End of a Mull of Galloway day.

We continued eastwards along the Mull of Galloway and came to a huge cave.


As we left the cavern in the gathering twilight, we caught sight of a waxing gibbous moon.


That reminded me of a total eclipse of the moon that was due at 3am on 21/02/2008. Since I had already got a great view and some photos on the last eclipse at 23:20 03/03/2007, I decided to give this one a miss!


Rounding the Mull of Galloway we encountered a brisk eddy which impeded our progress towards East Tarbert.


The chill February air caught our breath as the sun sank below Tarbert leaving us in darkness.

I have said this before, but you should come and paddle this amazing coast before the crowds come!

17/02/2008

Sea kayaking perfection at the Mull of Galloway.

When we entered the Mull of Galloway tide race we found ourselves travelling at 12km/hour when not paddling. Fortunately there was no wind or it would have been a real wild ride!


There are a couple of bays along the Mull that you can break out of the tide into. There are a variety of caves and stacks to explore.


As the sun went down we realised we would need to move on...


..to allow time to play on the eastern race beforer the sun went down.


Why do we go sea kayaking?

17/02/2008

Winter sunset as we approach the Mull.

We left Rainbow Rock as the thin winter sun was sinking towards the south western horizon and the air was full of the mournful calls of wheeling gulls.


With each headland we felt the power of the tide increase until it was like a huge lazy river, pushing us ever faster and inevitably towards the Mull of Galloway.


The rocks turned red as the sun sank lower.


We were often tempted to break out of the tide and take a diversion through rocky channels.


At last the Mull of Galloway, surmounted by its lighthouse, lay before us. We would be rounding it at 3 hours after slack water and there was now no turning back....

Rainbow Rock

Rainbow Rock, Rhinns of Galloway


Leaving Slouchnamorroch Bay, we continued our paddle past cliffs that plunged straight into the sea. Just offshore huge blocks were inclined to the same angle as the cliffs.


With increasing tidal assistance we made our way round Crammag Head and found ourselves under the rocky ramparts of Dunman Hill. Two millenia ago, ancient Britons held a hill fort on its southern flanks.


On the north going flood tide (this is looking south) the sea builds up behind this gap and you shoot through the gap like a river rapid.


Far beneath the summit of Dunman lies the "Y" cave.


We stopped for a second luncheon of Christmas cake, just south of Portdown Bay, at the stunning Rainbow Rock with its folded strata.

17/02/2008

The bare bones of the Earth exposed in Slouchnamorroch Bay

Rounding Cairnywellan Head we came across the most amazing coast of indented coves and jagged headlands. We entered a small cove just to the north of Slouchnamorroch Bay. Just for a moment, dwell on what sort of a landscape gives rise to such an original name as Slouchnamorroch! There are only a couple of references to it in Google and one of these is this site! Let me now introduce you to this corner where land and sea meet.


We drew our kayaks up onto a beach of bare bedrock.


There were boulders scattered about on the rock and you could see where they had worn hollows in the rock. One can only imagine the bedlam here on a stormy night when wild waves drive these boulders about the beach like some crazy pinball machine.


The beach was mostly bare of sea weeds and shellfish, but here and there a few barnacles and limpets survived in protected hollows and crevices.


A dyke rose boldly in the middle of the beach and marched its way inland to rise to the sky in the cliffs behind.


One can only imagine the cataclysmic forces that have created this place and yet we had it all to ourselves. We did not even need to get up particularly early, we left the house at 8am!

17/02/2008

Ocean Paddler #8 "Myths and tides of the Mull"

The Mull of Galloway.

Unfortunately there was not space in Ocean Paddler for the fact box to accompany the article: "Myths and Tides of the Mull" part one of a Rhinns of Galloway Trilogy. I will make sure there is room for the fact box in one of the remaining two articles. In the meantime, here is some information to help those planning a trip to this fantastic location.

The Mull of Galloway Essential Information.

Distance: 27km day trip.

Launch site: Drummore: NX141363. There is no toilet at the car park so stop at Ardwell NX109453 en route.

Landing site: Port Logan NX494094.

