The Cave?

The Object Comes Into View

Flowing water eroded away until this durable limestone strata.  The majority of sedimentary rock is shale, only 6% is limestone.  Throughout the Finger Lakes and elsewhere, this is why when flowing water exposed the edge of a limestone strata, the underlying, soft shales are worn away to reveal a waterfall, ever deepening.  Eventually, the support of the limestone washes away to form this ledge.  Here it is an ephemeral cave behind a curtain of ice.

See “The Fang?” for the first post of this series.

Advertisements

Falling Water

SONY DSC

Amid the crystallized water, super-cooled, flowing water seeps through the structure to fall free.

See “The Fang” for the first post of this series.

Autumn Stroll in Sapsucker Woods

a meditaton

On Halloween morning 2004 I set out with a camera upgrade purchased spring of that year, a Sony “Cyber Shot, DSC-F828” with an inexpensive tripod. My photograph “Autumn Stroll in Sapsucker Woods”, the feature photograph and below, achieved prizes with the Photographic Society of American and a few sales of self-produced prints. It was an early success.

Click any photograph to visit my Online Gallery “Finger Lakes Memories.”

It is available on my Finger Lakes Memories online gallery where I provide recommendations for sizing, the best print medium with ideas for frame and matt.

The fall of 2005 I invested in a Kodak DCS Pro dslr-c and a Canon EF 50mm f/1.4 USM lens.  October 30, 2005, one day short of the 2004 Halloween shoot, found me driving down Fall Creek Road on a mission of revisiting Sapsucker Woods to possibly improve upon my offerings.

Over the years, travelling Fall Creek Road on my daily commute, I admired this well formed maple next to a farm field.  At 6:45 am the sun was about this rise, the frost limned grass not yet burned off.  This tree turned a bright yellow, here a green-yellow and dull.  The form of the tree is perfect.  I was never able to catch this at the right moment, it is still there and maybe I can time it this year during a pick-up of my grandson.  If I do, my intention is to climb the fence and use the 24 mm lens to capture the tree and shed with less sky (unless there are some dramatic clouds).  That day, I needed to make time for Sapsucker woods.

On site, thirty minutes later, as the leaves of the Fall Creek Road maple predicted, Sapsucker Woods foliage is behind last year’s by a week or so.  In “Autumn Stroll in Sapsucker Woods” the over story leaves have fallen and the understory is at peak.  Here, I believe the overstory is gone, the understory leaves are yellow-green.

I carefully choose the sites and this one is a risen walk of boards.  In the nine years since, the walk as deteriorated and this scene will be different, possibly.

This is a match for the 2004 photograph as far as the camera position.  What I enjoy from the 2004 version, aside from the foliage, are the details of the fallen leaves taking up the foreground, a carpet filling the field to lead the eye up through the trees, path fading from view to the right.

This effect is not possible on the boardwalk, above.  With the fixed focus 50 mm lens it might be possible with effort.  Today, the 24 mm is my first choice to capture this effect.

Here we can see the leaf carpet is possible, if the f-stop is higher to allow a crisp focus.  In this scene it is f2 because I happened upon a buck in a daze.  He was just standing there as I headed back to the car.  I did not risk changing out lenses to the telephoto, so I moved forward slowly.

The best I did was this rear view as he looked backward.  Lack of flexibility is a draw back of a fixed-focus lens.

In 2004 my day concluded with Robert Treman State Park.  In 2005 the 50 mm fixed focus with a ND filter and tripod was in its element.  The sun is higher and overcast, one background tree is a peak foliage.  The moderate water flow and stair complete the effect.  This was my best work of that day.  I need to get this up on the “Finger Lakes Memories” gallery.

Other postings of interest. Click the link to go there.

“Last Sunlight” — the Gorge Waterfall

“Autumn Evening Hike Part 1 of 3”

 

Copyright 2018 Michael Stephen Wills All Rights Reserved

Spillway Falls with Hemlock

hemlock grace and water

The Dry Creek dam is across the upper, eastern, end of Fillmore Glen. Historical records of the dam construction must exist someplace. My opinion is, somewhere in the federal bureaucracy there is a record proving this dam was constructed by Roosevelt’s Civilian Conservation Corps in the 1930’s. That is when the gorge trails were dramatically improved and it is logical a dam was necessary to control water flow during times of heavy rainfall and the spring thaw, to allow a full appreciation of the gorge beauty. It is a substantial concrete structure with cast iron controls, two spillways: one never, the second always flowing. This day the reservoir is full, frequented by beavers, stocked trout, herons, blue jays, crows, hermit thrush. The reservoir banks are thick with wildflowers of the season. This afternoon I noticed purple flowering raspberries: a past prime bloom or two, ripe fruit growing in the late afternoon shade on the south side of the dam.

