The cliffs of lunacy

Decades ago Simone Weil predicted that ‘‘We will see throughout the country the most incredible absurdities—and they will appear natural.’ She was right on any number of fronts. One of the most incredible is car advertisements on TV and online. Readers will remember that in 2019 FOBIF launched a complaint to the Ad Standards Bureau over a Suzuki commercial promoting reckless  and destructive driving: the ad actually suggested that responsible driving is boring, and driving around in circles was great fun. Our complaint was found to be partly justified, and the advertiser agreed to modify the ad…though we couldn’t see it made any difference.

In any case, the lunatic promotion of very silly behaviour continues. An avalanche of commercials for SUVs urges TV audiences to plough through creeks, churn up sand dunes, kick up dirt and disfigure beaches. A lot of this behaviour is actually dangerous, but presumably it appeals to the fantasies of those drivers who see it as an enhancement of their self image.

Our nomination for the silliest current commercial goes to Mitsubishi Outlander, whose effort culminates in the following image of a family ‘enjoying’ the outdoors:

 

Have a close look at where the car is:

We’re not sure how the happy family is going to get their picnic out of the boot. Maybe that’ll be in the sequel?

Does all this matter? Is anyone going to be stupid enough to park inches from a cliff edge? Probably not. But a significant percentage of people subjected to this barrage of propaganda will engage in bad practices. Have a look at this:

Castlemaine Diggings NHP, February 2022: some drivers have been persuaded that the only way to have fun is to gouge a bit of the bush. Our photo doesn’t really capture the destructive results of this hooning.

FOBIF has tilted at this particular windmill before, with mixed results. Should we try again? Mmmm…

Next in this infinite series: Flying, gouging, churning and splashing with Nissan Navara.

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Grevillea: check out a local speciality

Malmsbury Landcare and the Threatened Species conservancy have devised a project to map the distribution of our local rare Grevillea species, Grevillea obtecta – the Fryerstown Grevillea. The project uses a mobile phone app to capture and save data whenever a user locates and reports a population of this threatened species.

The app will be launched with an awareness and training session at Lauriston on Saturday March 12 at 1.30 pm. Participants will be shown how to download and use the app and there will be a field trip into nearby Lauriston forest reserve and the Fryers Forest to see some plants.

Fryerstown Grevillea is generally found in the Fryers Ranges from around Taradale south west to the Porcupine Ridge area. The Lauriston population is an isolated and unusual form. The plant flowers from around mid-October to mid-November but is easily recognised by its unusual leaves at any time of the year.

The project will help build up knowledge of this rare plant—one of ours!

The session is free, but you need to register: click here for details. The precise venue is still to be announced. Click on the image below to see full version.

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‘Nature in time’ show starts Saturday

Antechinus. Photo: Patrick Kavanagh

The ‘Nature in time: images from Central Victoria‘ show at the Newstead Arts Hub is starting this Saturday, 5 March, 10am – 5 pm. The opening event will take place on Sunday, 10.30, 6 March. There will be refreshments and everyone is welcome.  The exhibition will be open all weekends in the month as well as Labour Day, Monday 14 March.

You can find out more on this website and the Newstead Arts Hub website. For enquiries ring Bronwyn Silver 0448751111.

Aboriginal rock wells, Eureka Reef. Photo: Bronwyn Silver

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Take a closer look!

Night sky, Tarrengower. Photo Patrick Kavanagh

The Newstead Arts Hub is hosting a photographic exhibition, ‘Nature in time: images from Central Victoria‘, in March. The exhibition starts on the 5 March and will be open all weekends in the month as well as Labour Day, Monday 14 March.

The formal opening will be on 6 March at 10.30 am. All are welcome and refreshments will be provided.
 
The photographers are Patrick Kavanagh, Bronwyn Silver, Bernard Slattery and David Tatnall. 

You can find out more about the Newstead Arts Hub, the exhibition and the photographers here.

Salters Creek flume. Photo Bernard Slattery

Ironbarks. Photo David Tatnall

Barn Owl. Photo Patrick Kavanagh

Dog Rocks, Leanganook. Photo Bronwyn Silver

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Mind-boggling force, rocks that bend

Some people think the world is a messed-up place. I prefer to stay optimistic but, I have to admit, when it comes to the rocks beneath our feet, it’s a pretty accurate view.

These anticlines are just a selection of the crumpled rock strata that make up Castlemaine’s foundations. At least twenty anticlines lie between Castlemaine and Golden Point Road and some have been traced downwards by diamond drilling for at least 500 metres. Anticlines, and their companion synclines, are everywhere.

The strata that wrap around these beautiful folds were originally laid down on the deep ocean floor. Back then, some 440 million years ago, mind-bogglingly powerful tectonic forces were messing with eastern Australia by deforming the strata then raising them to form land. It started with a tectonic plate pushing from the east creating folds that run in a north-south direction. Try this with a sheet of paper: anchor one end and push the other towards it and you will see a fold forming at right angles. Most Castlemaine anticlines have sharp, narrow hinges like ‘The Anticlinal Fold’ (Photo 1) in Lyttleton Street but some can be quite broad, especially if there are a lot of thick sandstone beds in the area (Photo 2).

