Compiled by the Geological Survey of N.S.W., Division of Regional Geology. Topographical base compiled from Snowy Mountains Hydro Electrical Authority, Department of Lands, County maps and Snowy Lease Map. Other sheet adjoin this map. There are 13 formation sections grouped into 9 - Quaternary, Tertiary, Middle Devonian, Lower to Middle Devonian, Lower Devonian, Upper Silurian, Silurian, Upper Ordovician and Ordovician.Large coloured map showing geological features, faults, bores, rivers and mineral deposits.Scale of map, longitude and latitude, river names. "Tallangatta 1:250,00" written in black pen.tallangatta, new south wales, geological survey, topographical base, snowy mountains hydro electrical authority, department of lands, snowy lease map, department of mines, quaternary, tertiary, middle devonian, lower to middle devonian, lower devonian, uper siluran, silurian, upper ordovician, ordovician

Phyllograptus nobilis H. and K. Middle Ordovician Reddish brown coloured rock, 'Mo74' on sticker. Fossil collection was formerly held by the School of Mines Museum, Pall Mall, Bendigo.

Diplograptus (Glytograptus) austrodentatus H. and R. Middle Ordovician. Grey rock, multiple graptolite specimens on surface. "Mo51' and 'Mo52' on stickers. Fossil collection was formerly held by the School of Mines Museum, Pall Mall, Bendigo.geology, rock, specimen

Trichograptus immotus H. and T. (37442) Middle Ordovician. Dark grey rock. 'Mo63' on sticker on rock adjacent to graptolite specimen. Fossil collection was formerly held by the School of Mines Museum, Pall Mall, Bendigo.

Diplograptus (Glyptograptus) teretinseulus var. englyphus Lapw. (37397) Middle Ordovician. Pale brown rock, 'Mo54' on sticker alongside single stipe graptolite fossil. Fossil collection was formerly held by the School of Mines Museum, Pall Mall, Bendigo.

4 pages from the 'Mining and Geological Journal', July 1938. Front page is an index to figures in the graptolite collection. 'Numbers in brackets are taken from the Fossils Register of the Mines Department Museum, Melbourne, and refer to the specimens in the Museum.' Lancefieldian, Bendigonian, Chewtonian, Castlemainian, Yapeenian, Middle Ordovician, Upper Ordovician, Gisbornian, Estonian and Bolindian categories are described. The numbers on the BHS fossil collection relate to the numbers/names on the page. Two following pages illustrate the fossil types within the major categories. Small sign with pages ' 'Fossils, Bendigo & /surrounding Districts' was with the fossil display in a glass display cabinet, ex Museum of Mines Museum, Bendigo.

Four page document, not sequential. Front page: structural trends, major faults and folds in the Bendigo area are depicted in a diagram. Fault lines and folds include the Leichardt Fault, the Break O'Day Fault, Sebastian Fault, Whitelaw Fault, the Yankee Creek Fault and the Fosterville Fault. Aecond page shows the typical reef forms on the Bendigo goldfield (Willman 1988) in a diagram. The Sebastian goldfield is described, with its four lines of reef, the Eureka, Gaskill's, Frederick the Great and Gamboni. Third page describes the White Hills gravels. Fourth page is a table showing thel biostratigraphic zonation of the Ordovician bedrock based on key graptolite forms and assemblages.bendigo, mining, geological bulletin

The low rolling hills of the Kimbolton countryside consist of ancient, hard and fractured Ordovician rock up to 65 million years old, which was originally deposited deep under the sea. Rocks mainly are sandstone, mudstone, black shale and quartz conglomerates. Marine fossils can be found in the area. Around seven million years ago a basalt flow buried the original bedrock along the along the Campaspe River. Ongoing weathering, wind and water movement over the following years has produced younger clay, sand, silt and gravel deposits throughout the area. Patches of White Hills Gravel are also found in the area. Another unique geological feature of this area is the Permian Glacial Pavement rocks north and south of Eppalock and glacial sediments (such as “Dunn’s Rock” and “Kellams Rock”). During the ice age (up to 280 million years ago) large glaciers moving over the countryside, scoured out sediments, pulverized bedrock, polished and cut grooves into bedrock in the direction of ice movement. When the ice melted boulders etc where left behind in areas of entirely different rock types, such as a 100 Tonne granite block known as ‘The Stranger’ near Derrinal. Dunn's Rock (Glaciated Pavement) Eppalock - Photos of the rock and a field group collecting date with Lake Eppalock (Knowsley) in the backgroundhistory, bendigo, dunn's rock eppalock, kimbolton forest, lake eppalock, gately collection