The Ancient Doors to Mesa Verde

Two Ancient Cliff Swellings

The Anasazi (“ancient ones”) constructed 15 rooms on a 10 foot deep cliff alcove and used a toe-trail (literally a series of depressions in the rock used to gain traction) to climb to the mesa top (shown in this photograph) and the canyon.

A toe-trail security feature is the necessity to start using the correct hand/foot combination, otherwise there will be a point from which it is impossible to proceed. There are 15 rooms here: a kiva, on the far left, a multi-story building, on the right, with 4 upper rooms and 10 ground floor spaces. They probably blocked the openings in cold weather to conserve heat.

Click me for more Mesa Verde works in my Fine Art Gallery

The Anasazi had gardens on the mesa top or the canyon, plus they hunted and gathered wild foods. In the gardens, they planted corn, bean, squash and watermelon in the rich soil. They also gathered wild plants and herbs such as bee-weed, ground cherry, milkweed, cattail, wolf berry and sedge grass Cliff dwelling alcoves include a seep spring, a seam in the rock through which a small amount of water flowed. Imagine the difficulty of hauling water every day if there was not a water source in the alcove.

Can you find the unnamed ruin also in this canyon, we call it “Cliff Canyon”? These ruins are outside the national park boundary, inside the Ute Mountain Ute Indian Reservation.

House of Many Windows

The “window” of this cliff dwelling (ruin) was actually a door!! The Anasazi (“ancient ones”) constructed two rooms in this narrow cliff alcove.

The two rooms here are what seems to be a round wall, possibly a kiva ruin, on the left and a single story building, on the right, being the single wall with an opening for access. They probably blocked the opening in cold weather to conserve heat. It is possible this site had a special use and was occupied for a limited period of time each season/year.

Cliff dwelling alcoves include a seep spring, a seam in the rock through which a small amount of water flowed. Imagine the difficulty of hauling water every day if there was not a water source in the alcove. The large juniper to the left attests to a water source, since it grows from a shared crevice.

The protective alcove was deeper in the past. The desert varnish (the dark marking) above the alcove marks a place where water seeps from the cliff and, in cold weather, expands under the overlying rock, causing it to fall. Can you see where the cliff face has fallen above the ruin? The lack of desert varnish shows the rock fall was relatively recent.

Copyright 2023 Michael Stephen Wills All Rights Reserved

Point Lookout at Dawn, Mesa Verde

Dramatic Entrance

This dramatic butte at the entrance to Mesa Verde National Park, golden in the first light of a July morning.  My wife, Pam, and I were on this road in the pre-dawn hours.  Our delight with this surprise view was worth it.

Click me for more Mesa Verde works in my Fine Art Gallery

In this Point Lookout area, near the park’s entrance, the Mancos Shale is about 2,000 ft thick, and this is what this butte is composed of. Mancos Shale is the lowest formation of the park and is a thick sequence of gray to black marine shale containing minor tan siltstone and fine sandstone beds. On steep slopes, such as those near the northern and eastern boundaries of the park, this formation is prone to landslides and debris flows. This is the base of the butte. The lovely golden rock is Point Lookout Sandstone of the Mesaverde Group, a predominantly yellowish-gray or pale-orange, fine- to medium-grained marine sandstone, approximately 300-400 ft thick. The Point Lookout Sandstone forms much of the cap rock in the northern park area.

I reworked the above image into this Fine Art image of Point Lookout.

Reference: http://esp.cr.usgs.gov/info/meve/

Copyright 2023 Michael Stephen Wills All Rights Reserved

Sipapu Bridge Up Close

This post continues my story of Sipapu Bridge.

I created a series of fine art prints from a visit my wife Pam and I made to Natural Bridges National Monument in Utah.  Here are a few of these prints which grace fine homes around the world.  Click any of the photographs to visit the gallery.

We walked a narrow cliff patch climbed a series of weathered pine ladders  to  achieve these views of Sipapu Bridges National Monument.

While the sky is unchanged, below the canyon rim is another world.  The black stripes of the cliffs is desert varnish, a thin deposit of clay, iron and manganese oxides.  The rock supporting the varnish is resistant to wear and protected from direct precipitation (in this case by the overhanging cliff).

Eventually we came to a ledge with a view of Sipapu Bridge.  Pam took the opportunity to capture this amazing experience.

Mike at Sipapu Bridge
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A Utah Juniper (Juniperus osteosperma). Historically, across the west, Native Americans used the wood in building their houses. They ate the berries; smoked the bark; made shoes, clothing, and rope from it.

