False Solomon’s Seal, scientific name Maianthemum racemosum, is common in the Finger Lakes Region. I found this specimen during a walk with the grandchildren in a local fen among the post-glacial terrain of the Finger Lakes Region.
False Solomon’s Seal is a common, widespread plant with numerous common names and synonyms, known from every US state except Hawaii, and from every Canadian province and territory (except Nunavut and the Yukon), as well as from Mexico. What name do YOU know it by?
Because it resembles plants of the highly toxic Veratrum genus, this species should not be consumed unless identification is positive. The plant becomes fibrous and bitter after it completes flowering and seed-setting, but the tender young shoots can be stripped of their leaves, simmered in water and eaten. Their delicate flavor is somewhat reminiscent of asparagus. The ripe fruits are edible raw or cooked but may be poor in taste. They can be laxative if consumed in large quantities.
Ojibwa harvested the roots of this plant and cooked them in lye water overnight to remove the bitterness and neutralize their strong laxative qualities. Native Americans boiled the roots to make tea for medicinal purposes, including to treat rheumatism, kidney issues, and wounds and back injuries.
Reference: “Maianthemum racemosum” wikipedia
Images and captions Copyright 2023 Michael Stephen Wills All Rights Reserved
Yellow Lady’s Slipper, scientific name Cypripedium parviflorum, is also known as “Moccasin Flower.” I found these on a walk with the grandchildren in a local fen among post-glacial terrain. “All this swamp cabbage, phew!!,” said the youngest.
This is a wild orchid that grows all over, though picky as to habitat.
–Newfoundland to British-Columbia, south to Georgia, Arizona, and Washington; Europe. –Newfoundland to Alaska and south to Oregon in the West. –In the East along the Atlantic Coast, it is in every state except Florida and extends across to Louisiana and eastern Texas. –New Mexico state: Catron, Colfax, Grant, Los Alamos, Otero, San Miguel, San Juan and Santa Fe Counties. –Arizona state: Apache, Graham, and Greenlee Counties.
Habitats and requirements: A more upland plant preferring subacidic to neutral soils. Primarily in mesic to dry-mesic upland forests, woodlands with deep humus or layers of leaf litter, shaded boggy habitats, but also in hill prairies and occasionally in wetlands with organic, well-drained, sandy soils. Moderate shade to nearly full sun in fir, pine, and aspen forest between 6000 and 9500 feet (1830 and 2900 meters). Mountain meadows and on timbered slopes. Dripping seeps on steep to moderately sloped canyon walls.
Reference: “Cypripedium parviflorum” wikipedia
Images and captions Copyright 2023 Michael Stephen Wills All Rights Reserved
Have you wondered, “What is ‘pileated’ about a Pileated Woodpecker? The Latin word Latin pileatus means capped, so the adjective refers to the red “cap” the bird wears. Pileated Woodpeckers mmainly eat insects, especially carpenter ants and wood-boring beetle larvae. They also eat fruits, nuts, and berries, including poison ivy berries. Pileated woodpeckers often chip out large and roughly rectangular holes in trees while searching out insects, especially ant colonies. They also lap up ants by reaching with their long tongues into crevices. They may forage around the sides of human homes or even cars and can be observed feeding at suet-type feeders, as you can see below.
Our Resident Pileated Woodpecker enjoying a suet meal one spring evening
Usually, pileated woodpeckers excavate their large nests in the cavities of dead trees. Woodpeckers make such large holes in dead trees that the holes can cause a small tree to break in half. The roost of a pileated woodpecker usually has multiple entrance holes. In April, the hole made by the male attracts a female for mating and raising their young. Once the brood is raised, the birds abandon the hole and do not use it the next year. When abandoned, these holes—made similarly by all woodpeckers—provide good homes in future years for many forest songbirds and a wide variety of other animals. Ecologically, the entire woodpecker family is important to the wellbeing of many other bird species. The pileated woodpecker also nests in boxes about 4.6 m (15 ft) off the ground. The large cavities made by pileated woodpeckers during their nesting process not only serve as a home for the birds but also play an essential role in the forest ecosystem by contributing to nutrient cycling. Woodpecker cavities can lead to increased soil nutrient levels and microbial activity, providing a nutrient-rich environment for other plants to grow.
A pileated woodpecker pair stays together on its territory all year round and is not migratory. They defend the territory in all seasons but tolerate floaters during the winter. Drumming is most common during courtship and to proclaim a territory. Hollow trees are often used to make the most resonant sound possible. The pattern is typically a fairly slow, deep rolling that lasts about three seconds.
