The photo was probably taken by Will Herbert and used at the 1937 "Back to Orbost" celebrations. The photo depicts the Snowy River at Orbost when it was at a high level.A coloured photograph in a brown wooden frame which has gold painted decorated edges. A wire hanger is attached. The photo shows reflections of trees along the bank of the Snowy River in 1937.On bottom right of photo - Snowy River Orbost On back of frame - Back to Orbost 1937 from Will Herbertphotography snowy-river orbost-1937

Mount Bogong located in the Alpine National Park and part of the Victorian Alps of the Great Dividing Range, is the highest mountain in Victoria, Australia, at 1,986 metres (6,516 ft) above sea level. The Big River separates the massif of the mountain from the Bogong High Plains to the south. From the nearby town of Mount Beauty to its summit, Mount Bogong rises more than 1,600 metres (5,200 ft), thus making it one of the highest peaks in Australia not only in terms of its elevation above sea level, but also in terms of actual base-to-summit prominence. Mount Bogong is a popular backcountry skiing mountain through winter but only has snow for the mid winter-spring months. It is around 30 kilometres (19 mi) by road and walking track or 12 kilometres (7.5 mi) direct to Mount Beauty. Falls Creek and Mount Hotham ski resorts are also nearby. Camping is relatively safe below the tree line but the summit ridgeline is very exposed. Emergency shelter is also available at Bivouac Hut on the Staircase Spur, and at Cleve Cole, above Camp Creek on the broad ridge to the south of the summit, and Michells Hut on the Eskdale Spur. Mt Bogong is a popular recreational venue in the Kiewa Valley for back country skiing and bush walking and is a favourite with sightseers and popular subject for photographersBlack and white photograph of Mt bogong taken from Tawonga - Thursday May 6th, 1937Handwritten on back of photograph. Thursday May 6th, 1937. Mt Bogong Tawongamt bogong, tawonga, kiewa valley

This photograph was taken during construction of the Rocky Valley Dam and wall. Work was commenced in early 1947 but had to be suspended during winter and then resumed in October. Work continued in 1948 with the establishment of work facilities and, at the dam site, the river was diverted through a temporary pipeline. Rocky Valley and associated spillway and outlet works were completed in 1959.A pictorial record of the construction of the rock and earth filled dam wall at Rocky Valley. Shows the extent of the project undertaken and the level of importance of the project as indicated by the large representation at the parliamentary party visit on 15/4/48.Photocopy of black and white photograph of parliamentary party visiting Rocky Valley Dam site 15/04/1948Typed on the bottom of photocopy - State Electricity Commission of Victoria. Date: 15-4-48 Time: 4.30pm No: K4397. Kiewa Hydro-Electric works. Parlimentary Party at Rocky Valleyrocky valley dam, parliamentary party, secv

This bamboo fishing rod was used in the mid to late 1900's and demonstrates that local production of recreational fishing poles was at a high level and their demand was high. Imported recreational sporting goods from either the United Kingdom, the United States of America or Asia countries was due to the larger lead up times from these suppliers and the greater import costs from slower ocean supply ships. It was only after World War II that the trade influx from other countries has supplied cheaper goods. This recreational fishing pole is highly significant to the Kiewa Valley as it demonstrates that recreational fishing has been evolved from the need to supply a balanced diet by the early pioneer families of fish from the major Kiewa rivers. The ability of the Kiewa Valley rivers to provide a good fishing environment (high protein diet) for both early indigenous families and early pioneers was the important food source that provided for a balanced diet and the higher level of nutritious development of both body and mind. This two piece wooden fishing Rod is made from bamboo shafts or poles, one length thicker than the other. The smaller diameter shaft is the top end and fits into the longer thicker shaft at a stainless steel tube end.The smaller shaft has a stainless steel reinforcement ring where both shafts fit together. At the bottom end of the thick shaft is a black rubber "stopper" or "foot". There are two stainless steel rings, each with a reel holding "bulge" which allows for the the reel's "prongs" to be secured. The top ring has a greater diameter allowing it to move up and down the shaft/pole to secure the top "prong" firmly onto the shaft/pole.recreation, river, rod, fishing, industry, fish

