cooley Peninsula where my mother’s family still has farms.

The stones may have been transported to Newgrange by sea and up the River Boyne by fastening them to the underside of boats at low tide. None of the structural slabs were quarried, for they show signs of having been weathered naturally, so they must have been collected and then transported, largely uphill, to the Newgrange site. The granite basins found inside the chambers also came from the Mournes.

Geological analysis indicates that the thousands of pebbles that make up the cairn, which together would have weighed about 200,000 tons, came from the nearby river terraces of the Boyne. There is a large pond in this area that is believed to be the site quarried for the pebbles by the builders of Newgrange.

Most of the 547 slabs that make up the inner passage, chambers, and the outer kerbstones are greywacke. Some or all of them may have been brought from sites either 3 miles away or from the rocky beach at Clogherhead, County Louth, about 12 miles to the northeast.

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Copyright 2023 Michael Stephen Wills All Rights Reserved

Cliff Stairs IV

A Wall with Moss Padding

Pam examining thick moss growth on the sedimentary rock of Treman gorge. These layers of shale, sandstone, siltstone formed at the bottom of a broad, shallow sea over 380 million years ago.

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Towards the bottom of the 223 Cliff Stair steps moss takes over the Devonian shale of the cliff wall surface. Here, the cliff shelters the wall from sunlight 365 days a year.

Robert H. Treman New York State Park.

Click for a slideshow of this sequence Lucifer Falls and Cliff Stair Views
Copyright 2023 All Rights Reserved Michael Stephen Wills

Cliff Stairs III

“Red-shanks”

This geranium species (scientific name Geranium robertianum) are also called “Herb-Robert” for a reputed ability to ward off disease.

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Scottish Highlands residents call these wild geraniums “red-shanks” for the deep red color of the stalks, seen in both photographs.

Robert H. Treman New York State Park.

Source, “How to Know the Wildflowers” by Mrs. William Star Dana, 1989, Houghton Mifflin, Boston.

Click for a slideshow of this sequence Cliff Stair Views
Copyright 2023 All Rights Reserved Michael Stephen Wills

Cliff Stairs II

read the sign

Each autumn, species of fern turns yellow towards a winter death. Here we see growing from Devonian shale, both the yellowed and desiccated fern fronds. Robert H. Treman New York State Park.

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Click for a slideshow of this sequence Cliff Stair views
Copyright 2023 All Rights Reserved Michael Stephen Wills

Cliff Stairs I

Pam pauses for a photograph

On a day in late October 2017 Pam and Mike did a photography walk. Here is Pam pausing to pose during a descent into the gorge on the cliff staircase after visiting the overlook high above Lucifer Falls, Robert H. Treman New York State Park in the Finger Lakes Region.

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Grasses, hemlock saplings, goldenrod, spent leaves and ferns on the wall of the 223 Cliff Stair steps.

Click for a slideshow of this sequence of Lucifer Falls view from the overlook.
Copyright 2023 All Rights Reserved Michael Stephen Wills

Juniper Sunrise

crack of dawn

In this post we start the day of my posting “Family Trek, July 19, 2008, when, well before the sun rose at 6:23 am Mountain Daylight Time (the Navajo Reservation observes daylight savings, the rest of Arizona does not), Pam and I were at the Spider Rock Overlook.

Most visitors to the canyon make use of a system of roads and parking lots next to strategic views.  There is the White House Overlook we visited our first day, July 18, to hike from the trailhead into the canyon.  There are also, on the south side of the canyon:

  • Tsegi Overlook, taken from a Navajo word that translates directly to “between the rocks” and usually refers to a deep canyon with steep cliffs.
  • Junction Overlook above the point where Canyon Del Muerto (see my posting “Sun and Shade, Canyon Del Muerto”, and Canyon De Chelly intersect.  There is an Anasazi ruin in the south-facing cliff across the canyon.
  • Sliding House Overlook, another Anasazi run across the canyon.
  • Face Rock Overlook, to view the eponymous formation.
  • Spider Rock Overlook, the most stunning rock formation. 
Sunrise Canyon De Chelly
Looking east from the Spider Rock overlook, Canyon De Chelly.

While getting ready I scoped out the location for interesting visual tropes.  Utah Junipers are exceptionally hardy shrubs, stressed individual plants grow into compelling forms shaped by hardship.  As the sun rose, this specimen emerged from the gloom and caught the first sun rays.

Juniper Sunrise
A distressed Utah Juniper on the edge of Canyon De Chelly overlooking Needle Rock a few moments after sunrise.

Enjoy!!

Click for the first posting of this series, “Portrait of a Navajo Guide.”
 

The Flatiron

Where is the ironing board?

The setting sun’s glow on the end point of Upper Siphon Draw trail, The Flatiron.

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The mountain was formed by a series of volcanic eruptions between 20.5 and 18 million years ago. The west face of the mountain is composed of dacite lava and rhyolitic tuff. The overlying tuff was deposited during an eruption which created a collapse caldera bounded by faults. Dome resurgence reactivated these faults, causing uplift of the caldera floor which juxtaposed the softer tuff and more resistant dacite. Differential weathering caused the outer tuff to erode faster, leaving the dacite cliffs exposed and creating the prominent mountain visible today.

