Pam and I ambled around the Arboretum for our Easter 2023 outing. We discovered this seeming lily growing from the muck along the Treman Woodland Walk. Scientific Name: Lysichiton camtschatcensis. Common names: Asian skunk cabbage, white skunk cabbage, Far Eastern swamp lantern or Japanese swamp lantern.
This is a plant found in swamps and wet woods, along streams and in other wet areas of the Kamchatka Peninsula, the Kuril Islands, Sakhalin and northern Japan. The common name “skunk cabbage” is used for the genus Lysichiton, which includes Lysichiton americanus, the western skunk cabbage, noted for its unpleasant smell. The Asian skunk cabbage is more variable: plants have been reported in different cases to smell disgusting, not at all, and sweet.
All photography using the IPhone 14 ProMax triple camera, raw format, edited on the phone.
In Japanese it is known as mizubashō (lit. “water-banana”) from a supposed similarity to the Japanese banana, a name with poetic rather than malodorous associations. It is not closely related to the true cabbage.
Copyright 2023 Michael Stephen Wills All Rights Reserved
Pam and I ambled around the Arboretum for our Easter 2023 outing. Found here growing outside native range, being the Appalachian Mountains from Georgia to southern Pennsylvania, the Table Mountain Pine is named after the landform, not a particular mountain.
All photography using the IPhone 14 ProMax triple camera, raw format, edited on the phone.
Its pinecones drew me to this scraggly, ungainly, poorly formed tree. All general mankind finds useful in the, scientific name, Pinus pungens, otherwise known as Hickory Pine, Prickly Pine and Mountain Pine, is to grind it up for pulp or chop it for tinder.
Last of the Mohicans
That said, the final scene of the 1992 film The Last of the Mohicans takes place in a nice Pinus pungens stand on a rocky mountaintop in North Carolina.
Personality
The tree has personality. Pinus pungens is the Lonesome Pine of the 1908 novel The Trail of the Lonesome Pine by John Fox, and popularized in the Laurel and Hardy film Way out West: “On the Blue Ridge Mountains of Virginia On the Trail of the Lonesome Pine” Several “Lonesome Pine” hiking trails have been waymarked in the Blue Ridge Mountains and elsewhere in the Appalachians.
Pinecone Bud
Pinus pungens prefers dry conditions and is mostly found on rocky slopes, favoring higher elevations, from 300–1,760 meters (980–5,770 ft) altitude. It commonly grows as single scattered trees or small groves, not in large forests like most other pines, and needs periodic disturbances for seedling establishment. The three tallest known ones are in Paris Mountain State Park, South Carolina; they are 26.85 to 29.96 meters (88 ft 1 in to 98 ft 4 in) tall.
Reference: “Pinus pungens” Wikipedia.
Copyright 2023 Michael Stephen Wills All Rights Reserved
Pam and I ambled around the Arboretum for our Easter 2023 outing. A type of sandstone popular with Cornell monument builders, called “Lenroc” after a mansion build by Cornell’s founder, was used for these benches built into the hillside of the FR Newman Arboretum. The views are more interesting than the bench, the arch of stone in midground in one photo.
All photography using the IPhone 14 ProMax triple camera, raw format, edited on the phone.
The stone is mined locally from surrounding hills. Calling it “Lenroc” (Cornell spelled backward) is a misnomer as the stone is mined widely throughout the region.
Feldspathic Greywacke
“Bluestone from Pennsylvania and New York is a sandstone defined as feldspathic greywacke. The sand-sized grains from which bluestone is constituted were deposited in the Catskill Delta during the Middle to Upper Devonian Period of the Paleozoic Era, approximately 370 to 345 million years ago…..
Glacial Landscape on an early spring day, Easter 2023
Textures
…The Catskill Delta was created from runoff from the Acadian Mountains (“Ancestral Appalachians”). This delta ran in a narrow band from southwest to northeast and today provides the bluestone quarried from the Catskill Mountains and Northeastern Pennsylvania. The term “bluestone” is derived from a deep-blue-colored sandstone first found in Ulster County, New York.”
You can feel the origin of this bluestone from these macros of two pavers from a monument bench.
Reference: “Bluestone” Wikipedia.
