The BOM site was going
crazy late last week about the impending winter storm conditions that were
going to sweep, Assyrian – wolf like, down on the southeast. Snow! Wind! Cold!
Rain! End of CAWKI*! A big system pushing north from Antarctica. Snow down to 700
m, at any rate. Beauty, I think, a chance to get out and do some walking in the
cold, possibly see some snow, feel buzzing finger tips and ears, eat something
great in front of a roaring fire, with a glass of red.
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A big system coming up from Antarctica. BOM image |
Sunday sees me on a
Blue Mountains bound train before dawn. It IS cold, on the walk from home to
Central, but lovely in the carriage, as we head through dark suburbs to the
inaptly-named Emu Plains. Well — have YOU ever seen an emu thereabouts?
About Warrimoo, the
very first sun cuts the dark, a pale pink, nacreous glow; a huge ball of orange
soon follows. It is exquisitely, heart-stoppingly beautiful, as I see it
through darkened trees, and suggests that, at least to the east, the sky is
unclouded. If we are going to see some snow, that system coming in from the
west needs to make good time.
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Warrimoo sunrise |
It is just after eight when I leave the train at
Blackheath, elevation 1070 m. Crisp, but no snow. Rime and frost on the grass
near the railway station, and I am off searching for a hot cup of tea and some
breakfast.
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Civic information, Blackheath |
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Area of Operations, west of the railway and town ridge |
I get walking, and
head southwest out of town along empty streets, to the Centennial Glen car
park. The sign gnomes near there have a dim view of walking speed. 1.5 km in 40
minutes? Along a sealed road? Even I
can walk faster than that.
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1.5 km in 40 minutes? |
From the car park, the track winds west though low
heath, which really is being blasted today, buffeted by a roaring gale from the
west. The track runs along the spectacular cliff top, then takes a dive like an
Italian soccer player; all ladders and cut steps, down the cliff line through a
deep gully. In places spray from the creek flies up in drifts onto the ladder
ways. I walk quickly through those, not wanting to start the day wet. In
summer, this would be a lot of fun! Today, it will just be annoying, at best.
The track levels off
and follows the base of the cliff line along Colliers Causeway. It is
reasonably wide and even in some places, rough and narrow elsewhere.
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The wide path ... |
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... and the narrow |
It is
generally fairly easy walking. In places, there is some track improvement going on,
with masonry works in progress, building retaining walls and easy paths.
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Track upgrades |
The
path is usually right at the very base of the cliff — I can touch sandstone
faces with my right hand all along here. The cliffed landscape is the defining,
iconic feature of Blue Mountains.
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Typical cliffed landscape of the Blue Mountains. Banks Wall Sandstone forms the cliffs in the western Blue Mountains, as here on the Blackheath ridge. |
The western edge of the Blue Mountains is
transitional land. Cliff-bound hills covered with nearly continuous eucalypt
forest, give way westward to a more rolling terrain of open grassland, with
patches of forest, usually forming the higher ground. And so it is, as well,
with the original inhabitants. The western Blue Mountains, the Megalong and
Burragorang valleys, is the home of the Gundungurra people, which continues
south into the Southern Highlands. To the west is Wiradjuri land, home of the goanna
people, dwellers of the grasslands of the Central West.
As always, geology is
at the bottom of it. The cliffs in the western Blue Mountains are formed from my
old acquaintance — Triassic-aged Banks Walls Sandstone, part of the Narrabeen
Group in the Permo-Triassic (300 – 200 million years ago) Sydney Basin. Further
east, down the mountains, beginning about Woodford, the cliffs are built of younger
Hawkesbury Sandstone, which crops out so well around Sydney itself. Cliffs form
when a resistant layer is underlain by a more easily-eroded rock layer. The
soft rock erodes back more quickly, making an overhang; the overlying rock
collapses, forming cliffs.
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Overhang cave and cliff |
Over time, the process continues and the cliff line
retreats. In the Blue Mountains the rock layers are nearly flat-lying, so the
cliffs can continue, essentially unbroken, along ridge lines for many kilometres.
If you stand at vantage points like Govetts Leap in Blackheath, you see the
cliffs extending, in spectacular fashion, all the way down the Grose Valley.
The rock overhangs must have been magnets for Aboriginal occupation over millennia.
They offer shelter, and water from seeps, dripping roofs and cascading streams.
Further east, near Wentworth Falls, an occupation site has been dated at 20,000
years old, or possibly older. The tribes have walked these hills for a long,
long time.
