ElQ bills itself as a wilderness
park, meaning that the portion of the station around the tourist facilities – a
few hundred thousand acres or so, I am guessing – is managed in its more or
less natural state. That means fewer
cows and more native flora and fauna, plus the horses for tourists and at least
one donkey (he bites, according to signs).
For our purposes, it meant that there are a variety of walking tracks to
try out. After reading the ElQ
descriptions, we decided on Champagne Springs – at Class 5, it seemed long
enough (six hours return) and challenging enough (lots of scrambling, little
shade) that it would appeal less to other guests. The springs at the end sounded like they were
worth the effort. You will notice a
congruent trend going forward in how Paul and I like to hike – with as few
other people as possible.
To expedite, we leave camp at dawn
and make a quick breakfast at the trailhead, all of a one kilometer drive. It’s already 23 C, and we get moving before
the flies come out. We transect up a
fault-controlled stream drainage, with a high ridge of quartzite to our
right. Some shade for a while, and lots of quartzite boulders to scramble
over. This is not a trail, it’s a route
with massive potential for dislocating or breaking a joint. The boulder patches seemed piled up as well;
maybe high discharge flood events. Not
something I want to see. Tiresome joy,
climbing up and down angular boulders.
Eventually the boulders thin out, as we move along a dip slope of
quartzite, the broken upper surfaces of a number of beds. Treacherous:
The ridge gets higher and pools appear.
The sun is well up, I suspect its well over 30 C, stimulating the flies. We come to the pools. They are pretty:
Alas the thermal pool in the
trail description hosts a layer of algae.
Ain’t going in that. We take
pictures, avoid the sun, and recover a bit.
Then time to retrace our route.
Eventually the truck. Too tired to think. Camp.
Stare into hot space. The carrots
at the end of this stick are hot showers and a meal at the ElQ Steakhouse
(arguably the best, if not the only restaurant in the Kimberley). Paul has been talking about since we started planning. Once clean, we divide up. Paul goes to the restaurant bar, I sit
outside at the Swinging Arm, the outdoor snack bar, and write this blog:
There is a herpetology lecture
going on in the background. ElQ sponsors
some good work, or at least the presenters sound like academics. They get tough questions from audience.
Dinner, well worth it. The staff all seem to be young women from far
away – our servers are from Peru and somewhere in the British Caribbean. I have noticed that all the visible staff
seem to be young good-looking and energetic.
The food they bring us is good.
Paul is happy with the cocktails.
Tuesday June 11 - we leave ElQ by way of Emma Gorge:
There are people, flies, and
dust.
OK, I should explain flies. The more subtropical you get in Australia,
the higher the fly density. There’s also
a control based on the abundance of cattle.
They are just part of being up here.
No bites, they just land on you in the tens to hundreds. Occasional attempts to enter the ears, nose
or eyes are annoying, as is the personal fly cloud as I walk. At least the flies are small, so when a
breeze comes up, they blow away. For a
while, till the downwind flies land. I’m
mostly indifferent to them, except when they are about in high numbers. I think Purnululu was the worst. Like the sun, they go away at night. To be replaced by the all-night mosquito
patrol. Actually the worst is when we
get in the truck; it takes a while to clear the fly swarm that comes in with
us. Opening the windows sucks them out
once we are moving, but this interferes with the AC. Yes, we have a modern Toyota, six speed, six speakers, Bluetooth, and
cupholders. I speculate that our actual
evolutionary function on this drive is to help mix the fly populations along
the Gibb.
Speaking of that, onto the real
road. Much of the drive to ElQ was
paved, but as we enter deeper into the heart of the Kimberley Plateau it gets
rougher. Today the road winds up and over the Pentecost Range (quartzite, what
a surprise) and onto the Plateau per se.
We pass Home Valley Station. The
Plateau hosts younger more flat-lying sedimentary rocks than to the east,
covered by what I’ll have to call savannah.
At least seven distinct combinations of acacia trees (ghost gum,
bloodwoods, salmon gums, paperbarks to name a few), boabs, broad leafy things,
and grasses ranging from wimpy ankle-high spinifex to head high stands. I don’t know what controls the transitions
between them, I assume microclimates, drainage, bedrock (thus soil), and
overgrazing are factors. I steal glimpses
at them as we drive along, but mostly have to watch the road to pick the best path
along the gravel, sand. Washboard, and potholes. Examples from the road:
Boabs are my FAVORITE.
Today is to drive. 280 or so kms to Drysdale River Station, to
stage for a further rougher drive and then hike at Mitchell River National
Park. Therein, Mitchell Falls is supposed
to be a “must see” for the Gibb.
We pause at Ellenbrae Station,
which has absolutely nailed its tourist niche; it’s a half day drive from the most
frequented Gibb camping stops, so they advertise homemade scones, jam, and
cream. Lots of people stop. We get diet Coke and souvenirs.
The Gibb is OK. We average 75-85 kph, avoiding the worst
washboard and sandy patches. There are
occasional trucks towing caravans to pass.
Eventually a turn north on the Kalumbru Road to Drysdale:
Paul begins to practice opening
gates. Drysdale is a real station
compound, a mix of traveler facilities and the ephemera of a working outfit. We find a site at the edge of
campground. Paul can’t drive the stakes
for his tent into the ground. I look; it
seems to be an aluminous pisolite, i.e., deeply weathered surface rock rich in
aluminum. Looks sub-ore grade. Right geography for this.
Flies. Hot.
We are too tired to think.
