The deep gully on the west side of Crantock Beach is known as Piper's Hole. Within this, inside the first cave on the right is a flat surface with carvings which include a female figure, a horse and a few lines of verse.
This has given rise to romantic stories that the poem and drawings were carved by an an artist after his lover got cut off by the tide on her horse and both were washed out to sea. However the horse was added around 40 years later and its tail wasn't added until 2011!
The original carving made of the female figure was made by London artist Joseph Prater who often visited relatives in Crantock and made the carving on one of his visits, probably in the early 1900s. The identity of the woman is not known. The horse was carved in the 1940s by James Dyer of Crantock but for some reason this didn't include a tail. The carving was tidied up by an artist commissioned by the Parish Council in 2011, removing some graffiti, re-carving the poem and adding the missing tail.
During the summer months, a ferry operates at high tide between the Fern Pit Café and the beach at Crantock.
Crantock beach is a dune-backed beach south of Newquay across which the River Gannel runs. Due to the strong currents associated with the tidal river, the northern area of the beach is not recommended for swimming. The best place to swim is towards the southern side, backed by the cliffs of West Pentire.
From West Pentire, there are steps from the coast path leading down to the inlet near the Bowgie Inn and another path leading down at Vugga Cove. However, there is no way up from the cliffs around Piper's Hole at the back of the beach so care should be taken not to be trapped in the inlets here by a rising tide. Currents along the cliffs also sometimes create depressions in the sand which fill up with water as the tide comes in forming deep pools which can result in unwary people being marooned on sandbars.
The name of the river is from the Cornish An Ganel meaning "the channel". At high tide, the River Gannel used to be navigable all the way to Trevemper Bridge, and schooners and barges would transport coal, timber and sand to the mining and agricultural industries further inland. In 1838 the East Wheal Rose mine began discharging mine waste into the tributaries of the river. This caused silting and slime to coat the riverbed. Despite complaints to the Admiralty about the impact on the river's navigability, the silting continued.
Since the closure of the mines, the water quality has greatly improved and the Gannel river supports wildlife including salmon and the once common but now endangered European eel. The salt marshes created by the silting have also become an important habitat which is now earmarked for protection within a Marine Conservation Zone.
The settlement of Penpol was recorded in 1216, and is Cornish for "top of the creek". The word pol - literally "pool" - was also used to refer to a natural harbour, e.g. Polperro.
Rosebay willowherb is a tall plant with a spike of pink flowers in late summer which can often be seen beside paths and tracks. Their long leaves have a distinctive thin, white vein along the centre.
The name "rosebay" dates from at least Tudor times and is thought to be based on loose resemblances of the leaves to bay leaves and the flowers to wild roses. The overall family are also known as "willowherbs" due to the resemblance of the leaves to willow leaves. The two names have since been brought together resulting in the slightly confusing duplicate description of the leaf shape.
As long as the sun is below 42 degrees from the horizon, you can see a rainbow. In the summer, the angle of the sun is too high during the middle of the day for rainbows but you can still get them in the morning and evening (you can potentially see a rainbow before about 10 am and after about 5 pm on any day in Cornwall).
The path to the left leads down to the shore, but a deep stream runs from the top of the creek, cutting off the higher part of the Gannel estuary.
Common knapweed (also known as black knapweed) is most easily recognised by its bright purple thistle-like flowers but without spiky leaves. It's actually a member of the daisy family and is often seen along paths and roadside verges. Other names for the plant include "hardhead" (used in Cornwall in Victorian times) and "loggerhead" due to the sturdy flower heads. "knap" is from the Middle English word for "knob" and consequently another name for the plant is "knobweed".
It is an important plant for pollinating insects and was rated in the top 5 for most nectar production in a UK plants survey. In terms of plants that produce both nectar and pollen, it is rated as the top producer overall, producing a good amount of each.
