Fillmore Glen Autumn
Between bridges six (6) and seven (7) on the Gorge trail a cascade comes down the canyon wall. Mid-summer this brook can dry out, the waterfall disappears leaving this spot naked of water.
Taken over a period of thirteen (13) years, the cascade was alive and well autumn-time. This year, after the summer drought our autumn rains were sparse, the flow is the lowest photographed.
A Photo Essay
Down and Down
Weathered masonry at the height of Torr Head was there to serve the custom house and as support for a spotting station where ships transiting the Strait of Moyle (Irish Sruth na Maoile), the 12 miles of water to the Mull of Kintyre.
Lloyd’s of London, vitally interested in the appearance of ships’ progress crossing the oceans, had notice of passage via semaphore (and, later, Marconi’s “wireless”). Destination ports were copied in.
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The Way South –
Scottish influences touched the landscape covered by yesterday’s post, today we continue on this subject with these south facing views from Torr Head. The far ridge of Torrcor marks Loughan Bay.
A townland on the other side of Torrcor hill (and townland) has an eponymous ruin, Altagore Cashel. Mores the pity we did not visit this site, a thick drystone enclosing wall from the 5th century (you can see photographs from another site at this link). Cashel is from the Irish Caiseal, a circular, defensive fort (“ring fort”).
Books such as “Antrim and Argyll: Some Aspects of the Connections” tell of connections over the millennia, clan associations between the islands and ring forts such as Altagore Cashel.
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Salmon Run
Late spring and summer, weekdays, a net is stretched across the bay to catch salmon nosing up the coast, searching for their home spawning stream, here called Altmore Burn. “Burn” is a Scottish term for a fresh water source, evidence of the influence 12 miles across the north channel.
The small harbor seen here from Torr Head is for the salmon fishery. Small boats will seek shelter here from the wind and tides strong enough to roar in passing the Head, like a fast flowing river.
Neolithic Passage Tomb
Taking in a flower meadow, foreground, coaster sheep pastures, the photograph, below, looks north from Torr Head. The high hill, midground, is Greenanmore, notable for a the largest passage tomb of the Antrim Glens. Locally known as “Barrach’s Tomb,” for the Red Branch knight of the 1st Century AD fort on Torr Head, tree ring research of the mid-20th Century dates these tombs in the neolithic The hilltop passage tomb was an ancient relic when the mortar of Barrach’s Torr Head fort was drying.
When I enlarge the original photograph, visible on the ridge is a decommissioned Cold War listening post, the tomb is near that. The distant land across the North Channel water is Rathlin Island.
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Lima is home to 10 million Peruvians and over 1000 historical sites.
View of Clinica Delgado (hospital) from Lima Peru’s Elias Aguirre (street), Huaca Pucllana filling the foreground. Huacas are commonly located in nearly all regions of Peru outside the deepest parts of the Amazon basin in correlation with the regions populated by the pre-Inca and Inca early civilizations. They can be found in downtown Lima today in almost every district, the city having been built around them. Huaca Pucllana, located in Miraflores district, is an adobe and clay pyramid built from seven staggered platforms. It served as an important ceremonial and administrative center for the advancement of the Lima Culture, a society which developed in the Peruvian Central Coast between the years of 200 AD and 700 AD.
This is the New York Times article that inspired me to remember visiting Huaca Pucllana during our February 2016 tour of Lima, Peru. “3,000 Years of History Are Literally Just Beneath Our Feet.”
Looking east
This the fifth and final of a series of landscape photographs taken from this position.
The peak is named, in the English language, Slievenaglogh. It is so strange as it’s not English, being instead a transliteration of the Irish name “Sliabh na gCloch.” This is “Rock Mountain” translated literally. Slievenaglogh is carried to the townland, a long thin swath of land being the peak and associated ridge-line.
The rocks up there are called “gabbro,” a type of magma slowly cooled under ground. Slievenaglog, Slieve Foy across the valley, and the Morne mountains all formed within volcano magma chamber(s) of the Paleocene, 66 million years ago, a time associated with extensive volcanism and the Cretaceous–Paleogene extinction event that gave rise to the current age.
Our younger cousin has been up there, optimistically we left it for a later trip.
View of Slieve Foy
This the fourth of a series of landscape photographs taken from this position.
The distant ridge, Slieve Foy, is the site of a mythic battle from the epic “The Cattle Raid of Cooley” (Irish: Táin Bó Cúailnge).
Pam and I did a circuit of the island, returning to the home of my Mom’s first cousin. Our last full day on Ireland a cousin took us on the Tain Trail, over Maeve’s Gap of Slieve Foy and into Carlingford town.
Our route is partly visible to the right of the ridge, hidden in low clouds.
Rural Scenery
These are the second and third of a series of landscape photographs taken from this position. See the previous post for the first.
I visited here early morning of the Monday Pam and I embarked on a trip around the island of Ireland.
Arrived the previous Saturday when, after some sites between Dublin airport and the Cooley Peninsula, we met my Mom’s first cousin who had invited us for a visit. We had a grand time meeting them.
The ruin in this view is on the slopes of the peak. Some of these ruins are former homes with the replacement nearby. This appears to be an abandoned farm.
Click Me for the first post of this series.
Click me for the next post of this series.
Michael Stephen Wills Photography 