This photo was taking during construction of the tailrace tunnel between West Kiewa Power Station and Mt. Beauty. Much of the area was unstable and timber supports were erected prior to concreting. The tunnel was commenced in 1941 and completed in 1952. It brings water from the power station into the open tailrace at Mt. Beauty and then into the regulating pondage before discharge into the Kiewa River.Shows method of construction for supporting walls and ceiling of tunnel with timber, size of tunnel (note worker on upper level), and conditions in the work place during construction in the 1940's/50's - note the timber ladder to gain access to the upper level.Black and white photographHand written on back of photograph "Tunnel face at Tailrace showing Arch Drive".tailrace, power station, water, construction

The toothed whales (also called odontocetes, systematic name Odontoceti) are a parvorder of cetaceans that includes dolphins, porpoises, and all other whales possessing teeth, such as the beaked whales and sperm whales. Seventy-three species of toothed whales are described. They are one of two living groups of cetaceans, the other being the baleen whales (Mysticeti), which have baleen instead of teeth. The two groups are thought to have diverged around 34 million years ago (mya). Toothed whales range in size from the 4.5 ft (1.4 m) and 120 lb (54 kg) vaquita to the 20 m (66 ft) and 55 t (61-short-ton) sperm whale. Several species of odontocetes exhibit sexual dimorphism, in that there are size or other morphological differences between females and males. They have streamlined bodies and two limbs that are modified into flippers. Some can travel at up to 20 knots. Odontocetes have conical teeth designed for catching fish or squid. They have well-developed hearing, that is well adapted for both air and water, so much so that some can survive even if they are blind. Some species are well adapted for diving to great depths. Almost all have a layer of fat, or blubber, under the skin to keep warm in the cold water, with the exception of river dolphins. Toothed whales consist of some of the most widespread mammals, but some, as with the vaquita, are restricted to certain areas. Odontocetes feed largely on fish and squid, but a few, like the killer whale, feed on mammals, such as pinnipeds. Males typically mate with multiple females every year, but females only mate every two to three years, making them polygynous. Calves are typically born in the spring and summer, and females bear the responsibility for raising them, but more sociable species rely on the family group to care for calves. Many species, mainly dolphins, are highly sociable, with some pods reaching over a thousand individuals. Once hunted for their products, cetaceans are now protected by international law. Some species are attributed with high levels of intelligence. At the 2012 meeting of the American Association for the Advancement of Science, support was reiterated for a cetacean bill of rights, listing cetaceans as nonhuman persons. Besides whaling and drive hunting, they also face threats from bycatch and marine pollution. The baiji, for example, is considered functionally extinct by the IUCN, with the last sighting in 2004, due to heavy pollution to the Yangtze River. Whales occasionally feature in literature and film, as in the great white sperm whale of Herman Melville's Moby-Dick. Small odontocetes, mainly dolphins, are kept in captivity and trained to perform tricks. Whale watching has become a form of tourism around the world. Reference: https://en.wikipedia.org/wiki/Toothed_whaleWhale teeth were much prized for use in scrimshaw work.Whale tooth. Significant staining and yellowing. Broken at base, and missing the root.Noneflagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, whale tooth, whaling, whaling industry, whales

Diggers & Mining. Getting the Gold. Slide: On some fields - notably those on the Ovens and its tributaries, where there were no leads - ancient gold-bearing sands and gravels were found in river terraces high above the level of the stream. These were usually treated by a process known as sluicing. Water from higher levels of the stream was diverted through races to point of operations . . . Markings: 59 994.LIF:4. Used as a teaching aid.hanimounteducation, tertiary, goldfields

