Cultivated vs Wild
Today I walked the Gorge Trail to below Lucifer Falls, crossed the bridge and returned via the South Rim Trail, a trip of over 5 miles according to the Apple IPhone 14 Pro Max used for these photographs.
Thankful I was not here when this tree gave way across the trail.
Information about a cultivated fern, followed by a photograph of the wild version, trailside.
Flourishing hayscented fern.
Swimming Under The Waterfall
Swimming area closed for the season, the waterfall is still a draw.
An overview on a perfect September morning.
The waterfall at the height of summer in years past.
A palatial bathhouse built by the Civilian Conservation Corps, “For the people, by the people.”
nonmigratory?
Thursday last, grandsons Sam and Rory and I visited Sapsucker Woods, enjoying a late summer morning. From the north side on Wilson Trail, these Canada geese landed on the pond.
In North America, nonmigratory Canada goose populations have been on the rise. The species is frequently found on golf courses, parking lots, and urban parks, which would have previously hosted only migratory geese on rare occasions.
Owing to its adaptability to human-altered areas, it has become one of the most common waterfowl species in North America. In many areas, nonmigratory Canada geese are now regarded as pests by humans.
They are suspected of being a cause of an increase in high fecal coliforms at beaches. An extended hunting season, deploying noise makers, and hazing by dogs have been used to disrupt suspect flocks.
A goal of conservationists has been to focus hunting on the nonmigratory populations (which tend to be larger and more of a nuisance) as opposed to migratory flocks showing natural behavior, which may be rarer.
Here is a sample of my wife Pam’s photography skills by way of a video with music created by her IPhone 8.
A Wall with Moss Padding
Pam examining thick moss growth on the sedimentary rock of Treman gorge. These layers of shale, sandstone, siltstone formed at the bottom of a broad, shallow sea over 380 million years ago.
Towards the bottom of the 223 Cliff Stair steps moss takes over the Devonian shale of the cliff wall surface. Here, the cliff shelters the wall from sunlight 365 days a year.
Robert H. Treman New York State Park.
“Red-shanks”
This geranium species (scientific name Geranium robertianum) are also called “Herb-Robert” for a reputed ability to ward off disease.
Scottish Highlands residents call these wild geraniums “red-shanks” for the deep red color of the stalks, seen in both photographs.
Robert H. Treman New York State Park.
Source, “How to Know the Wildflowers” by Mrs. William Star Dana, 1989, Houghton Mifflin, Boston.
read the sign
Each autumn, species of fern turns yellow towards a winter death. Here we see growing from Devonian shale, both the yellowed and desiccated fern fronds. Robert H. Treman New York State Park.
Pam pauses for a photograph
On a day in late October 2017 Pam and Mike did a photography walk. Here is Pam pausing to pose during a descent into the gorge on the cliff staircase after visiting the overlook high above Lucifer Falls, Robert H. Treman New York State Park in the Finger Lakes Region.
Grasses, hemlock saplings, goldenrod, spent leaves and ferns on the wall of the 223 Cliff Stair steps.
Several possible sources have been proposed for the name Taughannock, all of which describe Native American origins. One translation suggests that the name is derived from a combination of Iroquois and Algonquin terms meaning “great fall in the woods”. An alternate theory suggests that the name may refer to a Lenni Lenape (Delaware) chief named Taughannock who died near the falls during a battle.
During the second half of the nineteenth century, steamboats, railroads and Victorian hotels were built in the region to serve tourists who traveled to view the falls. By 1925 the hotels were failing due to a decline in tourism, and New York State began acquiring land to form a park.
J.S. Halsey built a two and a half story hotel in 1850, known variously as the Cataract Hotel or Taughannock House (or simply as Halsey’s Hotel) at the Taughannock Falls Overlook.
Visitors could reach the hotel by taking a train to Cayuga Lake, take a steamboat across the lake to Goodwin’s Point, then finally board a stagecoach to reach the hotel. The hotel site today is the location of the park visitor center and parking lot.
Enjoy!!
and ice cream!!
The waterfall and gorge comprise an example of a hanging valley, formed where Taughannock Creek’s stream-carved valley meets the deeper glacially carved valley that contains Cayuga Lake.
The gorge has continued to retreat westward from Cayuga Lake as easily eroded shale near the fall’s base is worn away by the stream, which supports erosion-resistant siltstone and sandstone found in the upper portions of the gorge.
Annual freeze and thaw cycles also act upon small faults in the rock, causing large sections to occasionally break away, further expanding the gorge.
Taughannock Falls’ main cataract is a 215-foot drop (66 m), making it 33 feet (10 m) taller than Niagara Falls. It is the tallest single-drop waterfall east of the Rocky Mountains. The waterfall is located along Taughannock Creek, which flows through a long gorge with cliffs up to 400 feet (120 m) high.
Enjoy!!
