Lucifer Falls on an Autumn Evening

The post explores the symbolism of Lucifer and the Tiger Lily, suggesting that beauty and pride can lead to downfall, reminiscent of Lucifer’s narrative.

A reader’s comment to this blog, thank you “Urban Liaisons,” prompted me to explore the word, Lucifer. “Lucifer”, in Christian tradition, refers to the devil as it was in a time of glory before the fall from grace. The original, ancient meaning of Lucifer is the planet Venus as it rises just before the sun at dawn.  In this sense, the name refers to the bright beauty of the spot.  The effect is heightened at midday when the hiker passes from the relative gloom of Devils Kitchen to the full light and sweep of the waterfall chasm.

Standing next to the falls on the Gorge Trail, the stone wall of the Rim Trail Overlook is overpowered by the grandeur of the 300+ foot cliff. The falls photographs were taken from behind the wall.

Occasionally, we have experienced individuals climbing over the wall to stand on the other side. “Why?”

Summertime thick stands of tiger lilies flourish on the cliff face. Can you find the withered leaves?

I must delve into symbolic interpretations to explore the connection between Lucifer and the Tiger Lily. Lucifer, traditionally associated with rebellion and the fallen angel in Christian theology, symbolizes a break from divine order and beauty tainted by pride. On the other hand, the Tiger Lily is often seen as a symbol of wealth, pride, and prosperity in various cultures. The connection lies in the shared symbolism of pride and beauty. Just as Lucifer was a beautiful angel before his fall, the Tiger Lily is a strikingly beautiful flower, often associated with pride. This juxtaposition creates a metaphorical link, suggesting that beauty and pride, while alluring, can lead to downfall, mirroring Lucifer’s story.

This session I finally “cracked” the puzzle of the Devil’s Kitchen Waterfall. I posted the results to the online gallery yesterday, for your enjoyment. Click the link to go there.

Click link for my fine art print “Devils Kitchen.”

Click Me to view my photographs on Getty.

Copyright 2023 Michael Stephen Wills All Rights Reserved http://www.MichaelStephenWills.com

Shuffle off

All Souls’ Day, observed on November 2, is a Christian tradition of praying for the deceased, originating from ancient practices and shaping cultural rituals like Mexico’s Día de los Muertos.

Shuffling through the hot coals of autumn on All Souls Day.

Click image for a larger version.

All Souls’ Day, observed on November 2nd, is a day of prayer and remembrance for the souls of the deceased. Stemming from ancient traditions and solidified within the Christian liturgical calendar, this day serves as a solemn occasion to commemorate the departed. Its roots are deep, with a rich history that intertwines with both religious and cultural practices over centuries.

Origins
The concept of dedicating a day to remember the dead predates Christianity. Many ancient civilizations, such as the Egyptians and the Celts, held ceremonies and festivals to honor the deceased. The Celts, for instance, celebrated Samhain, which marked the end of harvest and the beginning of winter. This was believed to be a time when the veil between the living and the dead was thinnest.

As Christianity spread across Europe, there was an attempt to integrate pagan practices into the Christian framework, leading to the establishment of days dedicated to the deceased. By the 7th century, monastic communities in Europe had begun to designate a day to pray for the departed members of their communities.

Establishment
All Souls’ Day was formally institutionalized by St. Odilo of Cluny in 998 AD. He declared November 2nd as a day for all the monasteries associated with his Benedictine congregation to pray for the souls in purgatory. This practice quickly spread, and by the 11th century, it was widely celebrated throughout Christian Europe.

Theology Behind the Celebration
Central to All Souls’ Day is the belief in Purgatory – an interim state where souls undergo purification before entering Heaven. It’s believed that the prayers of the living can aid these souls, expediting their journey to paradise.

Modern Observations
Today, All Souls’ Day is observed with varying levels of prominence across Christian denominations. In Roman Catholicism, it retains significant importance, with masses dedicated to the departed. In other Christian traditions, it may merge with other observances, like All Saints’ Day (November 1st) or be passed over entirely.

Cultural Influences
Over time, All Souls’ Day has influenced and been influenced by local customs and traditions. In Mexico, for instance, Día de los Muertos (Day of the Dead) coincides with All Souls’ Day but has its distinct flair, involving vibrant parades, elaborate altars, and specific foods.