Getting there: From Glasgow, head south for Stranraer on the M77, then the A77. through Stranraer. Leave A77 on A716 for Ardwell then B7065 to leave shuttle car at Port Logan. 100 miles allow 2hours 30mins. Then take B7065/B7041 to Drummore 4.5 miles allow 15 minutes. If coming from the south or the east, head for Dumfries then west for Stranraer on the A75. Just before Stranraer, take the B0784 then A716 for Ardwell then B7065 for Port Logan. Dumfries to Port Logan is 60 miles allow 2 hrs.

Accommodation: For Hotel, B&B and self-catering accommodation: www.visitscotland.com. New England Bay Caravan Club Site NX120424, tel 01776 860 275, has beach access for kayaks.

Local weather forecast: BBC Radio Scotland (94 to 95 FM, 810 MW) Outdoors conditions forecasts are broadcast at 19.12 Monday-Friday, 06.58 and 18.58 on Saturday and 06.58 and 19.58 on Sunday.

Tidal constant: Mull of Galloway +0035 HW Dover; Drummore: +0045 HW Dover.

Tidal streams: Tidal stream information here that differs from the pilots is from personal observation and discussion with local fishermen. The pilots show that well south of the Mull of Galloway the E going stream (flood) begins at -0545 Dover and the W going stream (ebb) begins at +0020 Dover but close inshore, where kayakers will be, the east going stream begins about +0530 HW Dover and the W going stream about -0130 HW Dover. Spring rates exceed 9km/hr. From Port Kemmin to the Mull there is an E going eddy close inshore during the W going ebb, from about +0120 HW Dover. The interface with the main west going stream can be very disturbed.
To the west of the Rhinns of Galloway and close to shore, the S going stream (flood) begins +0425 Dover, the N going stream (ebb) begins -0135 HW Dover. There are overfalls at frequent places and after half tide (on both flood and ebb) counter eddies form close inshore. Spring rates at headlands exceed 12km/hr.

Tides on the day (24/03/2007): Our trip was midway between springs and neaps and we arrived off Lagvag, the east point of the Mull, at -0145 Dover. Note that Cooper and Reid suggest arriving slightly earlier than HW Liverpool (about HW Dover) if you do this, you will not round the Mull at slack water and you will face stronger eddies on the north part of the trip.

Warnings: This can be a serious trip if there is any wind against tide; here is a selection of descriptions from the pilots: one of the most dangerous points on the British coastline; heavy and violent race; the race at the Mull of Galloway is violent; passage can be hazardous on an outgoing tide in SW winds above force 4 and should not be attempted; very heavy seas off the Mull. Check tidal information with original sources and take account of conditions on the day.

Danger Area: Luce Bay is an active bombing range. If you keep inside the yellow buoys you should be well clear but if in doubt phone the range on 01776 888741.

Maps: OS Landranger 1:50,000 sheet 82; Imray Chart 1:150,000 sheet C62

Books: West Coast of Scotland Pilot, UK Hydrographic Office
West Coast of England and Wales Pilot, UK Hydrographic Office
The Yachtsman’s Pilot Clyde to Colonsay, Martin Lawrence
Firth of Clyde inc. North Channel, Solway Firth & Isle of Man, Clyde Cruising Club
Blazing Paddles, Brian Wilson
Scottish Sea Kayaking, Cooper and Reid

Useful website:
http://seakayakphoto.blogspot.com/search/label/Mull%20of%20Galloway

24/03/2007

Rockhopping down the Rhinns.

We set off from High Ardwell Bay on the wild west coast of the Rhinns of Galloway.


What followed is some of the best sea kayaking rockhopping you will get anywhere.


Round each headland there were yet more rocky channels and small stacks.


As we approached the Mull of Logan the flood tide began to build.


It ran through the channels like a river.


This magnificent arch is just SE of the Mull of Logan, it is not even marked on the map!


For the second time in a week, we bypassed a perfectly good sea kayaking pub (at Port Logan). Instead, we rounded Cairneywellan Head on our way to our first stop at Slouchnamorroch Bay.

17/02/2008