Copyright 2023 Michael Stephen Wills All Rights Reserved
Some nights I travel to the farthest reaches of the universe right from my backyard. Here is a guide to the spring night sky for those of you in the northern hemisphere. Even sunbathing we are time travelling, bathed in starlite over 8 minutes old. Time taken by sunlight to reach Earth = (150,000,000/3,00,000) seconds = 500 seconds = 8 minutes 20 seconds).
Another Cayuga Waterfront Trail stop is this memorial. The plaque reads ” ‘Grandpa’ (Ironwood) Trees in memory of John A. ‘Jack’ Dougherty; June 15, 1927 – March 12, 1995; City of Ithaca 1949-1989, Retired as Superintendent of Public Works.” Located near the intersection of Pier Road and Willow Avenue, Newman Golf Course, Ithaca, Tompkins County, New York. That is an Ironwood tree, midgound center.
The American Hornbeam (scientific name: Carpinus caroliniana) is also known as Musclewood for the rippled surface of the mature trunk. Other names are blue-beech, ironwood and muscle beech.
Nestled on the trunk……
Copyright 2023 Michael Stephen Wills All Rights Reserved
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.
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.
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 BridgeSONY DSC
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.
“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.
Resting place of double great Grandparents George and Mary WillsWooden Plaque on left sdie of entry pavilion. Sign to left of pavilionGeorge Wills, Hotel Keeper, around 1850Father, George Wills, Sr., Born August 2, 1809, Died July 21, 1884 Aged 76 years., May his soul rest in peace, AmenMary Dellett Wills, as widow after 1894Mother Mary wife of George Wills, Born August 28, 1809, Died February 18, 1895 Aged 85 years. May her soul rest in peace, Amen
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.
Twenty million years ago a then nonexistent earth-bound human civilization could recognize none of the prominent stars of the constellation Scorpius (The Scorpion) as these, compared to our 4.6 billion year old star, lit up less than 12 million years ago. The brightest star, Alpha Scorpii AKA Antares, is a red giant destined to burst into a supernova bright as the full moon within two million years. Will the human race be around to witness it?
Such as it is, The Scorpion was traced out by the Babylonian astronomers around 8 BCE following even more ancient Sumerian traditions naming Alpha Scorpii “The Heart of the Scorpion.”
I first became aware of Antares March 2009 during a stay on Cocoa Beach. Setting the room clock to a 5 am alarm to view the sunrise. As I sat listening to the surf, Antares glowed dark red in the south. It is the reddish tint star in the following illustration.
Here is a photograph of Antares, the reddish dot in center, along with the 6 of the 18 Scorpius bright stars. For this shot a Canon EOS 5D Mark IV dlsr had mounted a Canon lens EF 70-300 f4-5.6L IS USM set to 70 mm focal length, 1600 ISO. Exposure was “bulb,” meaning when the shutter button is pressed and held the shutter remains open: for this exposure this was for approximately 10 seconds. The equipment was held steady on a Manfrotto BeFree Carbon Fiber tripod. As the Earth continued to turn, the resulting star images are smeared a bit.
Bracketing Antares, the Scorpion Heart are “The Arteries” Theta and Tau. About those Greek letters, these designate relative brightness of each star respective of the others in the constellation. “Alpha” the first letter of the Greek alphabet is the brightest. Here are the other letters listed, with the alphabetic order in brackets Beta(2), Delta(4), Pi(16), Sigma(18), Tau(19). Ancient Greek built on the traditions of the Mesopotamians (Babylonian and Sumerian) and were in turn used for modern stellar nomenclature, including the tracings of sky images, the constellations.
The position of a relatively minor star, Tau, near Antares elevates it to the important function of an artery. The stars themselves run against their brightness hierarchy placement: The star Delta Scorpii, after having been a stable 2.3 magnitude star, flared in July 2000 to 1.9 in a matter of weeks. It has since become a variable star fluctuating between 2.0 and 1.6. This means that at its brightest it is the second brightest star in Scorpius.
Copyright 2023 Michael Stephen Wills All Rights Reserved
Fall Creek meanders through the esker fields of the Malloryville Preserve. Here is the view from an abandoned railroad bridge. A major watercourse of the Finger Lakes, throughout the 19th century Fall Creek provided water power for local industry: grain grinding mills, cooperage and furniture. Here the stream bed is wide, flow slow and pacific for a mirrored surface, the effect broken by a single drop from an overhanging tree or, maybe, a fin’s flash.
Pam and I visited Malloryville last weekend to enjoy a “socially distanced” walk with family.
Michael Stephen Wills Photography 