Junction Cabin is a cosy place on a wet day as long as someone has lit a fire. The area around here has been used for camping as well at times, and I have heard people say it was the first place they took their young children for an overnight walk. The grassy areas around the hut are a little slopy, but you could certainly put a tent up. The hut has a water tank and table/benches inside. There is often a supply of firewood left here by the rangers/council.
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Sunday, 31 August 2008
Organ Pipes Walk, Mt Wellington - 30th August 2008
Thursday, 28 August 2008
Remarkable Cave
Most of the solid information I have found about Remarkable Cave comes from the work of David Leaman. This comes from his books The Rock Which Makes Tasmania (Review here) and Walk Into History In Southern Tasmania.
The cave was originally called “Remarkable” because of the way there appeared to be a map of Tasmania if you stood inside and looked through the cave at the right angle. You can see this clearly as you stand on the viewing platform.
Now, to make the cave more interesting, it has two entrances from the sea-end. Two separate caves have joined up. I recall walking through the cave many years ago. I think at that time access to the floor of the cave was less restricted. The viewing platform these days tends to discourage venturing further. I didn’t clamber down, as the sea was washing into the cave rear, and there was little point. However, when you can walk through the cave it is very interesting. I’m trying to find photos from all those years ago.
David Leaman’s view is that the cave is quite unremarkable (“run-of-the-mill”). He’s speaking as a geologist. His view is that the intrusion of the dolerite, the rocks it intruded, and the effects that intrusion has, is what makes the area remarkable. I suppose most tourists would disagree, but the rocks are very interesting. They can be seen clearly from a number of vantage points. I think there is also much to be seen inside the cave, so I’m keen to return when the tide is low enough.
In summary, Leaman says the following:
Most of the rocks here are Triassic sandstones. These were intruded by Jurassic dolerite. The intrusion can be seen clearly around Remarkable Cave. The top of the intrusion and its contact with the sandstone can be seen in the cliffs and shore platforms around the area.
The sandstone in contact with the dolerite as it intruded displays “exquisite and intense folding”. The easiest place to see this is from the lookout below the car-park, looking south to the cliff below. Leaman says that if you can walk through the cave, then there is more folding to be inspected. Dolerite of course forms many major nearby features; Mt Brown, Cape Raoul, Cape Pillar etc
The question is whether the folding occurred at the time of the intrusion, or when the rock was laid down. There is no firm answer. A previous doctoral thesis (Powell, 1967 - Studies in the geometry of folding and its mechanical interpretation) had suggested that the folding was caused by the heating of the rock with hot liquids and gasses related to the intrusion. Leaman thinks this is unlikely, and that the sandstones were folded soon after they were deposited, when they were poorly compacted. They were then overlaid by more sandstones, and then later intruded by the dolerite. The dolerite intrusion has altered (metamorphosed) the sandstone by heat. Leaman notes that the distorted sandstones are also intruded and cut by the dolerite suggesting that the folding existed before the intrusion of the dolerite.
Interesting place anyway.
Sunday, 24 August 2008
Freycinet Peninsula - 21st-23rd August 2008
Friday was mainly spent climbing Mt Freycinet. The actual Peninsula Circuit walk involves walking south along the west coast to Cooks Beach, and then returning via the heights of Mt Freycinet's flanks and Mt Graham. I did this last time, but this time I avoided the carry of a full pack up the nearly 600m climb to Mt Graham, and made Mt Freycinet a morning's walk with just a daypack. Mt Freycinet is the high point of the area at 620m. Snow was forecast down to 500m the night before I think, and, true, I found snow on top of Mt Freycinet. I presume this is not very common, although I did read the warning in the walk registration shelter that walkers should remember to take warm clothing as snow did fall there at times. I suppose it's unusual to think of snow on Tasmania's east coast in such a maritime location. I have to admit that the total area of snow I found still protected from the sun by rock shadows was probably less than a square metre. Flowing water was available in several creeks along the track to Mt Freycinet inlcuding quite high up.
The views from Mt Freycinet and Mt Graham of the peninsula, Wineglass Bay, The Hazards and Schouten Island are very good. Of course you can also see quite a lot of Tasmania's east coast. Mt Freycinet is the mountain the runners have to climb when the Three Peaks Race visits Coles Bay, and I have to say I admire people who can run up and down this peak, from Coles Bay, especially if they have to do it in the dark. In the afternoon I visited Bryans Beach for a short while, which looks south to Schouten Island. Bryans, which faces southwest, is often rougher than Cooks Beach, which faces east and northeast. However, when I visited it was very calm. I cut short the visit in order to get back to Cooks for sunset on the Hazards, which turned out to be well worthwhile.
Walked out by the low level route on Saturday, stopping to watch Southern Right Whales (Eubalaena australis) (See here for the best info on Right Whales that I can find so far) lazing around in Wineglass Bay. It was hard to tell how many there were from the shore, but inspection of the photos on return home revealed three in at least one shot - I suspect this is a mother, a smallish calf and maybe another older calf. I don't think father-whales hang around with the family, but I must read up on them a bit more. They were attracting attention from walkers, but it was interesting to see people gawping about the bay without noticing these very large creatures moving about only a couple of hundred metres away. I recall sitting in Wineglass Bay, on the granite near the track-end, on a Geology excursion some few years ago. The teacher was banging on about pink and grey granites while behind him a whale played in the bay. In the end he had to sit down and shut up until the whale got tired and moved on, when the class were able to direct some attention to how The Hazards formed.
