Welsh Equinox: Kath Norgrove |
This year’s Autumnal Equinox took place on Wednesday 22nd
September 2021. The date coinciding with
our latest holiday to Wales and having arrived at Porthmadog, Gwynedd. Sunrise was around 7.02 am and the weather
started mild and cloudy with a light breeze and wet on the ground from
overnight rain.
After a quick breakfast at our hotel, we headed to Porthdinllaen, a promontory on the Llyn Peninsular north coast adjacent to the town of Morfa Nefyn.
Here, we undertook a circular 3.5 mile walk from Morfa Nefyn around the coast following a trail from an old AA guidebook. The walk starts at a National Trust carpark, in Morfa Nefyn, and follows a lane up to the former coastguard station, which today is the headquarters for the Nefyn Golf Club. Missing National Trust car park entrance on our way, we ended up parking in a field adjacent to the golf club and started the walk from here.Following the trail, we went
through the Golf Club’s main gate and continued along a tarmac access road down
towards the golf course. At a green
roofed shed, used for storage and maintenance, the trail turned southwest and
headed across the golf course to an iron shed.
However, this the iron shed was no longer to be seen and all that
remained was a sandstone gateway and hedgerow where the shed once stood. Our route then continued roughly westwards across
the golf course to steep cliffs falling to shingle beaches and dark rocky
outcrops.
When the walk was originally
written it followed a path northward that descended to a shingle bay (Borth Wen)
below. The route then crossed the bay to
ascend the steep cliffs on the far side and back up to the golf course. However, we could not find the path and no path
down into the bay. Looking closer at the
cliff edge it was apparent that the original path had succumbed to coastal
erosion and landsliding since the walk was first written. The landslide backscar and slip mass clearly
visible along the cliff edge. The
missing iron shed, and path raised our suspicions that the trail had been
penned a long time ago and the route had changed since. Other walks in the guidebook seem to hint
that it was originally written around 1975.
Abandoning the bay, we continued
northwards along the cliff / golf course edge where Jarrow, Cats Ear, Bell
Flowers, Common Ragwort, Gorse and some heather still flowered. Westerly winds pushed the clouds inland and
replaced them with clear blue skies that eventually permitted warm sunshine to
appear. Warm moist air from the sea was
forced upwards as it hit land creating a line of cumulus clouds that aerially mirrored
the coastline.
Our walk continued northwards
onto the Porthdinllaen promontory following steep rocky outcrops to our
left leading down to the sea. Before
long we came to a straight cleft cut through the rocky beach below. To our right and smack in the middle of the
golf course fairway was a vast sinkhole, or crownhole, approximately 29m to 39m
across. The cleft in the rocky beach
below lining up nicely with a hole in the sinkhole’s base.
Later, a look at the British
Geological Survey website revealed that the rocks we were walking over were
Cambrian volcanics that included pillow basalts and tuffs. Intruded into these rocks were short and
straight, Ordovician, microgabbro dykes.
Once such dyke matched precisely the cleft we saw in the rocks and
associated with the sinkhole. The dyke
having weathered and eroded beneath the golf course and leading to the sinkhole
forming. Further along the walk, the
coastline had been dramatically reshaped where an historical dyke had eroded
leading to a crown hole collapse and coastal erosion.
Historically, the promontory was used as an iron age fort and all that
remained was a low earth embankment stretching from east to west. The old fort ramparts were a reminder that twelve
months previously, for the Autumnal Equinox 2020, we had ascended Moel Famau
and Foel Fenlli in the Clwydian Range in eastern North Wales. Moel Famau is the tallest peak in the range,
at 554m, and Foel Fenlli represents one of numerous Iron Age forts strung out
along the ranges length. Our recent Wales
excursions suggest that the region was a magnet for Stone and Iron Age
settlements, fortifications and burial places.
On reaching the promontory’s
northern end, we came to Trwyn Porth Dillaen lookout station sitting high up on
an exposure of Cambrian pillow basalts.
These rocks having formed from submarine eruptions on submerged volcanic
flanks around 600 million years ago. The
molten lava surface instantly chilling as it contacted seawater resulting in
the eruption effusing gently like toothpaste from a tube. The result being rounded structures
resembling pillows. Hence the name.
We sat and ate lunch on the
Promontory’s northern end, on exposed basalt rocks close to the sea. In the shallows up to five grey seals bobbed
about and rose and sank below the waves. One light coloured female seal made grunting
sounds and rolled over slapping her flippers on the surface to show her
dissatisfaction at a dark coloured male’s advances. The seals stayed away from the deeper waters
where the outgoing tides could be seen at surface. On a nearby rock perched numerous Cormorants
and Shags sunning themselves. Some could
be seen floating on the water below the rocks and raising their heads like
marine serpents. In the rocks and
vegetation around us Meadow Pipits flitted about and tweeted.
After over an hour watching the
seals, we headed south along the golf course / promontory eastern edge and down
to Porth Dillaen. A small cluster of
buildings that historically formed a port with its own shipyards. Today the local pub, Ty Coch Inn, does a
bustling trade for beach goers looking for refreshments. Back and north along the coastline from Porth
Dillaen, was the newer location for the lifeguard station. From Porth Dillaen, we followed a sandy and
shingle beach eastwards to Morfa Nefyn and to the National Trust carpark, before
stopping for an ice cream at Caffi Porthdinllaen and headeding back to the car.
Inland windy and cloudier
conditions prevailed and hid the sun. Leaving Morfa Nefyn, we headed east along the
coast to Yr Eifl which comprises three hills – Garn For (444m), Tre’r Ceiri
Hillfort (480m) and Garn Ganol (564m). Through
variable sunny and windy conditions, we ascended a circular route up to the
summit of Tre’r Ceiri Hillfort. This
2,000 year old structure being enclosed by stonewall ramparts and containing
around 150 stone hut circles. The cold
and windy, exposed conditions made the hill fort feel like it would have been a
tough place to live.
Now situated within a National
Nature Reserve, Tre’r Ceiri Hillfort is one of the finest of its kind. The
rocks forming the Yr Eifl hills are intruded Tre'r Ceiri Microgranite and
Caergribin Rhyolite, no date for which is given. The cold and blustery conditions on the Tre’r
Ceiri Hillfort summit and the sun going down put us off wanting to return via
Garn Ganol. So, we returned to the car
via the route we came. From Tre’r Ceiri
hill, the view around the surrounding landscape was spectacular and our
Ordnance Survey map revealed many more iron age and stone age wonders to visit.
With the sun rapidly approaching the horizon and before heading back to Porthmadog, we ended our equinox 12 daylight hours on the beach at Criccieth. South-westerly winds driving waves ashore and the sun putting on a colourful display as it set around 7.16 pm. Under darkening skies, we headed back to Porthmadog and to find somewhere for dinner.
1 comment:
Interesting Andy and so much information! We had a few days close to Morfa Nefyn last year during one of the brief periods when we were allowed out. Stayed in Cricceth too and visited Porth Madog.
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