10. BORENORE CAVES 


The pronunciation appears to be (or close to) "Boreenaw". 

Here are some quotes about this location: 

From "Speleo Handbook 1968". Situated 11 miles west of Orange . Massive beds of Silurian limestone outcropping for about 2 miles along the Boree Creek. First reported by Mitchell (1841). 

Caves: Big Caves; series of arches. Little Caves (Tunnel  Cave); 300 yards of cave, extensive silting has occurred. Verandah Cave; now largely silted up. McDonald's Cave: pothole 80 feet deep in sink; foul air.

Other caves exist in the area."

From "Limestone Deposits of NSW 1919" by Carne and Jones. Mineral Deposits of NSW 25 (NSW Geological Survey). Pages 148-149.

"Situated on Boree Creek, 11 1/4 miles by road from Orange and 3 miles west of Borenore Railway Station, 209 miles from Sydney."

"Mitchell mentions the limestone caves of the "Buree" locality which he and others partially explored."

"The limestone occurs chiefly in the sides of valleys in different places, and still contains many unexplored caves."

"These caves were subsequently examined by Mr O. Trickett L.S. M.S. in 1903 who described two - the "Big" and Little Caves."

From "The Limestone Deposits of New South Wales" 1986 by  Lishmund, Dawood and Langley. Mineral Deposits of NSW 25 (NSW Geological Survey, 2nd edition. Pages 117-118

"Caves. A number of large caves occur in the deposits, together with some smaller caves. One of the caves, the Tunnel Cave, is 100 m long.
However, mining of parts of the deposits would be precluded because of the presence of caves, while other environmental considerations might militate against extraction from other areas. parts of the deposit are deeply weathered, and overburden and clay-filled cavities might pose further problems.
Parts of the deposits were quarried until about 1940 for ornamental stone."
Map from Carne and Jones 1919

From The Guide to NSW Karst and Caves (2011)

"Access to Borenore Karst Conservation Reserve is by Orange–
Forbes Road, which is sealed. The access road to the picnic area is
an all-weather gravel road.
The reserve contains picnic facilities, including tables and gas
barbecues, and public toilets. Well-maintained walking tracks
traverse the area, providing an opportunity for visitors to explore
Arch Cave, a variety of protruding limestone outcrops and the
remnant stand of threatened white box–yellow box woodland.
Camping is not permitted at the reserve which closes at 7 pm daily."

The Arch Cave. Follow this link to a great article on the Arch Cave.
https://www.walkmyworld.com/posts/arch-cave-borenore


The Verandah and Tunnel Caves. 

Here is a link to an excellent article on these two caves.

https://www.walkmyworld.com/posts/verandah-cave

There are many other caves at Borenore. Those worth protecting are mostly gated and locked.

Song Studies. Bible studies based on hymns and songs

Shoalhaven District Geology.

Comments

Post a Comment

Popular posts from this blog

5. ROSEBROOK CAVES

Image
  ROSEBROOK CAVES                             The Rosebrook Caves have been formed in an extensive belt of limestone (the Bunyan Limestone) a few km north-west of Cooma in southern NSW. The caves described below are located in the northern part of the outcrop. Some of karst features in the limestone appear to be quite ancient. Fossils are relatively rare. The first mention of Rosebrook Caves that I have found was in the DailyTelegraph (Sydney) Tuesday 26th January 1892. " CAVES DISCOVERED NEAR COOMA , Monday.  Last week a few persons descended a hole on Rosebrook Station, six miles from Cooma, From Carne & Jones. The cave is under the M of "Woolumla" which has been known for years,in the hope of finding a cave. After descending about 60ft. they came to a chamber 30ft. high by 20ft. wide by 40ft. long. The cave was surrounded by splendid formations of stalagmites and stalactites, many of which were accid...
Read more

2 LIMEKILNS NEAR BATHURST

Image
 2. LIMEKILNS NEAR BATHURST I have selected Limekilns for the first blog entry, as this appears to be the first place in NSW where a limestone cave was reported and explored (1821) . Previously,  explorer George Evans had observed and recorded the presence of limestone in several places near Canowindra (1816). The discovery of limestone was  significant because of its use in making mortar and for agricultural purposes. Previously, sea shells had been gathered in large quantities around Sydney and Newcastle, including from aboriginal middens, and roasted to make quicklime which was then "slaked" by  adding water  to produce slaked lime, usually referred to as lime. Limestone is essentially calcium carbonate and it is commonly derived from marine shellfish.  Fossils of these are frequently  found in limestone and associated sedimentary rocks. A little chemistry:   calcium carbonate  (calcite)  CaCO 3;   calcium ...
Read more

4. ASHFORD CAVES

Image
  ASHFORD CA VES From the Ashford Tourism website The Ashford limestone caves are located about 20km north-west of the town of Ashford, between Inverell and the Queensland border. What was once a crown reserve (set apart in 1915) is now part of the  Kwiambal National Park (pronounced Kiamble), best known for the spectacular  MacIntyre Falls , near which is a delightful camping area at Lemon Tree Flat. Picnic and toilet facilities are also provided at the caves. These caves are not in the same league as the well-known show caves at Jenolan, Wombeyan and Yarrangobilly, in fact there are very few speleothems  (decorations) to be found. What you will find is bats, guano (bat droppings) and a sense  of adventure as you explore the unknown (to you) cave system. If you would like to read a fascinating account of “ An Excursion to the Severn River and the Wallangra Caves ” dating from 1892 ( here ) you will appreciate that some things have not changed, but others have c...
Read more