Unlike its name, Dry Creek is perennial, fed by a broad drainage of pastures, cornfields and forests. Year round the spillway runs, feeding into the gorge a constant, reliable supply of water for the many waterfalls for which Fillmore Glen State Park is known. The very first waterfall is on the rocks supporting the north side of the dam, formed where water from the spillway flows over these rocks into a deep, east west gorge overhung on the south side by mature hemlock trees.

I first encountered Fillmore Glen in the 1980’s with my young son, Sean. On Sundays he and I walked as far as he tolerated, about half way to the dam site, where the gorge makes a turn to the south, the trail on an unstable clay bank against a crumbling shale cliff. Rediscovering the park in the early 2000’s, along with my interest in photography, I noticed the waterfall just below the dam many times and admired it for how the water caught late afternoon light over the many grace points created by rock crags like a wedding cake. The angle from the dam path is wrong for capturing this effect. Today was a first for me to leave the safety of the dam path to climb into the gorge, on the south gorge wall, for a shot.

Here is a view of the spillway fall on a mid-August afternoon, 2017. My photography kit for this walk with my wife, Pam, was minimal: a Sony Alpha 700 with a variable lens, the flash and a Manfrotto carbon fiber tripod. For this version of the spillway I climbed into the gorge on the south wall, about 40 feet above the creek. A hemlock tree branch fell across the view, incorporated into the composition. These hemlocks are not a biological relative of the Socratic, poisonous, hemlock. The relationship is a similar aroma when the leaves are crushed. The f stop is cranked to 36, ISO set to 100 so slow exposure time to 1.6 second. Post shot processing via Photoshop.

Click this link or the photograph for my Online gallery of this offering

Spillway Falls and Hemlock Branch -- CLICK ME!!!!

Copyright 2017 Michael Stephen Wills All Rights Reserved

Rainbow Falls, Watkins Glen State Park

Want more? Click this link or any photograph for my Online Gallery.

In the nature of fame, today Watkins Glen is the best known of the Finger Lakes State Parks. The International Speedway of that name enhanced and amplified name recognition during the post war years. Founded in 1948, the course used public roads of the town until the inevitable happened, an accident and the death of a seven year old child in a group of sidewalk spectators when a racer lost control.

The glen predates the race by 12,000+ years formed at that time from glaciation using materials from distant eons . Watkins Glen was known as a tourist attraction from the 19th century for the resort hotel on the south gorge rim, acquired and developed by New York State in the first years of the 20th century.

From a gate off “Lovers Lane” a sturdy flight of concrete steps with custom made handrails lead to an observation platform over the gorge. This feature will be known to many future generations……

Lovers Lane Observation Platform– CLICK ME!!!!

…….the fine grained concrete is worthy of a Roman wall, the heavy iron handrails were built to specification as flowing curves unlike what is done today: built as modules and accommodated on site.

Lovers Lane Observation Platform– CLICK ME!!!!

In the 20th century the fame of Watkins Glen attracted the road race, the popularity of racing enhanced park attendance. Today, the gorge trail of crowded summer weekends. On Tuesday, August 1, 2017 Pam packed a picnic lunch and we made a late start for a weekday visit. The upper entrance is enhanced by mature trees, oak, elm, hemlocks. We had our picnic under these on a moldy smelling picnic table enhanced with a green striped table cloth and fresh coffee.

Pam is my personal photographer. Here is an example of her work.

Michael Wills in Watkins Glen– CLICK ME!!!!

To give me my due, I did the driving and carried the 30+ pound pack into the gorge.

Pam captured me in position downstream from Rainbow Falls with a Manfrotto tripod with hydrostatic ball head on which is mounted a Canon EOS 1Ds Mark III and Canon EF 24mm f1.4 II USM lens, Tiffen nd 0.9 filter.

It was coming up to 4 pm eastern daylight savings time, the sun still high overhead. I needed to carefully choose a position for a frame in the wide angle lens without hot spots. Here are two results.

The sun was just of the gorge rim, to the right. Rainbow Falls forms from the tributary to Glen Creek cascading over the gorge walls.

Rainbow Falls of Watkins Glen– CLICK ME!!!!

Visitors walk under the falls where falling water eroded the soft, underlying stone to form an overhang.

Rainbow Falls of Watkins Glen– CLICK ME!!!!

Copyright 2017 Michael Stephen Wills All Rights Reserved