The donation was accompanied by the following letter from the donor: "Hi. I found these in with family photos. Taken by family as Mamie McLeod was living in Fellows Street, Kew, so would be near there. Retain (or discard) as you see fit." [Donor's name and address withheld from public view]. To gain an insight into the flood levels at Kew, it is worth reading newspaper accounts of the event. The Age published an article - Valuable Gardens Destroyed at Kew - on 25 September 1916: "VALUABLE GARDENS DESTROYED AT KEW. From the heights of Studley Park, Kew, a splendid view of the flood waters can be obtained, and yesterday afternoon, despite continuous rain, crowds of citizens assembled there to witness the spectacle. There is a vast stretch of water some 300 or 400 yards broad, above the foot bridge connecting Gipps-street, Collingwood, and Studley Park. The river is only about 3 feet from the top of the embankment connecting with the ramp of the bridge on the Studiey Park side. When the upper llood waters come down it is almost a certainty that tne embankment will be submerged and the bridge rendered impassible. Below the bridge the waters again stretch out, and have submerged all the low-lying land on the Collingwood side and invaded the back premises ot the Kodak Co., Phoenix Biscuit Factory, a tannery adjoining thereto, the Shamrock Brewery, and Chinese gardens in the vicinity. At Walmer-street-bridge, at the end of Studley Park, the low-lying land on the Kew side is covered with water to the depth of many feet. Tlie land in question is owned in a great part by Mr Frank Lavers who haa gone in for intense culture on a pretty liberal scale on both the slopes of the hill and on the river flat. On the latter he is cultivating many acres of asparagus, and has at a considerable cost spent three years in preparing the ground and installing an irrigation system, reticulated from the Yan Yean water supply. This year the asparagus was put down, and the plants were in a promising condition. Tlie flood waters are now flowing fast over the land. The crop is ruined, and three years' work and expenditure destroyed. Mr. Laver's private residence fortunately is high above flood level, but two houses he owns off Young-street have been flooded out. Having been warned in time, the tenants removed their furniture hefore the water came down to Mr. Laver's residence, where they themselves have been given accommodation in the meantime. All the river flats in East Kew are under water. One or two low-lying houses have been flooded. Chipperfield's boat shed at Willsmere is nearly covered, and some Chinese gardens in the vicinity are several feet under water."This, and the other three photographs donated of floods in Kew are believed to be the earliest in the collection. Together with our original MMBW River Yarra map showing flood levels, these items, when compared allow researchers to gain a visual perspective of the extent of the flood in 1916. Black and white photograph of flooded trees in Kew with rising dry ground in distance.Inscription on reverse in pencil: "Flood River Yarra Kew Vic"river yarra, kew, floods 1916

The donation was accompanied by the following letter from the donor: "Hi. I found these in with family photos. Taken by family as Mamie McLeod was living in Fellows Street, Kew, so would be near there. Retain (or discard) as you see fit." [Donor's name and address withheld from public view]. To gain an insight into the flood levels at Kew, it is worth reading newspaper accounts of the event. The Age published an article - Valuable Gardens Destroyed at Kew - on 25 September 1916: "VALUABLE GARDENS DESTROYED AT KEW. From the heights of Studley Park, Kew, a splendid view of the flood waters can be obtained, and yesterday afternoon, despite continuous rain, crowds of citizens assembled there to witness the spectacle. There is a vast stretch of water some 300 or 400 yards broad, above the foot bridge connecting Gipps-street, Collingwood, and Studley Park. The river is only about 3 feet from the top of the embankment connecting with the ramp of the bridge on the Studiey Park side. When the upper llood waters come down it is almost a certainty that tne embankment will be submerged and the bridge rendered impassible. Below the bridge the waters again stretch out, and have submerged all the low-lying land on the Collingwood side and invaded the back premises ot the Kodak Co., Phoenix Biscuit Factory, a tannery adjoining thereto, the Shamrock Brewery, and Chinese gardens in the vicinity. At Walmer-street-bridge, at the end of Studley Park, the low-lying land on the Kew side is covered with water to the depth of many feet. Tlie land in question is owned in a great part by Mr Frank Lavers who haa gone in for intense culture on a pretty liberal scale on both the slopes of the hill and on the river flat. On the latter he is cultivating many acres of asparagus, and has at a considerable cost spent three years in preparing the ground and installing an irrigation system, reticulated from the Yan Yean water supply. This year the asparagus was put down, and the plants were in a promising condition. Tlie flood waters are now flowing fast over the land. The crop is ruined, and three years' work and expenditure destroyed. Mr. Laver's private residence fortunately is high above flood level, but two houses he owns off Young-street have been flooded out. Having been warned in time, the tenants removed their furniture hefore the water came down to Mr. Laver's residence, where they themselves have been given accommodation in the meantime. All the river flats in East Kew are under water. One or two low-lying houses have been flooded. Chipperfield's boat shed at Willsmere is nearly covered, and some Chinese gardens in the vicinity are several feet under water."This, and the other three photographs donated of floods in Kew are believed to be the earliest in the collection. Together with our original MMBW River Yarra map showing flood levels, these items, when compared allow researchers to gain a visual perspective of the extent of the flood in 1916. Panoramic view, believed to be looking north towards Fairfield from the Zig-Zag Bridge on the River Yarra. The inscription on the reverese identifies it as taken before 1920.Inscription on reverse in ink "(pre 1920) Flood from Zig-zag bridge Yarra River, Kew Vic."river yarra, kew, floods 1916, zig-zag bridge