Wednesday, 20 August 2008
Crescent Bay and Mount Brown - 19th August 2008
The Maingon Blowhole has a serious warning sign ("anything that happens is your own fault" -type of sign) just before you get to it, and I think it's justified. It's a narrow slit in the earth, which drops some rather large distance into a heaving sliver of white water. The edges are sloping, crumbly, grassy and slippery, and a fall would undoubtedly be fatal. Well worth a look! I'm not sure if it actually "blows" in a heavy sea. I haven't been there before, having done this walk from the opposite direction in years past. Just beyond here, the rocky shore could be explored at length if time and sea conditions allowed.
The track then passes Mount Brown, a large dolerite protuberance, and a rough cairned track heads steeply up the hill. The views from the top are great; Crescent Bay, Port Arthur, Cape Pillar, Tasman Island and Cape Raoul make a dramatic 360 degree vista. Particularly spectacular is the view from the high western end of the hilltop, which is basically a 170m cliff. There are great views from here down onto Dauntless Point, which has its own dramatic and interestingly fractured cliff. I can say the dolerite on this headland is particularly gritty and sharp, having personally tested it with hands and knees when a rock shifted beneath me.
Descending Mount Brown, the track then heads down to Crescent Bay, which is a beautiful beach with high dunes. At the far end of Crescent Bay is Standup Point, which has its own blowholes. I only made it to the first one (apparently smaller) before my turn-around time arrived, enabling me to be taxi in Hobart later in the afternoon. Apparently these blowholes do blow spectacularly in heavy seas when I assume they become more difficult and/or dangerous to access. The amount of time that could be spent taking in the views and investigating the various sights along the way took me by surprise, and I found I ran out of time, which probably requires a return trip (Phil).
I found three Hooded Plovers on the beach, and a gaggle of angry and noisy Yellow-Tailed Black Cockatoos in the dunes. None of them were very pleased to see me. I'm assuming the plover with the blotchy head markings is actually a juvenile, perhaps hatched last spring.
Monday, 18 August 2008
Mt Wellington - 18th August 2008
I walked up the ZigZag Track, and had some trouble on sections of it. The snow was mostly quite firm, but the usefully hard crust also made it difficult on the steepest section. The ZigZag isn't too bad, but there are sections where if you went sideways off it you'd slide a fair way before fetching up against a rock or a tree.
I hoped to have the summit to myself, but the snow ploughing crew were there. The little snow plough is quite interesting to watch, although they did rather shatter the silence. The design of the actual ploughing implement is intriguing, but obviously effective. I asked them to keep the road closed for a while so I could walk down it without having to look out for cars. They managed to do so.
The return was easier, as I avoided the ZigZag and used the road and other tracks to return easily around the north and east sides of the mountain. A couple of others who had climbed the ZigZag decided this was the best policy too. I think crampons would have helped in a descent (or an ascent for that matter). The snow is really quite deep in places, and reminds me of years past. I don't think I've seen this much snow on Mt Wellington for a long time. I recall a good fall when my eldest was about 12 months old (1994), and then some really deep snow in the 1970s, when the road was cut between 2-3m banks of snow. With more snow forecast, it looks like it will continue for a while. The amount of snow that is there now will take a while to melt even without further falls.
A pair of Wedge-Tailed Eagles passed across the front of the mountain as I walked down. I was accompanied at this point by Ray, who told me that there are two pairs of eagles who frequent the mountain at present. The only photo I could manage at the distance was unfortunately not worth the the inconvenience I caused the electrons with which it was recorded. I will refrain from troubling any more electrons, or your eyeballs. This is the northerly view to Mt Hull, Mt Faulkner, Mt Dromedary and Platform Peak, upon the last two of which it appeared to be precipitating in direct contravention of the BoM's instructions for the day!
Sunday, 17 August 2008
Chimney Pot Hill - 16th August 2008
Leaving the top, there are a range of options, and you can explore the tracks as time and your desire for hill climbs dictate. On days with dodgy weather, these tracks offer some good views without quite the altitude of the upper slopes of Mt Wellington. The forest is very open and attractive, and there are good views through the trees at many points.
As an aside, the nearby native plant nursery (Plants of Tasmania Nursery, 65 Hall St Ridgeway) has a great range of Tasmanian plants often seen only in their natural habitat, and is worth a look.
Saturday, 16 August 2008
Fungi from the South Cape Bay Track
South Cape Bay - 15th August 2008
The beach had some foam sitting on it, so the surf has been quite wild, but nothing like it was on a visit in 2005 following a full storm.
It's interesting to see the high-tide mark of pulverised plastic fragments along this beach. Most of the junk they came from appears to come from fishing boats. There's quite a collection of fishing junk along the track as it climbs onto the cliffs.