Sipapu is a Hopi word for the small hole or indentation in the floor of kivas used by the Ancient Pueblo Peoples and modern-day Puebloans. It symbolizes the portal through which their ancient ancestors first emerged to enter the present world. A natural bridge is formed through erosion by water flowing in the stream bed of the canyon. Sipapu Bridge is 268 feet across and, standing in the stream bed, it is 220 feet above your head.

Here is a close up of the white Permian sandstone of the bridge arch.  The entire canyon is carved from this stone and named after it.

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World Portal

Sipapu is one of the largest natural bridges known.

Part of the Natural Bridges National Monument in Utah, a place inaccessible until the “uranium boom” of the 1950’s and the road was only paved in 1976.

We visited on a July day of thunderstorms, which you see building here.  If you look closely at the base of the bridge, you can see the railings my wife and I used to climbed the steep sides of White Canyon.

We hiked a few miles along an unmaintained trail.  On the way we passed ancient cliff dwellings. The area is a maze of canyons throughout which these ruins are scattered.

Sipapu is a Hopi word for the small hole or indentation in the floor of kivas used by the Ancient Pueblo Peoples and modern-day Puebloans. It symbolizes the portal through which their ancient ancestors first emerged to enter the present world.

A natural bridge is formed through erosion by water flowing in the stream bed of the canyon.

Sipapu Bridge is 268 feet across and, standing in the stream bed, it is 220 feet above your head. That is white Permian sandstone, after which White Canyon is named.

Copyright 2023 Michael Stephen Wills All Rights Reserved

Anasazi Cliff House I

This group of buildings was crafted into a cliff face over 1,000 years ago.

Visitors must climb over the cliff and through narrow tunnels, security features created by the builders.

High Security and Adventure

Security barriers include a 32 foot, entrance ladder made from pine trunks and a narrow squeeze through a 12 foot tunnel.

My photograph of Balcony House features ruins to rooms on a plaza. Also shown are edges of two kivas (circular ceremonial chambers) built into the plaza floor. I am standing in a plaza, next to the cliff.

Behind me (not visible) is the narrow security tunnel used by the ancient builds to control access. Today, visitors crawl through the narrow tunnel to exit the site. There are 40 rooms in Balcony House.

Copyright 2023 Michael Stephen Wills All Rights Reserved

Pinelands Connections I

Geneology and DNA

“From the fire tower on Bear Swamp Hill, in Washington Township, Burlington County, New Jersey, the view usually extends about twelve miles. To the north, forest land reaches to the horizon. The trees are mainly oaks and pines, and the pine predominate. Occasionally, there are long, dark, serrated stands of Atlantic white cedars, so tall and so closely set that they seem spread against the sky on the ridges of hills, when in fact they grow along streams that flow through the forest. To the east, the view is similar, and few people who are not native to the region can discern essential differences from the high cabin of the fire tower, even though one difference is that huge areas out in this direction are covered with dwarf forests, where a man can stand among the trees and see for miles over their uppermost branches. To the south, the view is twice broken slightly — by a lake and by a cranberry bog — both otherwise it, too, goes to the horizon in forest. To the west, pines, oaks, and cedars continue all the way, and the western horizon includes the summit of another hill — Apple Pie Hill — and the outline of another fire tower, from which the view three hundred and sixty degrees around is virtually the same as the view from Bear Swamp Hill, where, in a moment’s sweeping glance, a person can see hundreds of square miles of wilderness. The picture of New Jersey that most people hold in their minds is so different from this one that, considered beside it, the Pine Barrens, as they are called, become as incongruous as they are beautiful.” From The New Yorker magazine, November 26, 1967, “Profiles, The Pine Barrens I” creative non-fiction by the great John McPhee.

This quote captures the contours of a place, now known as “The Pinelands,” a corner of Burlington County, New Jersey my English, Irish, Scottish ancestors settled from 1677 until my grandfather, James Edward Wills, left for northern New Jersey, Asbury Park, in the first years of the twentieth century. This past decade, more so since retirement 2017, I’ve explored these two hundred and twenty (220) or so years beginning with amorphous asides over the years from my father and second hand through my sisters then through online research via Ancestry.com (Ancestry) and other searches.