The donation was accompanied by the following letter from the donor: "Hi. I found these in with family photos. Taken by family as Mamie McLeod was living in Fellows Street, Kew, so would be near there. Retain (or discard) as you see fit." [Donor's name and address withheld from public view]. To gain an insight into the flood levels at Kew, it is worth reading newspaper accounts of the event. The Age published an article - Valuable Gardens Destroyed at Kew - on 25 September 1916: "VALUABLE GARDENS DESTROYED AT KEW. From the heights of Studley Park, Kew, a splendid view of the flood waters can be obtained, and yesterday afternoon, despite continuous rain, crowds of citizens assembled there to witness the spectacle. There is a vast stretch of water some 300 or 400 yards broad, above the foot bridge connecting Gipps-street, Collingwood, and Studley Park. The river is only about 3 feet from the top of the embankment connecting with the ramp of the bridge on the Studiey Park side. When the upper llood waters come down it is almost a certainty that tne embankment will be submerged and the bridge rendered impassible. Below the bridge the waters again stretch out, and have submerged all the low-lying land on the Collingwood side and invaded the back premises ot the Kodak Co., Phoenix Biscuit Factory, a tannery adjoining thereto, the Shamrock Brewery, and Chinese gardens in the vicinity. At Walmer-street-bridge, at the end of Studley Park, the low-lying land on the Kew side is covered with water to the depth of many feet. Tlie land in question is owned in a great part by Mr Frank Lavers who haa gone in for intense culture on a pretty liberal scale on both the slopes of the hill and on the river flat. On the latter he is cultivating many acres of asparagus, and has at a considerable cost spent three years in preparing the ground and installing an irrigation system, reticulated from the Yan Yean water supply. This year the asparagus was put down, and the plants were in a promising condition. Tlie flood waters are now flowing fast over the land. The crop is ruined, and three years' work and expenditure destroyed. Mr. Laver's private residence fortunately is high above flood level, but two houses he owns off Young-street have been flooded out. Having been warned in time, the tenants removed their furniture hefore the water came down to Mr. Laver's residence, where they themselves have been given accommodation in the meantime. All the river flats in East Kew are under water. One or two low-lying houses have been flooded. Chipperfield's boat shed at Willsmere is nearly covered, and some Chinese gardens in the vicinity are several feet under water."This, and the other three photographs donated of floods in Kew are believed to be the earliest in the collection. Together with our original MMBW River Yarra map showing flood levels, these items, when compared allow researchers to gain a visual perspective of the extent of the flood in 1916. Small black and white photograph of flooded trees in Kew.Inscription on reverse in ink "Flood R. Yarra Kew Vicriver yarra, kew, floods 1916