Pileated woodpeckers have been observed to move to another site if any eggs have fallen out of the nest—a rare habit in birds. The cavity is unlined except for wood chips. Both parents incubate three to five eggs for 12 to 16 days. The average clutch size is four per nest. The young may take a month to fledge. The oldest known pileated woodpecker was 12 years and 11 months old. Predators at the nest can include American and Pacific martens, weasels, squirrels, rat snakes, and gray foxes. Free-flying adults have fewer predators but can be taken in some numbers by Cooper’s hawks, northern goshawks, red-shouldered hawks, red-tailed hawks, great horned owls, bald eagles, golden eagles and barred owls.
Reference: “Pileated Woodpecker” Wikipedia
Images and Video Copyright 2023 Michael Stephen Wills All Rights Reserved
All photography using the IPhone 14 ProMax triple camera, raw format, edited on the phone.
We find boulders of crystalline rock, commonly derived from Adirondack sources, left behind on the surface of ablation moraine, in the Finger Lakes Region.
Cornell finds some and move them, maybe the case for this unremarked erratic found along the Allen Trail of FR Newman Arboretum.
Another enormous erratic, brought in from the Sixmile Creek valley, was carved into a seat as a memorial to Professor R.S. Tarr who deciphered much of the glacial history of the Finger Lakes Region. Find it at the southwest corner of McCraw Hall on the Cornell University Campus.
History (from wikipedia)
During the 18th century, erratics were deemed a major geological paradox. Geologists identify erratics by studying the rocks surrounding the position of the erratic and the rock of the erratic itself. Erratics were once considered evidence of a biblical flood, but in the 19th century scientists gradually came to accept that erratics pointed to an ice age in Earth’s past. Among others, the Swiss politician, jurist, theologian Bernhard Friedrich Kuhn [de] saw glaciers as a possible solution as early as 1788. However, the idea of ice ages and glaciation as a geological force took a while to be accepted. Ignaz Venetz (1788–1859), a Swiss engineer, naturalist and glaciologist was one of the first scientists to recognize glaciers as a major force in shaping the earth.
In the 19th century, many scientists came to favor erratics as evidence for the end of the Last Glacial Maximum (ice age) 10,000 years ago, rather than a flood. Geologists have suggested that landslides or rockfalls initially dropped the rocks on top of glacial ice. The glaciers continued to move, carrying the rocks with them. When the ice melted, the erratics were left in their present locations.
Charles Lyell’s Principles of Geology (v. 1, 1830) provided an early description of the erratic which is consistent with the modern understanding. Louis Agassiz was the first to scientifically propose that the Earth had been subject to a past ice age. In the same year, he was elected a foreign member of the Royal Swedish Academy of Sciences. Prior to this proposal, Goethe, de Saussure, Venetz, Jean de Charpentier, Karl Friedrich Schimper and others had made the glaciers of the Alps the subjects of special study, and Goethe,[15] Charpentier as well as Schimper had even arrived at the conclusion that the erratic blocks of alpine rocks scattered over the slopes and summits of the Jura Mountains had been moved there by glaciers.
Charles Darwin published extensively on geologic phenomena including the distribution of erratic boulders. In his accounts written during the voyage of HMS Beagle, Darwin observed several large erratic boulders of notable size south of the Strait of Magellan, Tierra del Fuego and attributed them to ice rafting from Antarctica. Recent research suggests that they are more likely the result of glacial ice flows carrying the boulders to their current locations.
References:
“The Finger Lakes Region: Its Origin and Nature,” O.D. von Engeln, Cornell University Press, 1961 page 106.
Wikipedia, “Glacial Erratics”
Copyright 2023 Michael Stephen Wills All Rights Reserved
Last Friday the grandsons and I had an outing to the hills above Moravia in Cayuga County, there we visited the birthplace of Millard Fillmore. The site is a rather steep, rocky hillside near where the future President was born in a log cabin. He was not the last future President thus born, James Garfield in 1831 was born fatherless in Ohio in a log cabin. The future 20th President and the last to be so born. Nine years after Millard Fillmore, Abraham Lincoln was born, February 12, 1809 in the same residential circumstance and was the first future President born west of the Appalachian Mountains at Sinking Springs Farm, Kentucky. At least seven (7) future USA Presidents were born in log cabins, the others are: Andrew Jackson, James K. Polk, James Buchanan, Andrew Johnson, Chester A. Arthur.
There is quite a bit to do at this open air museum: educational signs, split rail fencing from that time, a pavilion build from concrete, steel I-beams and a metal roof with picnic tables where we played games.
On the way to Fillmore Glen New York State Park to visit an actual log cabin from that time, we stopped at the Lickville Cemetery on Lick Street. Opened a few years after Fillmore’s birth, 1807, 180 headstones are still standing. We practiced sounding out words from the large carved letters on the stones.