The little egret - a white member of the heron family - can be seen on many of the creeks in Cornwall and yet is only a very recent settler in Britain. The birds first appeared in Britain in any number in 1989 and the first to breed was in 1996 in Dorset.
The more widely accepted theory for the name is that it is based on the way that the gate touches either side of the enclosure which is a key feature of the design. The word "kiss" is in the sense of "light touch" as used in e.g. billiards.
In order to attract pollinating insects, the plant heats the flower spike up to 15°C above that of the surroundings. The plant exudes a smell of decaying flesh which attracts flies and the flower is designed to trap these. Within the flower, the female organs mature first and insects carrying pollen from other plants (together with any unlucky enough not to be) are imprisoned behind a row a spines within the flower. Once the plant is pollinated, the male organs quickly mature and the plant's own pollen is dusted over the trapped flies. The spines then wither away enough for the flies to escape.
All members of the lily family, including wild arum, are poisonous to dogs.
Rooks nest in colonies and are one of the most social members of the crow family. Scientists have found that rooks are happy to work cooperatively to solve problems (e.g. each pulling on a separate string to release food).
During Victorian times there was a lime kiln beside the river and a quay for unloading coal and limestone.
Internally, a lime kiln consisted of a conical stone or brick-lined chamber which was loaded from the top with alternating layers of limestone and carbon-rich fuel such as charcoal, peat or coal. At the side of the kiln was an alcove known as an "eye" which was used to access the kiln and remove the quicklime from a hole at the bottom of the chamber. The kiln was often run continuously with more layers of fuel and limestone added to the top as the previous layers worked their way down through the kiln. Air was drawn in through the bottom of the kiln and heated up as it passed through the quicklime (also cooling the quicklime) before it reached the level where combustion was taking place.
One of the fields on the right was known as "Chapel Close". There is a record of some foundations of a building being found here in 1959. It was thought that these might be the remains of a mediaeval chapel. Nothing has been found or recorded since but there are remains of what appears to be a mediaeval field system nearby.
A settlement at Trevithick was already present in the 1880s, although not named on OS maps until the 1900s. The buildings are likely to have been built from stone quarried in one of the nearby fields (just where the public footpath emerges from a walkway crossing the stream). The quarry is referred to as "old" in the 1880s. The name in Cornish means something along the lines of "woodland farm" which would be consistent with the wooded valley along the stream. It's possible that the settlement may have early mediaeval origins (when the Cornish language was spoken by landowners and used to name places). There is evidence of old, possibly mediaeval, boundaries within the fields which are also recorded on 19th Century maps.
The wooded valley surrounds the small stream running into Penpol Creek. The tree cover provides shelter for wildlife including robins and blackbirds.
Blackbirds in the UK are resident all year round but the blackbirds that live further north (e.g. in Norway) migrate south for the winter. To help with migration and also to avoid being eaten by predators, blackbirds can sleep half their brain at a time. This allows them to get some rest whilst still maintaining enough alertness to fly or spot predators.
The reason the sky looks blue is due to rays of light travelling out from the sun in directions that would normally not reach your eyes. When these bump into a molecule of air, they are scattered in all directions, one of which is the way you are looking. As the blue-violet end of the rainbow is scattered more, there are more of these colours but we see just blue both because our eyes are much more sensitive to blue than violet and also because some of the violet is absorbed by other interactions with molecules in the atmosphere.
Red campion is also known by a few local names including Johnny Woods (from its habitat) and Ragged Jack (from its flower shape). Some are colour references such as Scalded Apples, and particularly in the southwest, Red Riding Hood. Cuckoo-flower is a reference to the time of year that it flowers. Another name - "Batchelors' buttons" - suggests it was once worn as a buttonhole by young men.
The Ramblers Association and National Farmers Union suggest some "dos and don'ts" for walkers which we've collated with some info from the local Countryside Access Team.