The Flatiron, the mesa-like projection above us in this view, is long solidified dacite lava. The word dacite comes from Dacia, a province of the Roman Empire which lay between the Danube River and Carpathian Mountains (now modern Romania and Moldova) where the rock was first described. Lost Dutchman State Park, Apache Junction, Maricopa County, Arizona

Reference: Wikipedia “Superstition Mountain” and “Dacite Lava.”

Copyright 2023 Michael Stephen Wills All Rights Reserved

Dragoon Ridge

Dragoon, not dragon

Dragoon Mountains of southeastern Arizona are named, not for the resemblance of this ridge to the back of a Dragon, but for a type of soldier trained for horseback riding and infantry.  These were the U.S. troops sent to “pacify” the Chiricahua Apache homeland.

Understanding location lighting is a matter of experience and luck.

Cochise Stronghold campsites are on the eastern slope of the Dragoons, sheltering them from the late afternoon sun.

One this day in April I explored the trails until sunset and was lucky enough to be setup for the 14 minutes of that day when the light was absolutely perfect.

Copyright 2023 Michael Stephen Wills All Rights Reserved

Dragoon Spires

Lucky enough

Understanding location lighting is a matter of experience and luck.

Cochise Stronghold campsites are on the eastern slope of the Dragoons, sheltering them from the late afternoon sun.

One this day in April I explored the trails until sunset and was lucky enough to be setup for the 14 minutes of that day when the light was absolutely perfect.

“Dragoon Spires in Afternoon Light”

These photographs are from two days spent at Cochise Stronghold, a part of the U.S. Forest Service Coronado Forest managed by Arizona State Parks located off the Interstate 10 East of Tucson between Benson and Wilcox.

This rugged natural fortress was, for some 15 years, the home and base of operations for the famed Chiricahua Apache Chief, Cochise.  Cochise and about 1,000 of his followers, of whom some 250 were warriors, located here.

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Born in present-day Arizona, Cochise led the Chiricahua band of the Apache tribe during a period of violent social upheaval. In 1850, the United States took control over the territory that today comprises Arizona and New Mexico.  Not hostile to the whites at first, he kept peace with the Anglo-Americans until 1861, when he became their implacable foe because of the blunder of a young U.S. Army officer, Lt. George Bascom.   In that year, Cochise and several of his relatives had gone to an encampment of soldiers in order to deny the accusation that they had abducted a child from a ranch. The boy was later proved to have been kidnapped by another band of Apaches.

During the parley, Cochise and his followers were ordered held as hostages by Bascom, but Cochise managed to escape almost immediately by cutting a hole in a tent. Bascom later ordered the other Apache hostages hanged, and the embittered Cochise joined forces with Mangas Coloradas, his father-in-law, in a guerrilla struggle against the American army and settlers. The capture and murder of Mangas Coloradas in 1863 left Cochise as the Apache war chief.   The U.S. Army captured him in 1871 and prepared to transfer the Chiricahua to a reservation hundreds of miles away, but he escaped again and renewed the resistance campaign. The following year after negotiating a new treaty with the help of Thomas Jeffords, the band was allowed  to stay in their homeland.

Cochise is reputed to have been a master strategist and leader who was never conquered in battle.  He died peacefully on the newly formed Chiricahua  reservation in 1874.  His son, Taza succeeded him as chief.   Upon his death, he was secretly buried somewhere in or near his impregnable fortress.  The exact location has never been revealed or determined.

The town of Cochise, Cochise County, the renowned geological feature known as Cochise’s Head in the Chiricahua Mountains, and the Stronghold are all named in tribute to him.

Copyright 2023 Michael Stephen Wills All Rights Reserved

Cochise Stronghold Introduction

Campground is closed in June, July, and August due to the often-extreme heat

These photographs are from two days spent at Cochise Stronghold, a part of the U.S. Forest Service Coronado Forest managed by Arizona State Parks located off the Interstate 10 East of Tucson between Benson and Wilcox.

“Idyllic Desert Landscape with Boulders”

 

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“Generations”

 

Here is the Cochise Stronghold information sign from the Douglas Ranger District of the Coronado National Forest.

The Dragoon Mountains are a low range that barely rises above the surrounding desert floor. Nevertheless, the granite boulders are spectacular and well worth visiting for the scenery alone. This mountain range is remote from cities or even any large towns, so visitation is light. Late fall, winter, and early spring are the best times to visit. Temperatures exceeding 100 degrees are common even in spring and fall. Cochise Stronghold Campground is closed in June, July, and August due to the often-extreme heat.

Safety First: Heat and low humidity are real hazards for people unfamiliar with desert climates. A person can loose up to 5 quarts of fluid a day and it is easy to become seriously dehydrated without realizing it, so drink plenty of fluids even if you do not feel very thirsty. Always carry extra water in your car. When going on a hike, even if a short one, take a day pack with water, snack foods, protective clothing, flashlight, first aid kit, compass, and map. To avoid sun in

Copyright 2023 Michael Stephen Wills All Rights Reserved