Eventually, we agree that a fixed wing-bus-hike-helicopter-bus-fixed
wing trip to Mitchell Falls, advertised at the station (it has an airstrip; all
the stations do) would be better than being beat to crap by the drive up there. The Weta test applies. We inquire.
Paul chats up the pilots. Alas, we
almost but don’t quite get the last two seats.
Psyche for drive tomorrow, then.
The sun sets:
Wednesday June 12 - I run in the morning (note logo on singlet):
Passed by and then run the last 8
minute mile with a triathlete from Melbourne.
I’ve noticed that my body is not adapted for the type of hiking we are
doing. I am unused to the lateral motion
and balance required. Strength and
endurance are no issue, but I feel slow.
Well, I get there and back.
Brekkie, and further north on the
Kalumbru Road: washboarded and sandy. 70
minutes. A turn onto the Mitchell River
NP road, which is supposed to be tougher.
It’s not worse but is narrower and windy. 90 minutes.
The flora gets denser – lots of endemic Mitchell Plateau fan palms:
Worse than it looks |
This is pretty much as real wilderness gets
in Australia. The map shows that we drive
past a “Laterite Conservation Area”. I
am unclear why laterite needs conservation, it’s a common rock. Maybe this means “future mine once we get the
Aboriginals to agree”.
Mitchell River park. 35 C, noonish, flies, dust. An end to wilderness. Airstrip.
Campground. Helicopter pads. The campground looks tight, so we decide to skip
it, do the hike to Mitchell Falls, and sleep somewhere else.
So another Grade 5 exposed track
over quartzite boulders and beds, supposedly 5 hours for 8.5 kms. The only trail map is an aerial photograph
with the route labelled on it. It seems
accurate, as I can tell where we are by the changes in vegetation. Heat, flies.
Not as tough as Champagne Springs (more sandy areas to trudge through,
fewer boulder patches). It seems hotter,
maybe that’s the sun. I dunno, hard to
think. The first stream we are supposed
to cross at Big Mertens Falls is mostly dry, although there is water in the gorge below:
OK, bonus, sign in the Mitchell River NP composting toilet |
We plow onwards to Mitchell
Falls. The Mitchell River is flowing but
seems lower than in the descriptions I read. We see clean helicopter people, so we must be
in the right place. I lose the trail
while looking at the rocks. Paul finds
it, and eventually we get to the Falls.
They are flowing, but less dramatically (and in less oversaturated
colors) than in most of the tourist brochures:
Knackered:
We find the best overlook and rest. I think I actually fall asleep, only to wake
when the pilots we met yesterday show up with their tour group. They seem very impressed to see us. Mitchell Falls is still pretty:
There are flies, it is hot, so we
hike back to the truck. I notice that my
running endurance kicks in on this return; my exhaustion plateaus and I
actually move faster, slightly revived. But too tired to think.
Truck. Escape from Mitchell River. We bounce back out the access road, and stop
to camp at the Munurru Campground, run by the Kalambru Aboriginal group. They have done a really good job, nicely
spaced sites (we take one at the periphery), new two-holer composting toilets. Likely financed by the $45 per capita fee to
use the Kalambru Road. Dinner,
sleep. Mosquitos.
Thursday June 13 – Dawn walkabout at Munurru, pretty by the King
Edward River:
Today is to drive again. We are tired, but it seems like a push to the
interesting areas further east is doable.
Back south, hello and goodbye to Drysdale, and onto the Gibb. Lunch at Mt. Barnett Roadhouse, diesel for
the truck. We head onwards. Over the Packhorse Range, past Over the Range
Tyre and Mechanical, a stop at Adcock Gorge: tired and underwhelmed:
Further. I listen to the truck as I drive. It’s complex, tires sound different on dirt
and gravel than on paved roads, with further variations on every combination of
loose sand, gravel, and rocks. I’m
twitchy about this, it’s hard to recognize when something is off. But then, something does sound weird. We stop.
The back left tire is fubar. At
least the wheel is fine. Bugger. Paul and I efficiently change it out, given
the dust, flies, and heat. What to
do. No spare. So another Plan B: back to Over the Ridge, a new
tire, further destinations depending on how long this takes.
I hate myself for a bit for loosing
a tire. No way to tell cause, it was some
unknowable combination of road surface, tire condition (this was an older tire)
and speed. I only had control over the
last of these, so I worry I was going too fast for conditions.
We drive gently back to Over the
Ridge. I immediately have a good feel
about the place. A half dozen handy
looking blokes sitting around a good looking shop, classic rock playlist on
loud, three well-maintained workbays, and LOTS of new tires. We get out to many handshakes and g’days,
whatcha need? Eventually Nev(ille) the
owner sorts himself out and says sure I can help you boys out. He quotes a price which essentially takes all
of our cash; the electronic payment system is down. Luckily Paul carried a lot. We meet Nev’s partner and six year old daughter. The latter is persuaded to show us Nev’s
photobook of life in the Kimberley – a decade of amazing pictures of floods,
heat, things that bite, and his life.
A new tire, in less than an
hour. So here’s my one regret of the
trip; I didn’t take pictures at Over the Range.
I think it felt like we were there on business, plus there was literally
a tour bus there for photo ops when we arrived.
Alas. The place was a true slice
of Aussie outback.
Late afternoon. Back to Mt. Barnett, which has a campground. It is pleasingly far off the Gibb, but unpleasingly
chockablock with other campers. We find
a spot towards one end. Too tired to
think.
You are truly blessed to have the energy, desire, knowledge, to explore that universe. We are so lucky to have access to your very descriptive blogs. Enjoy and stay safe and healthy to bring us more tales of these travels that most of us will never do.
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