Photo 1: The Anticlinal Fold is fantastic because it shows so clearly the way sandstone layers are bent. Of course, they would have been quite plastic at the time of folding.

Photo 2: Broad anticline south side of Forest Creek near the Leanganook Track. Just north of Montgomery Street.

A lesser-known anticline is on the Kalimna Tourist Road (Photo 3) and a forgotten one is in Bull Street (Photo 4).

Photo 3: This anticline on the Kalimna Tourist Road is about 700 metres north of the top end of Lyttleton Street. It’s best to look at it from the north side.

Photo 4: A very nice anticline on the south side of Bull Street about 70 m east of Kennedy Street – it was once a quarry and now is a Council depot. Memoir 2, Geological Survey of Victoria 1903.

This is the sixth post in our geology series written by Clive Willman. 

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Cootamundra: it looks great, but it’s getting to be a menace

Cootamundra wattles: they’re all over the place. The species is native to a small area of NSW around Cootamundra, but has been planted widely in Victoria. It’s become a bit of a weed, and is capable of suffocating areas of bushland where it becomes dominant. Not only that, but it’s a menace in other respects, too. A new leaflet produced by local plant specialist Margaret Panter argues that it actually harms local wattles by interbreeding with them. The leaflet is below. To get a clearer look, click on it:

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Looking down into the distant past

Geology creeps into everyday life in the sneakiest ways. Take Castlemaine’s gutters and buildings; they exhibit a gallery of local rocks. At Stonemans Bookroom corner, deep gutters are paved with sandstone blocks and a dash of Harcourt granite along the road edge (Photo 1). By adding a sprinkling of basalt around the corner we have three rocks representing the key events in our region’s geological history; sandstone from a vast and ancient ocean floor, a later intrusion of granite (granodiorite to be technical) and lava flows from almost yesterday.

Photo 1: Gutter outside Stonemans Book Room with local sandstone on the inner edge and Harcourt Granodiorite forming the main gutter.

Posting a letter at the Post Office alcove in Lyttleton St gives a glimpse into two successive local metamorphic events (Photo 2). Look down at the magnificent slate flagstones that pave the Lyttleton Street alcove (also the Market building steps). They began as mudstone on the seafloor and later were weakly metamorphosed by heat and pressure, which converted clays to mica minerals. But it took a second dose of heat from the Harcourt granite to finish the job and harden the slate. Everything around the granite was baked hard so that the only decent and durable paving slate is found within 1.3km of its perimeter.

Photo 2: Slate paving in the Post Office alcove. The inset magnifier shows the typical spotted appearance of slates baked by the Harcourt granite. Note the granite has been used as a foundation stone which is common to other major Castlemaine buildings.

In the mid 19th century sandstone quarries were dotted all around the town. The Telegraph Station in Barkers Street, like many of our earliest buildings, is built of local sandstone (Photo 3). It has a beautiful warm colour with fascinating textures derived from its seafloor origins but the rock can become flaky where the clay content is high.

Photo 3: Castlemaine sandstone in the old Telegraph Station, Barkers Street.

This is the fifth post in our geology series written by Clive Willman. 

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2022 walks program

The 2022 FOBIF walks program is now on the website. The first walk is on Sunday 20 March. All walks start at the Community House in Templeton Street at 9.30am apart from the July 17 Long Walk led by Jeremy Holland which will start at 9am. All members and supporters are welcome.

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2022 FOBIF memberships due

Our annual newsletter with this year’s walks program and the 2022 membership renewal form has been sent to Friends of the Box-Ironbark members. For those who don’t receive this in the mail or new members, there is a 2022 renewal/join form here

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New Year fireworks 110,000 BC: Lalgambook!

Mt Franklin, or Lalgambook, is a volcanic scoria cone with a wonderfully preserved crater. Lalgambook was once thought to be 470,000 years old but a more accurate and surprising date was published in 2013; it turns out to be amongst the youngest volcanoes in central Victoria – a mere 110,000 years old. This is probably way too old to have been witnessed by first nation people, but they certainly witnessed eruptions in western Victoria as evidenced by the Bushfield stone axe, found buried by volcanic ash dated at about 34,000 years old.

Lalgambook would have started with a powerful and impressive display. Deposits along the north flank shows that the initial eruption was highly explosive with fragments of sandstone bedrock ripped up and mixed with scoria. This first unpredictable stage soon transitioned to a steady eruption of gas, ash and scoria fragments. The ash and scoria were thrown high into the air and quickly built the cone – scoria fragments called bombs, now seen along the entrance road, were welded together as they hit the ground. Some of the finer material would have formed an ash cloud that spread eastwards carried by the prevailing winds.

Welded scoria fragments (bombs) of all sizes can be seen along the entrance road to the Mt Franklin picnic area.

Mt Franklin was the largest volcano but several smaller eruption points are closely scattered around the mount. Lady Franklin is on the western flank of Lalgambook and an even smaller cone can be seen on the northeast side. Lalgambook would have been a mighty New Year fireworks display.

Mt Franklin is the tree covered scoria cone and Lady Franklin is the bare cone to the right.

This is the fourth post in our geology series written by Clive Willman. 

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