Bullet Points Summary:

Ancient Foundations: All Souls’ Day has its roots in ancient civilizations that honored the dead.
Samhain: The Celts observed Samhain, marking a time of close proximity between the living and the dead.
Christian Integration: Early Christians attempted to integrate existing pagan rituals into their religious framework.
Monastic Observances: By the 7th century, monastic communities began designating days for the departed.
St. Odilo of Cluny: He formalized All Souls’ Day in 998 AD for his Benedictine congregation.
Spread: By the 11th century, the observance had spread throughout Christian Europe.
Purgatory: Central to the day’s theology is the belief in purgatory and the power of prayers to aid souls.
Variation in Observance: The day’s significance varies across Christian denominations.
Cultural Mergers: Local traditions, like Mexico’s Día de los Muertos, have both influenced and been influenced by All Souls’ Day.
Modern Practices: Today, the day may involve attending masses, lighting candles, and visiting graves of loved ones.
In essence, All Souls’ Day is not just a day on the liturgical calendar; it’s a reflection of humanity’s timeless effort to understand, honor, and find meaning in the cyclical nature of life and death. Through rituals and observances, we bridge the gap between the past, present, and the profound mystery of the hereafter.

Click Me for another Malloryville post, “Formed By Water.”

Copyright 2023 Michael Stephen Wills All Rights Reserved

Dappled Sunlight

The Malloryville eskers near Freeville, New York, highlight the region’s glacial history and contribute significantly to biodiversity and local ecology.

Walking here, I enjoy telling the grandchildren of the immense, mile-high ice sheet that once covered this land 10,000 years ago, creating these hills and hollows.

Click Me for another Malloryville post, “Formed By Water.”

Eskers are geological features that tell a rich tale of the glacial history of an area. In the landscape near Freeville, New York, the eskers of Malloryville stand as prominent reminders of the last Ice Age and the profound effects glaciers have had on the North American terrain. These elongated ridges, composed primarily of sand and gravel, not only offer a visual spectacle but also provide crucial insights into the glacial processes that shaped the region.

Eskers are formed by the deposition of sediment from meltwater rivers flowing on the surface of or within glaciers. As these glaciers recede, the sediment accumulates in the paths previously carved by the meltwater streams, eventually forming ridges. The Malloryville eskers are particularly notable for their well-preserved structure, giving geologists and enthusiasts alike a clear vision of the patterns of glacial meltwater flow from thousands of years ago.

Located just a few miles from Freeville, the Malloryville eskers are an intriguing natural attraction. The topography of the area, largely shaped by the Laurentide Ice Sheet during the last glacial maximum, is characterized by various glacial features, but the eskers are undeniably some of the most distinct. Their serpentine-like appearance, weaving through the landscape, immediately captures one’s attention and beckons further exploration.

From an ecological perspective, the eskers of Malloryville contribute to the area’s biodiversity. The unique microenvironments created by these ridges offer habitats that differ from the surrounding landscape. This differentiation allows for a variety of plant species to thrive, some of which are specially adapted to the well-drained soils of the eskers. Additionally, these ridges act as corridors for wildlife, facilitating movement and offering vantage points for species like deer and birds of prey.

Historically, the eskers near Freeville have also had an impact on human activity. Native American communities, recognizing the strategic advantage of these high grounds, are known to have used them as pathways or even settlement sites. In more recent history, the gravel and sand composition of the eskers have made them targets for mining activities. While this has led to the alteration or destruction of some sections, it has also highlighted the importance of preserving these unique geological features for future generations.

Efforts to study and preserve the Malloryville eskers have grown in recent years. Local educational institutions, in collaboration with geological societies, have undertaken detailed studies to understand the formation and significance of these features better. Such initiatives not only contribute to the scientific understanding of glacial processes but also raise awareness about the importance of conserving unique geological formations. Given the potential impacts of climate change on glacial landscapes worldwide, the eskers serve as a poignant reminder of the dynamic nature of our planet and the traces left behind by the ebb and flow of ice ages.

In conclusion, the eskers of Malloryville near Freeville, New York, stand as testaments to the glacial history of the region. These winding ridges, with their intricate patterns and rich ecological contributions, weave a story of natural processes that have spanned millennia. They remind us of the ever-changing nature of our planet and underscore the importance of understanding and preserving its geological wonders. Whether one views them with the eyes of a scientist, historian, or nature enthusiast, the Malloryville eskers offer a captivating glimpse into the ancient forces that have shaped the world around us.

Copyright 2020 Michael Stephen Wills All Rights Reserved

Coming and Going

beneath the bridge

Standing on a stream spanning bridge it is fun to drop a stick or leaf, watch the progress, disappearing beneath the bridge to emerge and continue riding the water downstream.

Click image for a larger version.

Click Me for another Malloryville post, “Formed By Water.”

Copyright 2023 Michael Stephen Wills All Rights Reserved

Treman Early Autumn Walk IX

The post discusses various unique kennings, their meanings, and reflects on the term “Swan-Road” symbolizing a serene river.