Do
Don't
There are several different reasons why passing walkers should never feed horses. A range of plants can make horses ill and many human foods such as chocolate also contain cumulative poisons that build up over time. The horse could also have allergies to a normally safe plant or have an underlying medical condition such as blood sugar issues. A horse may have behavioural problems that feeding it can make worse, and singling a horse out for "special" attention can also cause it to be attacked by jealous herd members. Some horses may also accidentally bite a hand containing food even when held flat.
The Latin name of the buttercup, Ranunculus, means "little frog" and said to be because the plants like wet conditions. It is thought it may have come via a derogatory name for people who lived near marshes!
The efficiency of the chemical processes that plants use to metabolise nitrogen compounds varies with pH (acidity). In soils that are too acidic, many plants have trouble absorbing nitrogen (apart from specially-adapted ones known as "ericaceous"). The ongoing decomposition of plant matter into humus within the soil creates acidic compounds. Some soils contain rocks such as chalk and limestone which will react with the acid and neutralise it. In Cornwall, the beach sand includes a high proportion of seashell fragments which contain the same chemical compound as limestone.
The settlement of Crantock dates back to AD 460, when a group of Irish or possibly Welsh hermits founded a chapel there. The parish was once known as Langurroc, which translates as "The Dwelling of Monks". The chapel of Langurroc was said to have been covered up in a sandstorm, and may lie beneath the sand dunes behind Crantock Beach. The village church is dedicated to St Carantoc - said to be one of the founders of the village. In its heyday, when the River Gannel was navigable, Crantock was a river port.
The Memorial Hall commemorates the villagers lost in the First World War.
During the First World War nearly 10,000,000 military personnel and over 10,000,000 civilians were killed. A further 23 million people were injured. In addition, over 8,000,000 horses, mules and donkeys and more than 1,000,000 dogs lost their lives. The sixteen million animals that served in World War 1 are commemorated with purple poppies.
Crantock holy well, located beside Well Cottage, is thought may date from mediaeval times although it has also been reported by one source as being 17th Century. In mid-Victorian times, the well was covered by a flat-topped structure. In 1894, it was recorded with a well-house resembling the one seen today:
the holy well still exists, in the centre of the village, near the church, covered with a curious bee-hive shaped structure with a door. The villagers use the water for all household purposes, and when a pump was erected still preferred the sacred water. It has never been said to have possessed any special virtues.
The Old Albion Inn is around 400 years old and was partially rebuilt after a fire in 1902. Albion is thought to be the name of a ship built in the Gannel shipyard when Crantock was a busy sea port. The main fireplaces in the pub both have original pasty ovens and the one in the lounge (originally the kitchen) had an entrance to a hole for storing smuggled goods. Water for the pub used to be drawn from a deep well beneath the old bar.
After the Norman conquest, the church at Crantock was re-founded in the 13th Century as a college of canons. The 13th Century church included a tower which had fallen into disrepair by the 15th Century and collapsed, destroying much of the nave. The church was rebuilt but in Tudor times, the college was shut down as part of the dissolution of the monasteries and the church once again went into slow decline. At the end of the 19th Century, a restoration was carried out which was completed in 1902, rescuing as much of the mediaeval material as possible. An electrical fault caused a fire in 1985 which damaged the organ and roof. The stained-glass windows tell the story of St Carantoc.
The old village stocks are now in the church.
The stocks was a form of punishment introduced in mediaeval times and was a common sight in most villages by the 16th Century. Many sets of village stocks were able to accommodate the ankles of multiple offenders seated on a bench. The last recorded use was in 1872 but it was never formally abolished and is therefore still a legal form of punishment in the UK although the acts carried out by passers-by in mediaeval times would not be. By Victorian times, it was mostly foot-tickling by mischievous children.
The stiles in Cornwall that consist of rectangular bars of granite resembling a cattle grid are known as "coffen" (coffin) stiles. These often occur on footpaths leading to churches such as the Zennor Churchway. The mini cattle grids are fairly effective at containing livestock and were significantly easier for coffin-bearers to navigate than stiles crossing walls. They are more frequently found in West Cornwall but there are a few in East Cornwall such as those on either side of Advent Church.
