My Favourite Rocks Pt. 2

Blowin’ In The Wind

(click above..you won’t be sorry)

One of my bestest favouritest rocks is a ventifact (pictured below). It sat on my office desk in downtown Vancouver for the last 4 years and was terribly neglected during lock down, so I brought it home last week to make it feel loved again. It now sits under my computer screen next to a 1kg cube of tungsten metal and a small brass cock. (As an aside, the tungsten cube is unbelievably dense – the same specific gravity as gold at about 19.2).

It’s the size of a small brass cock.

Ventifacts are naturally polished rocks that have been shaped by wind-blown sand or ice, typically in desert environments -a process known as as “corrasion“; a new technical word for me, which just goes to show you’re never too dumb or too old to learn. They’re found in deserts all over the world from Antarctica to Egypt and have even been recognised on Mars where they’re suspected to have damaged a wheel on NASA’s Curiosity Rover. The term -which loosely translated from the Latin means something made by the wind- first appears in the literature around 1911; a British geologist coined it to describe wind-shaped rocks he saw in Africa and parts of Asia.

Ouch. Who left that bloody lego ventifact there?
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My Favourite Rocks Pt 1

A Surfeit of Sulphides

I was fondling my rocks the other night -something I do often- gently touching them, stroking each one, talking to them like the fine old friends they are. My collection is growing, so mid Covid I bought some rickety, white Ikea Billy shelving to show off the best pieces in my home office, where nobody can see them but me. Mid-caress, my eyes were drawn to the 3 sulphide specimens perched on the top shelf which has begun to sag worryingly under the weight of sexy, coloured rocks.

Billy is groaning.

They’re 3 of my favourite samples: very different visually but closely related chemically. There’s some eye candy pyrite from Huanzala in Peru, a particular favourite; a wonderful chunk of arsenopyrite from Kosovo, and some meaty looking yellow-orange orpiment I collected in Iran. They represent points on a chemical spectrum with iron sulphide at one end, iron-arsenic sulphide in the middle and pure arsenic sulphide at the other end. Pyrite has cubic crystal structure, and orpiment and arsenopyrite are both monoclinic – an off-kilter matchbox shape.

At this point, the mineralogists out there will nerdily tell me that it isn’t that simple you idiot, and they’re right – there’s all sorts of pressure/temperature/chemical considerations that influence which mineral forms and when- but I like to think of them as a simple spectrum.

Continue reading “My Favourite Rocks Pt 1”