Below Lucifer Falls this quiet water flows beneath a bridge linking Gorge and Rim trails. The reflection of blue sky between river trees brings to mind the kenning “Swan-Road.” To me it is more fitting than the established meaning: “The Sea,” also associated more appropriately with Whale-Road.

Swan Road

The seldom used English verb “ken.” The Oxford English dictionary proposed the word was borrowed from Norse based on a confluence of meaning, i.e. to know. When it is turned into a noun with the -ing ending, it is a phrase that brings to mind and object described.

Other kennings from : “Whale road = sea (e.g., a place where whales travel); Treasure seat = throne (e.g., the source of treasure or reward, or the role of the king in rewarding his men); Ring giver, ring breaker = king (e.g., the person who bestows rings, or breaks off a piece of his golden bracelet as a reward); Sword sleep = death (e.g., a “sleep” caused by a sword wound); Rapture of heaven = sun (e.g., the sun, brightest of heavenly objects, the joy of heaven); Weaver of peace = wife (e.g., a person whose grace and mildness instills peace, or one who creates domestic tranquility); Earl’s defense = Beowulf (e.g., the one who defends Hrothgar); Mead seats = benches in Heorot (e.g., the places where people sit and drink).”

Click Me for a master work of English poetry that employs kenning forms, “The Porcupine” by Galway Kinnell.

References:

–text in italics and quotes is from the eNotes.com, “Beowulf.”

–Kinnell, Galway. “The Porcupine.” The Hudson Review 20, no. 2 (1967): 219–22.

Copyright 2023 All Rights Reserved Michael Stephen Wills

Treman Early Autumn Walk VIII

Park staff evaluate and dislodge dangerous rocks on trails before springtime opening.

Overhangs such as this worry me, always forcing a faster pace. Over the years during early springtime walks, sometime before the gorge trail is opened officially, the path is littered with huge blocks fallen during the winter, possibly even that same day.

A task the park staff undertakes before opening is an evaluation of sequences such as this, with cliffs and overhangs, for portions ready to fall. Rock climbers are engaged to dislodge these rocks. At times, larger segments of the cliff are blasted resulting in landslides.

On a gentler note, these asters grace Finger Lakes trails this time of year.

Click Me for another Fall Aster post.

Copyright 2023 All Rights Reserved Michael Stephen Wills

Treman Early Autumn Walk VII

Unnamed though memorable

An unnamed waterfall along the Gorge Trail is memorable for the steps alongside.

I have captured it in all seasons from the beginning of my photography interest. Here it is at midday, early autumn, 2023, taken with the Apple Iphone 14 proMax. Bright sunlight ruins the shot.

Here, evening, early summer 2003, the foreground shaded, late day sunlight on trees beyond. The Sony dsc F828 camera, on a tripod, was used.

Here, bright sunlight at midday is handled by framing the brightly lit waterfall, April, 2002. A handheld Sony Mavica was used.

Daring visitors jump from the wall at right into a plunge pool, seen here as the quiet water at base of wall. It is a doubly dangerous activity as the force of water can hold a swimmer under indefinitely, missing the narrow pool results in striking the rocks. Robert H. Treman New York State Park, Tompkins County, Ithaca, New York.

“Plunge pools are formed by the natural force of falling water, such as at a waterfall or cascade; they also result from man-made structures such as some spillway designs. Plunge pools are often very deep, generally related to the height of fall, the volume of water, the resistance of the rock below the pool and other factors.[4] The impacting and swirling water, sometimes carrying rocks within it, abrades the riverbed into a basin, which often features rough and irregular sides. Plunge pools can remain long after the waterfall has ceased flow or the stream has been diverted. Several examples of former plunge pools exist at Dry Falls in the Channeled Scablands of eastern Washington. They can also be found underwater in areas that were formerly above sea level, for example Perth Canyon off the coast of Western Australia.”

“Plunge pools are fluvial features of erosion which occur in the youthful stage of river development, characterized by steeper gradients and faster water flows. Where softer or fractured rock has been eroded back to a knickpoint, water continues to bombard its base. Because this rock is often less resistant than overlying strata, the water from the higher elevation continues eroding downward until an equilibrium is achieved.”

Reference: text in italics and quotes is from the Wikipedia, “Plunge Pool.”

Copyright 2023 All Rights Reserved Michael Stephen Wills

Treman Early Autumn Walk VI

Fairy Forest

Over a period of 11,000 years this former stream bed, abandoned when a melting tongue of the Laurentide Ice Sheet deposited drift across Enfield Creek, transformed to this sun dappled glade, one of two along the Gorge Trail of Treman Park.