After visiting the log cabin our day was interrupted by symptoms of a stomach flu that has been terrorizing all our families. Fortunately, I escaped. Our plan is to continue to explore Fillmore Glen at a later time.
More about Millard Fillmore from Wikipedia
Millard Fillmore was born on January 7, 1800, in a log cabin, on a farm in what is now Moravia, Cayuga County, in the Finger Lakes region of New York. His parents were Phoebe Millard and Nathaniel Fillmore, and he was the second of eight children and the oldest son.
Nathaniel Fillmore was the son of Nathaniel Fillmore Sr. (1739–1814), a native of Franklin, Connecticut, who became one of the earliest settlers of Bennington, Vermont, when it was founded in the territory that was then called the New Hampshire Grants.
Nathaniel Fillmore and Phoebe Millard moved from Vermont in 1799 and sought better opportunities than were available on Nathaniel’s stony farm, but the title to their Cayuga County land proved defective, and the Fillmore family moved to nearby Sempronius, where they leased land as tenant farmers, and Nathaniel occasionally taught school. The historian Tyler Anbinder described Fillmore’s childhood as “one of hard work, frequent privation, and virtually no formal schooling.”
Over time Nathaniel became more successful in Sempronius, but during Millard’s formative years, the family endured severe poverty. Nathaniel became sufficiently regarded that he was chosen to serve in local offices, including justice of the peace. Hoping that his oldest son would learn a trade, he convinced Millard, who was 14, not to enlist for the War of 1812 and apprenticed him to clothmaker Benjamin Hungerford in Sparta. Fillmore was relegated to menial labor, and unhappy at not learning any skills, he left Hungerford’s employ.
His father then placed him in the same trade at a mill in New Hope. Seeking to better himself, Millard bought a share in a circulating library and read all the books that he could. In 1819 he took advantage of idle time at the mill to enroll at a new academy in the town, where he met a classmate, Abigail Powers, and fell in love with her.
Later in 1819 Nathaniel moved the family to Montville, a hamlet of Moravia. Appreciating his son’s talents, Nathaniel followed his wife’s advice and persuaded Judge Walter Wood, the Fillmores’ landlord and the wealthiest person in the area, to allow Millard to be his law clerk for a trial period. Wood agreed to employ young Fillmore and to supervise him as he read law. Fillmore earned money teaching school for three months and bought out his mill apprenticeship. He left Wood after eighteen months; the judge had paid him almost nothing, and both quarreled after Fillmore had, unaided, earned a small sum by advising a farmer in a minor lawsuit. Refusing to pledge not to do so again, Fillmore gave up his clerkship. Nathaniel again moved the family, and Millard accompanied it west to East Aurora, in Erie County, near Buffalo, where Nathaniel purchased a farm that became prosperous.
Copyright 2023 Michael Stephen Wills All Rights Reserved.
Thank You for exploring with me the South Rim trail of Taughannock Falls State Park on this first day of Spring 2023.
Photographs with video from this walk, with nature sounds and music in 4K HD
Click photograph for a larger view. To do this from WordPress Reader, you need to first click the title of this post to open a new page.
Here, before the epynmous creek flows over the falls, glacial outflow carved this deep canyon through relatively soft sedimentary rock. Distant Lake ViewThe place for rest and wonderLooking into the gorgeSouth Rim view of fallsTaughannock creek below the fallsRed Barn on Gorge Road, off South Rim rial.Perched on the north rim of the gorge, the Visitor Center for the Falls Overlook is visible before trees leaf out.On spring’s first day Taughannock Creek is full beneath the old railroad bridge, now a connector between South and North Rim Trails.The creek here plunges into the chasm below a former railroad bridge. Gorge from Railroad Bridge Walkway
Our Winter Aconite started blooming around Valentines Day, February 14, 2023.
The following photograph is from the Apple IPhone 14 ProMax, raw format and perfected on the phone. The rest are from the Canon 5D Mark IV with the lens EF 100mm f/2.8 Macro USB.
As a spring ehemeral plant, its life cycle exploits the deciduous woodland canopy, flowering at the time of maximum sunlight reaching the forest floor, then completely dying back to its underground tuber after flowering.
All parts of the plant are poisonous when consumed by humans and other mammals because it contains cardiac glycosides.
The species name Eranthis hyemalis proclaims the early nature of its flowering both in the genus, “Eranthis” – “spring flower”, and species, “hyemalis” – winter flowering. The genus encompasses eight species, all early flowering winter aconite.
Reference: Wikipedia “Eranthis hyemalis” and “Eranthis.”
Copyright 2023 All Rights Reserved Michael Stephen Wills
Michael Stephen Wills Photography 
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