Assynt, Day 2: Solus Na Madainn

For the second day of my holiday last Autumn, I got up – again! – at a ludicrously early hour and drove from Tongue round to the Assynt peninsula, to my favourite viewpoint for sunrise.

It was some drive.

All the way from Tongue to Loch Assynt without seeing another car. Bliss.

Take the A838 road (abused as part of the ghastly NC500 coastal route) via Durness at 5am in the pitch black, the wind blowing a gale, rain + windscreen wipers on full speed.

Picture avoiding a herd cows intruding across the road. Avoiding more than 10 deer.

At that surreal pre-caffeinated hour of the morning, seeing a signpost advertising “serving local seafood” makes me picture a restaurant waiter taking a scallop’s order at table.
The music of choice was Arcade Fire Mountains beyond Mountains – a song bemoaning city life with its world so small – a mental image contrasting with my surroundings, passing rural Scourie, pop 132 – the sort of place that takes longer to say the name than drive through.

And so I arrived at Rhicarn – the landscape black, clouds a grey plasma, just a little bit windy…

And the sun rose. Quite spectacularly, casting brilliant crepuscular rays from the horizon and underside edges of clouds.

Throughout the sunrise, the light was spectacular – brightly illuminating colourful clouds.

Simple abstract patterns: bright early morning sunlight illuminating clouds a warm yellow/orange.

…and casting a subtle hazy glow over the morning fog across Little Assynt, outlines of hills receding into the mist

Perhaps my favourite image from the morning has to be Suilven, the unmistakable mountain on the horizon, catching a subtle patch of oblique sunlight on a flank.

The unmistakable shape of Suilven (Sùilebheinn) catching an oblique beam of warm early morning sunlight.

Once the sun rose, I explored the Falls of Kirkaig outside Inverkirkaig. A nice long walk through lumpy landscape, to a large thundering waterfall.

Returning to above Rhicarn, clouds had flowed in obscuring the mountains on the horizon, so I experimented flying the drone to admire the surrounding landscape.

There’s something about finding a thin strip of old tarmac that obviously used to be a road – it makes a connection with the story and heritage of a location. From researching on Pastmap, it appears there was not much road here at all throughout the 19th century – presumably a cattle drovers’ track or similar. Then the old tarmac was laid, following a circuitous path around the gneiss rock hills. Finally, some time after the 1960s, a new road, now the B869, was laid through it in a boring straight line, the old route relegated to a carpark yet visible and walkable either side of the road.

I suspect at one stage this might have been nothing more than a cattle drover’s track down to the lowlands, maybe up until the early 1900s; up to 1960 the road was just a thin narrow track of tarmac with a couple of moderately sharp twisty turns in. Since then the B869 has been rerouted into a simple and less inspiring straight line and the old road relegated to a path, some of it widened to form a carpark beside the new. The bedrock is mostly Scourian gneiss, metamorphic, formed 2500-4000 million years ago (and therefore amongst the oldest rock to be found on the planet); down the centre of this view is a line of Lewisian metagabbro, gneissose, also metamorphic, formed 541-4000 million years ago. I’m not sure what the large central depression might be – it looks rather like a quarry, although there’s no evidence of anything on the maps.

Behind this scene, on the way to Clachtoll, lies some beautiful Karst landscape (cnoc’n’lochan or knock-and-lochan), formed by underground erosion of softer rock, leading to a classic pattern of rocky knolls interspersed (almost 50-50 by area) with lochs.

Further along the road lies the Maiden Loch, of which I’ve been very fond since first catching sight of it years ago. That first view was on a sunny afternoon, the sky blue reflecting in the water. I flew the drone over it, to admire the gneiss landscape all the more…

Fantastic scenery: Assynt at its very best. A very windy moment flying the drone above one of my favourite lochs, the Maiden Loch near Clachtoll. The landscape is typical knock-and-lochan Karst formation: shaped by the dissolution of a layer or layers of soluble bedrock, small undulating gneiss hillocks emerge amongst the lochs. In the hazy distance, Suilven cuts its familiar outline on the far horizon.