From my father and sisters I knew to search southern New Jersey. The United States decennial census, “thank you Constitution,” listed a George and Margaret Wills with my grandfather among their children. Great Grandfather George Wills was listed as a 14 year old child of George and Mary Wills in the 1850 census. How could I be sure? DNA technology with internet based social interaction helped there. I was contacted by a Dellett descendant, identified by DNA as a fourth cousin, who claimed Mary Wills as a double great aunt, the daughter of James and Ann Dellett. Here is a screen capture of an Ancestry “ThruLines” analysis showing the six living ancestors of James and Ann in the database. I removed the names and photos of the other five to preserve privacy. The DNA fourth cousin relationship was an exact match to the family tree.

Cousin Delette provided antique photographs of George and Mary. I did a “FindAGrave” search, their final resting place is in a place named Tabernacle, Burlington County, New Jersey. September 2019 my wife Pam and I did a weekend tour with a bed and breakfast base in the city of Burlington, New Jersey. The rest of the photos in the following slideshow are from that weekend.

Here is the same Ancestry “ThruLines” analysis with the immediate family links exploded. through my “first cousin 1 time removed” I was able to communicate with a “lost” niece of my father who shared reminiscences of him from the time he was just released from World War II Naval Service, before meeting Mom.

….Click me for Pineland Connections II.

Copyright 2023 Michael Stephen Wills All Rights Reserved

Valentines Day Greetings

1959 through today

Theresa (2), Michael (5), Christine (4) in the livingroom of 107 Deepdale Parkway, Albertson, New York on Valentines Day 1959

Chocolate Valentines Day cake by Pamela Wills

Pam and I aboard the Oceania Regatta sailing the Pacific Ocean off Chile. The following day we reached Puerto Montt.
Copyright 2025 Michael Stephen Wills All Rights Reserved

Oak Creek Reflections

early one still morning

The fault of Oak Creek changes direction, here it turns east/west through Schnebly Hill Formation red sandstone for which Sedona is famous.

West Fork (108) Trail, Sedona, Yavapai County, Arizona

“Hello” from Oak Creek Canyon, “Photo by Pam Wills”

Click this link for my Fine Art Photography gallery. You can find Oak Creek Mandala in the Arizona gallery.  The gallery description gives more information about the site.

Click this link for another Arizona post, “Cochise Dawn.”

Sandstone Gallery

early one still morning

The fault of Oak Creek changes direction, here it forms a north/south gallery through Schnebly Hill Formation red sandstone for which Sedona is famous.

West Fork (108) Trail, Sedona, Yavapai County, Arizona

“Hello” from Oak Creek Canyon, “Photo by Pam Wills”

Click this link for my Fine Art Photography gallery. You can find Oak Creek Mandala in the Arizona gallery.  The gallery description gives more information about the site.

Click this link for another Arizona post, “Cochise Dawn.”

Frozen Fall Creek III

Across the years into a future

Gratitude for miracles witnessed is my emotion for this series, “Frozen Fall Creek.” Fifteen winters after Pam and I walked Fall Creek as a solid walking path, the stream flows without ice most years. My son, whose family now lives in the house, and his wife recalling walking the creek a few years ago, not in the past few years.

Weather records support our recollections and observations: here is an analysis of Ithaca January temperatures. The years 2009 through 2019 show a warming trend in daily temperatures for both minimum and maximum.

Analysis

Excel I used to plot minimum and maximum temperatures (Fahrenheit) for the 31 days of each January for eleven years 2009 – 2019. Click on the images of this post for a larger version.

Click any image for a larger view.

Forecast

Pam and I moved to Ithaca 2011 and missed our Fall Creek winter walks, miss them even more now our weekend excursions are only memories. Here are January minimum/maximum average daily temperature projections from 2020 through 2044 based on the trend established from the 2009 through 2019 series. The trend is the solid color, projection the faded color.

Reading from the chart, if the current trend continues by January 2044 the average maximum daily temperature will be 47 degrees compared to 29 for 2009. In other words, the temperature never rose above freezing in the year 2009. By 2044 temperatures will be above freezing every day, on average, with daily minimums averaging 21 degrees.

From what I read, we can expect these warming trends to accerate within our lifetimes. My son named small mid-creek hummocks “islands” with numbers. Here is a view of his Second Island in late summer. What will Second Island be in 2044 late summer?

Late Summer 2018, second island

Memories

Reader of posts I and II of this series have commented about snow shadows. Here are the shadows produced from snow fallen on the vegetation of the last photograph: soft mounds to contrast with tree trunk shadows.

Winter 2009, second island

I prefer the composition of the following photograph. What do you think?

Play of winter shadows

A combination of contrasting shadow forms.

Low Winter Sun
Copyright 2023 All Rights Reserved Michael Stephen Wills