To the west Sydney
Basin gives way to the underlying, older rocks of the Lachlan Fold Belt. These can
be highly variable over short distances, compared to the regular, continuous
geology of the Sydney Basin. Their variability give rise to the diverse range
of landscapes, soil, and vegetation of the Central Tablelands and the Central
West regions. Granites are often deeply eroded to soft, rolling landscapes with
deep, relatively fertile soils that can sustain grasslands — such as the area
around Bathurst. Stronger, more resistant rocks — often metamorphosed sandstone
and mudstone, give rise to hilly county with shallow, stony soils that support
forest, such as the prominent chains of hills — Mount Lambie, Dark Corner, the
Catombal Range, the Hervey and Coccaparra Ranges.
And so, as I walk at
the base of the cliff, I can look west across this geological, topographic,
ecological, anthropological divide. I am looking through the forest, from Gundungurra
land, to the more open grasslands of Wiradjuri country.
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Looking through the trees, from Gundungurra, towards Wiradjuri country |
Nestled in the valley,
right at the bottom of the hill, is a white farm house and outbuildings, in an opening between the trees I can see a house which is the closest to
the cliff line. I think of this as The First Farm.
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The First Farm |
The bush is mainly the
olive drab, grey green of eucalyptus forest, but in the deep gullies, where the
sun doesn’t penetrate easily, the vegetation changes to dense, multi-green
temperate rainforest, fed by the constant spray from waterfalls.
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By channels of coolness the echoes are calling,
And down the dim gorges I hear the creek falling. |
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Temperate rain forest in the tight gullies |
Scattered
through the bush at this time of year, are splotches of beautiful lemon-yellow
wattle — always the first to flower.
Even in the middle of winter, the wattles
have got their hurry on, when other plants won’t start to flower until spring
starts to warm them up. As well, there is a pretty, but tiny, pink
trumpet-shaped flower. It’s pretty. It’s pink. It’s shaped like a trumpet.
That
exhausts my knowledge on this plant. I’m better with rocks.
And, in the way of
Blue Mountains bushwalks, at the end of the day you repeat the climbing, in
reverse. Back up through the cliff line on ladder pitches, to win to the
plateau again. At the top of the climb up Porters Pass, there is a lookout,
with views again out to the west, over the mix of bush and pasture. This time,
the wind is howling, fiercer than before, and a lot of cloud is inbound. I take
a short time to enjoy the view, and celebrate my return to the top by supping a
wee dram.
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Cheers! |
In this cold and wind, the whiskey is most welcome. It burns and
warms on the way down. I think of the characters in Tim Winton’s “The Riders” —
the father and the neighbour — who spent a lot of time standing in an Irish
bog, taking a spot of drink against the cold. I don’t think I’ve ever drunk
whiskey like this before — outdoors, in the whistling wind and with my fingers
freezing. It’s a wonderful moment. The drinking and looking and general huzzah is
cut short by the wind, which is screaming always more loud. As I take a
picture, light flurries of snow arrive, and this makes my day. Snow, at last.
It’s not settling, but, by God! I came to see snow, and here it is!
But the wind doesn't
die, and I can feel my legs stiffening. I walk on, staying warm by keeping moving.
It’s a short walk through the streets of 1930s holiday cottages, back to the
railway station. Where a transformation has been wrought in my absence. The
early morning Blackheath was empty of people, bar a few hardy (mad?) souls like
me. Now, it is teeming with rubberneckers. It seems that tout Sydney and the mountains has ascended on Blackheath to witness
the impending meteorological onslaught. Wintergeddon. The streets seem crowded
but the indoors are even worse. The cafes are full to bursting; both pubs have
queues as long as a mother-in-law’s memory, waiting to order counter lunches.
My dream of a delicious and hearty feed in a quiet café is disappearing, fast. Eventually,
I eat an indifferent steak sandwich in a crowded café. But it DOES have a
roaring fire, and I am seated right next to it. I am looking out at more snow
flurries, although they melt on hitting the ground.
On the way down the hill, there is a serendipitous moment. Near Warrimoo, where I saw the sunrise, the train runs through a short section, where a gap in the trees aligns with a gap in the hills. Far, far out to the east, on the coastal plain, I can see the skyscrapers of Sydney, 60 km away. A shaft of sun drops on the city, through a hole in the clouds, and it is beautiful, glowing, crystalline, in the way it is lit up. It looks like Dick Whittington's London, Dorothy's Oz, beckoning me on.
This is pretty damn good, after a stiff walk. Warming up, enjoying a sit. Nodding off on the train home, whilst savouring chocolate and a surreptitious nip of whiskey. I drowse off. Simple delights on an afternoon after a stiff walk in the cold. Snow. Just a bit, but good enough.
* CAWKI: Civilisation As We Know It