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Friday, 17 January 2014

THE HARTLEY GRANITE, BLUE MOUNTAINS NSW AUSTRALIA



From 1875 Heritage Map
At Mt Victoria the Great Western Highway leaves the level of the Blue Mountains plateau and descends into the valley below via the Victoria Pass. From top to bottom you can see the sedimentary layers of the Sydney Basin, first the Narrabeen Group (Triassic) and then the Illawarra Coal Measures and Shoalhaven Group (Permian). Once the valley floor has been reached, cuttings reveal further Sydney Basin sediments before the road begins to descend again towards Hartley.

Granite outcrops McKane's Falls road
It is at this point that the first granite outcrops may be seen and it is noteworthy that the elevation of the first granite is similar all over the northern part of the Hartley Valley and adjoining areas. This is because the Sydney Basin sediments here are resting on an old land surface mostly made of granite which was itself formed as an intrusion (in the Lower Carboniferous period) into older Devonian and Silurian sediments. See the blog entry on the Unconformity at South Bowenfels here for more information.

Normal granite, somewhat weathered
Aplitic granite
The difficulty you will experience in examining exposures of the granite is essentially one of access. The land  around is all private property so you will be reduced to looking at road cuttings, for the most part. Parking alongside the Highway or the Jenolan Caves Road at Hartley is not recommended and
Typical granite
in any case there is rarely anywhere to park near a cutting where the best exposures are.

Here are three suggestions, based on approaching from the direction of Sydney.  
Firstly, Hartley Village historic site. You will not be very popular with the National Parks and Wildlife Service if you start hammering the natural outcrops here, but at least you can see the typical granite tors on the hillside from a safe place. What you will see is that the granite consists mainly of quartz and pink orthoclase felspar (I prefer this spelling to feldspar) with lesser amounts of greenish plagioclase felspar, biotite mica and miscellaneous other minerals.

This evening I looked up my first field notebook from August 1959 when I was 17 and just beginning to study geology. I had ridden my bike from Lithgow and examined many outcrops along the way. Life was somewhat simpler then! Here is my observation at Hartley.

Near 2nd church Hartley. Many granite boulders freshly blasted. Very big crystals of pink feldspar.  
Orthoclase phenocrysts weathering out
One boulder covered with fern-like growths of a silver mineral (hardness 4) and a brassy one (hardness 6).”
Back to the present. Perhaps that boulder or one like it is still there. What might the minerals have been? The pink feldspar is orthoclase, in the form of phenocrysts, which is typical of the Hartley Granite. You will find it in every outcrop, though not always as larger crystals. The fern-like growths are dendrites, a form which is typical of minerals which crystallise in confined spaces along joints. They probably formed this way in the last stages of crystallisation of the granite as the rock cracked and watery mineral solutions percolated through it. The silver mineral could be pyrrhotite (FeS), sphalerite (ZnS) or perhaps arsenopyrite (FeAsS). The brassy one could be pyrite (FeS₂). Perhaps a reader will locate specimens and let us know what they think. 

NOTE 20th December 2015.There is major road construction going on around Hartley. This has removed parking opportunities almost completely except at Hartley village. Lots of fresh granite has been exposed and then covered up with concrete. This may be good for roads, but it's certainly bad for the study of geology.

Pegmatite outcrop, River Lett Hill
Secondly, an old quarry on the left of the highway about 200m past the Jenolan Caves turnoff. There is somewhere to park. The quarry is through the fence. This is best accessed if you are in the left lane and not safe if you are coming down the River Lett Hill instead of going up. You can get clear of the traffic here and have a good look around. The place has become a dumping ground for all sorts of rocks and rubbish as well as a parking area for machinery, but there are some outcrops of quartz-orthoclase pegmatite on the upper side. I guess this is what was being quarried, probably for the extraction of the orthoclase which has lots of uses in industry. There are many small outcrops like this around Hartley. Few have been very productive. You can read about the industry and the origin of the pegmatite in the references given below.

Thirdly, along McKane’s Falls Road. This is a narrow, sealed road linking the Great Western Highway and the Jenolan Caves road. It turns off to the left towards the end of Hassan’s Walls at Old Bowenfels, several kilometres after the top of River Lett Hill, immediately after the new road constructions. Parking isn’t easy, but there is a reasonable spot on the right 3.1 km from the highway. From here you can see granite outcrops in the nearby paddocks and especially 
Outcrops near Mt Blaxland
towards Mt Blaxland on the left. Look out for aplite (microgranite) outcrops and areas with orthoclase phenocrysts weathering out of the granite and coarser pegmatites. From here you can continue on to the Jenolan Caves Road, crossing Coxs River just below Mt Blaxland which was the terminal point of the 1813 expedition led by Blaxland, Lawson and Wentworth.

Orthoclase from pegmatite
These early European explorers noted the outcrops of granite in the area, as did George Evans who followed up on their discoveries. William Cox’s road builders passed though here in 1814/15 and made good use of the rock for culverts and embankments. Later visitors
Crystalline quartz from pegmatite
included some of more scientific bent and the area formed part of the first detailed geological map of the country west of the Blue Mountains (1875). Small quantities of gold and other metallic minerals were discovered, but the granite itself and the orthoclase in its pegmatites has always been the resource of greatest value. Austen Quarry is extracting large quantities of these materials today and you will see it from a distance on the right as you return towards Hartley along the Jenolan Caves Road.

These references are all downloadable. Check my blog entries on how to do this from Trove and DIGS.

The Geology of Sydney and the Blue Mountains (J Milne Curran 1899). Trove. Tick “Books” “online” and use the keywords “Curran” Geology” and “Sydney”. You will find several downloadable versions. Mineral Resources 26 Felspar in NSW (1917). DIGS Report Number: Mineral Resources 26.

Mineral Industry NSW Feldspar (1969) DIGS Report Number: Industry 15.

Austen Quarry (2013) Click here.

The Gap silver-lead-zinc mine, Hartley, near Lithgow (1970). DIGS Report Number: GS1970/293

NSW Department of Primary Industries report on Felspar (c.2004). Click here.

Geological Map of Hartley, Bowenfels, Wallerawang, Rydal districts (1875). DIGS Report Number: Heritage Map H0252

Metallogenic Map Sydney (1980). DIGS Report Identification Number: R00027967
From the Sydney Metallogenic Map



 

3 comments:

  1. A delight to find this blog entry.

    I am a still working doctor in my 70s who started doing Science at Sydney Uni before doing Medicine. In my first Year while doing Geology 1 we went on a field trip to Hartley.
    No parking problems then, we arrive by coach and had unfettered access to the virgin rocks.
    Started me on a lifelong love affair with all things Geological.

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  2. Thank you for your comment. My experience is somewhat similar to yours - Geology 1 in 1959, field trips to Bondi, Stanwell Park, Kiama, Prospect and Hartley.
    With access and parking problems I'm finding it difficult to write more blog entries on what is now my local area (Lithgow).
    Most of my geological entries are in my New England Minerals blof.

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