Pam calls this the Fairy Forest for the feeling of peaceful expectation she feels here. Another reason is the small flowers of this native myrtle after which the periwinkle is named.

Fallen trees are left be to return to the soil.

“Vinca minor (common names lesser periwinkle, dwarf periwinkle is a species of flowering plant in the dogbane family, native to central and southern Europe, from Portugal and France north to the Netherlands and the Baltic States, east to the Caucasus, and also southwestern Asia in Turkey. Other vernacular names used in cultivation include small periwinkle, common periwinkle, and sometimes in the United States, myrtle or creeping myrtle.”

“Vinca minor is a trailing subshrub, spreading along the ground and rooting along the stems to form large clonal colonies and occasionally scrambling up to 40 centimeters (16 in) high but never twining or climbing. The leaves are evergreen, opposite, 2–4.5 centimeters (0.79–1.77 in) long and 1–2.5 centimeters (0.39–0.98 in) broad, glossy dark green with a leathery texture and an entire margin.

“The flowers are solitary in the leaf axils and are produced mainly from early spring to mid-summer but with a few flowers still produced into the autumn; they are violet-purple (pale purple or white in some cultivated selections), 2–3 centimeters (0.79–1.18 in) diameter, with a five-lobed corolla. The fruit is a pair of follicles 2.5 centimeters (0.98 in) long, containing numerous seeds.”

“The species is commonly grown as a groundcover in temperate gardens for its evergreen foliage, spring and summer flowers, ease of culture, and dense habit that smothers most weeds.”

“Vinca minor contains more than 50 alkaloids, including vincamine. Other alkaloids include reserpine, rescinnamine, akuammicine, majdine, vinerine, ervine, vineridine, tombozine, vincamajine, vincanine, vincanidine, vinburnine, apovincamine, vincaminol, desoxyvincaminol, vincorine[ and perivincine.  Vinpocetine (brand names: Cavinton, Intelectol; chemical name: ethyl apovincaminate) is a semisynthetic derivative alkaloid of vincamine.”

It is possible this is a cemetery as myrtle was once commonly planted in cemeteries in parts of the United States and naturalized periwinkle may indicate the presence of graves whose other markers have disappeared.

Reference: text in italics and quotes is from the Wikipedia, “Vinca Minor.”

Copyright 2023 All Rights Reserved Michael Stephen Wills

Treman Early Autumn Walk V

a drift filled stream bed

Wisconsin Glacial Episode was only the latest of a series of ice wall incursions. For this walk I went off the path to bushwack, following a drift filled stream bed, evidence of multiple glacial incursions with subsequent changing the stream bed of Enfield Creek. Here I am walking on glacial deposition to the north of the current creek bed. A park ranger informed us of this location, it is difficult to comprehend or imaging a 50 foot hill of material deposited in this way. The creek does bend at this point and the deposition is easily seen from above.

Enfield Creek flows to the right of the deposition.

The surface of the hill is hummocky, typical of glacial deposition.

Eventually the former stream bed intersects with a work road sloping back down to the Gorge Trail. It was here I found the oak apple gall of yesterday’s posting.

Copyright 2023 All Rights Reserved Michael Stephen Wills

Treman Early Autumn Walk IV

Oak Gall

This is an Oak Apple gall. An adult female wasp lays single eggs in developing leaf buds. The wasp larvae feed on the gall tissue resulting from their secretions, which modify the oak bud into the gall, a structure that protects the developing larvae until they undergo metamorphosis into adults.

“Oak galls have been used in the production of ink since at least the time of the Roman Empire. From the Middle Ages to the early twentieth century, iron gall ink was the main medium used for writing in the Western world.”

“Gall nuts are a source of tannin in the production of iron gall ink. Tannins belong to a group of molecules known as polyphenols and can be taken from different parts of plants such as leaves, pods, fruits, and gall nuts.”

“Along with gall nuts, other important ingredients in the production of iron gall ink include iron sulfate and gum arabic. The reaction between the tannins from the gall nut and the iron produces a complex that gives the iron gall ink its color. The gum arabic makes the ink more viscous and helps bind the ink to the writing surface.”

“According to recent research, traces of iron-gall ink have been found on the Dead Sea scrolls and on the ‘lost’ Gospel of Judas. Iron-gall ink may have been used for 1,800 years, but it does not withstand the test of time well. Over the course of centuries, the ink fades, and discolours and damages the paper. Iron gall ink is manufactured chiefly by artists enthusiastic about reviving old methods or possibly forgers of old documents.”

Reference: text in italics and quotes is from the Wikipedia, “Oak Apple Gall” and “Oak Marble Gall.”

Copyright 2023 All Rights Reserved Michael Stephen Wills