Some of the above photos are available on my photo gallery website: ShinyPhoto: Assynt

Autumn at Glen Affric (1)

For about 13 years I have been of the opinion that it has not been a year without at least one trip to Glen Affric.

My favoured time is autumn, late October, to catch the trees in the Caledonian Forest reserve at their most colourful.

Arriving before sunrise, the light is all dull  and the scenery a moody shade of gloomy – the last vestiges of moon stars remaining in the cobalt blue sky.

One of my favourite scenes at Glen Affric – two ncie birch trees amongst purple and green heather.
Sadly this shot has been marred in recent years by the installation of a large wide path cutting right through the heather between bench and trees; this photo used to be easier to compose but now I’m too conscious of having to position the frame to avoid the path just below; it’s becoming too much of a trick-shot for my liking.

 

Slowly, over the course of an hour after the posted sunrise time, the sun will gradually rise behind Meall Dubh beyond Loch Beinn a Mheadhoinn, casting a beautiful light on the forest:

Having arrived so early, it is a delight to bask in the first proper warm sunlight of the day:

One of my favourite birches – always think it should be called “Dancer” for some reason – basking in the first warm rays of sunrise amongst the heather.

Around Glen Affric 3: Morning Sunrise

I first visited Glen Affric in September 2006, more or less 10 years ago. Not long after, I discovered the joy of standing at my favourite bench watching the sun rise behind the distant mountains, its light casting shadows of the trees on the mist. Since then I’ve been longing for a second chance at the same scene – and this year, with a bit of good timing, I think I managed it.

And another behind-the-scenes 360-pano selfie of what it’s like to be there…

[sphere 2868]

Around Glen Affric: water

I had a short holiday at the start of last November, a few days spent in Glen Affric. There are several aspects why it’s my favourite part of the planet, but for the purposes of this post, we consider the role of water in shaping a landscape, eroding its way through rocks to form river, gorges and waterfalls.

First, the impressive 150-foot drop of Plodda Falls from the top:

Second, some of the cascades in the River Affric, part of the way around the River Walk, rich autumn colours glowing in the morning sunlight:

And finally, a couple of 360-degree panoramas, partly to offer a behind-the-scenes view – they take a little while to download once clicked:

[sphere 2834]

[sphere 2836]

Glen Affric: Caledonian Forest

From wikipedia:

The Caledonian Forest is the name given to the former (ancient old-growth) temperate rainforest of Scotland. The  known extent of the Roman occupation suggests that it was north of the Clyde and west of the Tay.

The Scots pines of the Caledonian Forest are directly descended from the first pines to arrive in Scotland following the ice-age; arriving about 7,000 BC. The forest reached its maximum extent about 5,000 BC after which the Scottish climate became wetter and windier. This changed climate reduced the extent of the forest significantly by 2,000 BC. From that date, human actions (including the grazing effects of sheep and deer) reduced it to its current extent.

Today, that forest exist as 35 remnants covering about 180 square kilometres (44,000 acres). The Scots pines of these remnants are, by definition, directly descended from the first pines to arrive in Scotland following the ice-age. These remnants have adapted genetically to different Scottish environments, and as such, are globally unique; their ecological characteristics form an unbroken, 9,000-year chain of natural evolution with a distinct variety of soils, vegetation, and animals.

To a great extent the remnants survived on land that was either too steep, too rocky, or too remote to be agriculturally useful. The largest remnants are in Strathspey and Strath Dee on highly acidic freely drained glacial deposits that are of little value for cultivation and domestic stock.

It’s also amazingly beautiful. I can happily drag myself out of bed at 3am and drive several hours north to arrive at the forest in time to watch the sun rise: with its ancient history, the scent of the heather, watching mist flowing around the old pine tree-tops catching the morning light, there’s nowhere more gorgeous on Earth.

Around Kilchurn Castle

It seems a while ago now, but last September I spent a weekend trundling around Argyll. The light on the Saturday morning was absolutely beautiful – so I spent a happy couple of hours standing on the shores of Loch Awe admiring the sunlight and mist on Ben Cruachan and Kilchurn Castle, as one does.