There was a single Hooded Plover (Thinornis rubricollis) wandering the beach yesterday. You normally see two together here, if you see them at all. They are always wary of people, but you can often get close to them by just sitting and waiting for them to wander closer. This one was very wary, and I didn't want to upset him. Obviously for photographing birds this size, I need a new camera with a much bigger lens! It was very difficult to capture a decent shot of this little bird, with my camera and lens, especially given the speed at which he darted about the beach. This one will do, but I'm not happy with it.
All in all it was quite a nice day, if persistently chilly. I'll finish with this shot of a rainbow and South East Cape.
Thursday, 14 August 2008
South Arm - 13th August 2008
The surf was impressively large yesterday, with the waves breaking along much of the length of the beach all at once.
This fish had been thrown up by the waves. As I was looking it up in the fish book, the kids told me it was a Cowfish. They know, apparently, because they've all been to the Woodbridge Marine Discovery Centre. See, an education is useful! I was thinking some sort of Toadfish, but the kids were right, and they're related in the order Tetraodontiformidae. Like toadfish, these are also poisonous. My book suggests it's a female Shaw's Cowfish, Aracana aurita.
Hope Beach cops a pounding from the swells that come into Storm Bay. The sand on the beach is always quite soft and hard to walk on. The beach also slopes quite steeply along much of its length. This photo taken last year shows this. At times, and in places, the waves wash right up to the dunes on a steep slope, or create a large berm hard by the dunes, against which they wash at high tide. Not a good beach for a casual swim, and you need to be careful in places. The whole of the South Arm Neck is apparently the result of a the original 200-metre deep Derwent River gorge being gradually filled in with clay, sand and gravel. (Ref. David Leaman 1999, Walk Into History In Southern Tasmania)
On the inside of the neck is quiet Ralphs Bay. This place seems to be the Hobart garbage filter, where the bottles and plastic bags end up. This tree was liberally festooned with crap.
This Eagle Ray, Myliobatis australis, was dead on the beach. Probably ate some of the garbage!
Calverts Beach is on the eastern side of Goats Bluff, and provided some spectacular viewing in the large surf yesterday. Behind this beach is Calverts Lagoon, considered to be an important wetland area. The lagoon does appear to be quite dry when viewed from the road at present. Information about it can be found by searching at this site.
Tuesday, 12 August 2008
Cape Hauy - 11th August 2008
The Cape Hauy walk is very worthwhile, with the scenery and surrounds quite spectacular. The walk undulates a little, and the need for climbs and descents can surprise the unwary given the proximity to the sea. Fortescue Bay itself is a lovely place, obviously very well used - this is a favourite fishing and camping spot for many - but quite well maintained and managed. The drive in however has gradually become more and more a showcase for Tasmanian forestry operations, with vast swathes of forest demolished within clear sight of the road. The old track to Cape Pillar has been re-routed due to forestry operations across its old route. The National Park also shows the effects of fire escapes, both here and on the Forestier Peninsula. The track itself is quite liberally strewn with the debris from fallen trees, burnt a few years ago. If this is to become an iconic walk, I can see a bit of effort is going to be required to make the track more usable. However, over recent years, some useful lengths of planking have been placed across the plateau to mitigate the worst of the erosion we were causing, and reduce the dampness underfoot.
Once you descend onto the peninsula of Cape Hauy, the views to north and south open up quite dramatically. To the south, Cape Pillar makes a fine sight, with The Blade and Tasman Island visible. To the north, the coastline of the Tasman and Forestier Peninsulas, Cape Bernier, Maria Island and Freycinet are visible. On a clear day you may be able to see further than that. The track emerges at the end onto a small rock platform with a sheer 100m+ drop into the sea. Great care is required (especially if here with children), but this is the best spot for stopping and taking in the views and having lunch. Cape Hauy is home to the Candlestick and Totem Pole, both of great interest to climbers. They make spectacular viewing.
The Candlestick stands next to the end of the Cape clearly visible just next to the lunch spot, and behind it are The Lanterns. The Candlestick is a very tall and thin sea stack, separated from the Cape and the Lanterns by the sea. Lots of information here about climbing these things. As their guide says, the crux of the climb up the Candlestick is the SWIM! You can scramble down the less steep side of the Cape towards the sea, and actually you can get within a few metres of the sea if you keep going. This requires great care in places, and of course you have to climb back up the 100m of height. It does however afford better views of the Candlestick and Totem Pole, and these start only a short way down. My perambulations yesterday had to be curtailed because I took a sidetrip to the Tesselated Pavement on the drive in and left myself rather short of time.
Next to the Candlestick stands the Totem Pole. The climbing guide says this about the Totem Pole: "It is over sixty metres tall, but only about four metres wide at the base. It sways in the wind and shudders with the crash of every wave." Go here for some more dramatic photos of the Totem Pole.
A final detour on the return is well worthwhile to the Monument Lookout. This stands on top of a vertical 150m drop to the sea, and requires great care, as the rocks are rounded and sloping, with good sized cracks between them. Views from here are to the rock stacks off Cape Hauy and Cape Pillar, and in fact very dramatically straight downwards to the surface of the sea. Great place to sit on a nice day.