This specimen was donated in 1868 by Alfred Selwyn. Olivine is typically found in basic and ultra-basic igneous rocks around the world, in a variety of colours including yellowish green, olive green, greenish black and reddish brown with a transparent to translucent diaphaneity. The luster of the specimen is vitreous, the luminescence non-fluorescent and when fractured the mineral is very brittle producing small, conchoidal fragments. Chromian diopside is normally found in small sizes as the larger the size of the mineral the darker the colour is, almost black rather than green. Chromium is the element that gives chromian diopside and emeralds their rich green colour. Diopside is found across the world in multiple colours however gem-quality chromian diopside is mined in Siberia, Russia and prominent within the jewellery industry as a more affordable substitute to emeralds. Chromium-bearing diopside has been located across Australia. Chromium-bearing Diopside is located across the world found in North America, parts of South America, and across Australia, Africa, Europe and Asia. Chromium-bearing Diopside is mined in Siberia, Russia and is sold as a commercial substitute for emeralds. The stone is often turned into jewellery. This item is one of many geological and mineral specimens that constitute a broader collection obtained from various regions across Australia (as well as some international locales) and generously contributed to the Burke Museum between 1868 and 1880. A significant portion of these specimens originated from Victoria and were acquired as a result of the Geological Survey of Victoria, initiated in 1852 during the Gold Rush era. The primary objective of this survey was to investigate and chart the geological characteristics of Victoria. The procurement of geological specimens played a vital role in advancing our comprehension of the Earth's scientific composition and was instrumental in supporting research and educational institutions throughout Australia, including the Burke Museum, in their efforts to foster further exploration and study. A solid mineral specimen in shades of green, grey and brownburke museum, beechworth, geological, geological specimen

This is a small book of 64 pages with a buff-coloured plasticised cover with printed material and a photograph of Elizabeth Rafferty. The pages contain printed material, maps, photographs and illustrations and an index.non-fictionFamily history of Elizabeth Rafferty bostock family, elizabeth rafferty, warrnambool, rachel rafferty, robert bostock

This book, written by Graeme Bennett, gives information on the Bennett family history and the history of the Stawell Woollen Mills. The Bennett family was associated with the textile industry for more than 200 years. The book gives information on John Edward Bennett (1862-1928) who, in 1909 became the first manager of the Warrnambool Woollen Mill. This mill opened in 1910 and closed in 2000 and was a dominant business, known throughout Australia for its woollen blankets. John Bennett was a highly-successful manager at the Warrnambool Woollen Mill from 1909 until his death in 1928. His son, who was the assistant manager at the mill, left in 1926 to take over the Stawell Woollen Mill.This book is of considerable interest as it contains valuable information on the author’s grandfather, John Edward Bennett, important in Warrnambool’s history as the first manager of the Warrnambool Woollen Mill, a prominent business in Warrnambool for 90 years.This is a soft cover book of 384 pages. The front cover has a mottled cream and black background with black lettering and a colour photograph of a painting of the Stawell Woollen Mill. The back cover and spine have the same mottled pattern with black lettering. The book has 22 chapters and several colour and black and white photographs. john e bennett, warrnambool woollen mill, stawell woollen mill