There are historic references to St Ambrew's Well, St Ambrose Well and St Ambrusca's Well and it is thought to have been destroyed many years ago to make way for the building of a house. The well on Beach Road marked "Ambrose" dates from the early 20th Century. Some confusion has arisen because of the wooden door with the Ambrose inscription but this is thought to simply be a memento to the original well added by the villagers when it was constructed in the early 20th Century.
The red telephone box was the result of a competition in 1924 to design a more aesthetically-pleasing telephone kiosk that would be acceptable to the London Metropolitan Boroughs who weren't impressed by the Post Office's first 1921 model made from concrete. Three subsequent versions were used mostly in London. The final design was created in 1935 to commemorate the jubilee of George V and was deployed widely across the country.
The bright red telephone box was initially not well-received and the Post Office was forced to use an alternative colour scheme (grey with red glazing bars) for areas of natural beauty. Ironically, many of the telephone boxes preserved in these areas have since been painted - the now iconic - red.
Sea purslane (Halimione portulacoides - Americans call a different plant "sea purslane") grows along estuary mudflats and is immediately recognisable by its grey-green leaves forming a large carpet near the high tide line. The greyness of the leaves is partly due to tiny hairs which reflect sunlight to reduce water loss. It's also due to salt expelled through special glands in the leaves drying on the surface.
Sea purslane leaves are edible (and often feature on Masterchef amongst "sea vegetables"). They are very salty when raw, but when cooked this diminishes to more mellow levels. They turn bitter if overcooked, so a short dunk is ideal. The young, green leaves are the most tender which are most abundant in late spring/early summer.
Tides in the Atlantic are closely aligned with the moon's position above the Earth which takes just under 25 hours on average to return to the same position; this is slightly more than 24, as the Earth has to chase the moon's orbit. The tides therefore shift forward by at just under an hour each day so that over a 7 day week, low tide and high tide have approximately changed places (e.g. no beach in the afternoon vs a huge beach in the afternoon).
The moon's gravity pulls the water in the oceans towards it causing peaks in the ocean both directly under the moon but also on the opposite side of the Earth so high tides occur every 12-13 hours when the moon is either directly overhead or is on the opposite side. There are therefore just over 6 hours between low and high tide.
The speed with which the tide comes in or goes out follows a sine wave: slow at low tide, speeding up to the fastest at mid-tide (known as the "tide race", when currents are at their strongest) and slowing down again towards high tide. Thus high and low tides are also referred to as "slack tide" when tidal currents are at their minimum.
Dunes (called towans in Cornish) form when dry sand from the beach is blown by the wind, and initially lodges against an obstruction, eventually forming a ridge. More sand can then accumulate against the ridge and vegetation such as marram grass can then take hold, preventing the resulting sand hill from washing or blowing away.
Erosion of the vegetation by foot traffic can cause the dunes to disintegrate, so areas are sometimes fenced off to allow the all-important weeds to recover, particularly the seaward edge which is both the most fragile and most visited area. During the 1970s-80s erosion was at its worst but many dunes have since been stabilised. Some of the fencing has now been removed to allow some bare areas of sand to be created which are necessary for the natural process of sand migration to the dunes further inland.
Most of the major dunes on the North Cornish coastline are thought to have formed from around 5,000 years ago when sea levels finally stopped rising after the glacial ice from the last Ice Age had finished melting.
Since water drains away quickly through the sand, marram grass has evolved a number of strategies to capture and retain water including its waxy, curled leaves which contain hairs inside to minimise evaporation caused by moving air. Its roots form a fibrous mat which traps water but also plays a vital role in stabilising the dunes by stopping the sand blowing away. During the 17th Century, large amounts of marram grass were harvested for thatch and this destabilised the dunes so much that farms, estates and even entire villages were buried.
Full page maps cannot be printed due to copyright and terms of use.