SHARP DOWNPOUR. ONE INCH IN 45 MINUTES. SOUTHERN SUBURBS DELUGED. TRAIN STOPPED AT SOUTH YARRA. One of the sudden downpours of rain which occasionally fall in Melbourne occurred yesterday afternoon, when nearly an inch of rain fell in the course of three quarters of an hour, and caused a flood for an hour or two in certain localities. During the early part of the day, the sky had been clouded over, but there was nothing to indicate a storm of such intensity as that which followed. At about half-past 1 o'clock residents of South Yarra, South Melbourne, Prahran, and St. Kilda noticed a few drops of rain. Still, it appeared unlikely that there would be anything exceptional, until with startling suddenness at about 10 minutes to 1 o'clock, one of the heaviest downpours within the memory of residents burst upon those suburbs. A strange feature of the storm was that it was practically confined to an area of about three miles square. The city was but little affected, though at a spot as close as the Observatory 86 points of rain were recorded in three-quarters of an hour. Thunder and lightning accompanied the downpour, which was cyclonic in character, the rain driving heavily from all points of the compass as the cyclone passed. It was in South Yarra and Prahran that the rain fell heaviest. Within a few minutes after it commenced, the low-lying portions of Toorak-road and practically the whole length of Chapel-street were under water. The depression at the intersection of Toorak-road and Darling-street speedily filled to the dimensions of a small lake. Several shops were inundated, while the water from the higher levels rushed down like a mountain torrent, and in several in-stances swept through the rear of houses and shops, carrying furniture in a floating mass against the further walls. In one case a footbridge was carried bodily away and dashed to pieces. Darling-street itself Great Davis-street, and other low-lying and flat thoroughfares in the vicinity became flooded from kerb to kerb, while on the other side of the railway-bridge the valley between Kensington-road and River-street became filled for some minutes to a depth of several feet. Meanwhile the waters from South Yarra hill, seeking a lower level, found it in the railway cutting, and the excavations from South Yarra station to Prahran on the one line, and to the Chapel-street bridge on the other, were converted into a couple of canals. At the platforms at South Yarra the water was two feet deep on the permanent way, and towards Hawksburn, at the sudden depression under Chapel-street bridge, it was at one time deep enough to cover a tall man's head. Into this swirling mass of water the 1:50 p.m. train from Oakleigh plunged on its way to Melbourne. The impact caused a mighty fountain of water to rise to a height of about 20 feet above the level of Chapel-street and send clouds of spray in all directions. Under the belief that a terrible explosion had occurred residents braved the rain and rushed to the spot, only to find that the train had been brought to a stand-still in the middle of what seemed to be a river. The water was so high that it had entered the fire-box from below, extinguishing the fires and cutting off the steam supply. In the meantime the officials at the South Yarra station had been preparing for emergencies. Inspectors were on duty at intervals along the line, and the moment the alarm was given an extra engine was backed carefully down and continued on to connect with the stranded train without losing its own power. There was a delay of about ten minutes in the service for an hour or two, but by 5 o'clock all the trains were running on time again, and the water had run off all but the spot beneath the Chapel-street bridge. Here the water remained about four feet deep until nightfall, and throughout the afternoon several hundreds of people including biograph operators and photographers, were gathered around watching each train pass through. Even with the water two feet lower, this was a work attended with considerable difficulty. Each train had to absolutely force its way through the weight of water, almost enveloped by the spray thrown up, and it was only just able to negotiate the "ford" by using every ounce of steam. ... The Argus, 26 January 1907, p19.The item forms part of the Laurie Bennett collection of thirty-six postcards and photographs of Kew and early Melbourne, donated to the Kew Historical Society in 1980. The postcards in the Bennett collection, like other images in the Society's holdings date from the 1890s to the present and comprehensively indicate points-of-view or scenes considered historically, aesthetically or socially significant in the period in which they were produced.Postcard depicting a flood at South Yarra Station in 1907. The title and photographer's name are identified on the front of the postcard. Donated by L. Bennett, 1980flood - south yarra, trains - melbourne, postcards, r mcgeehan - prahran

The Melbourne and Metropolitan Board of Works (MMBW) was established by an act of the Victorian Parliament in 1890 to prepare for and to implement a sewerage and water reticulation system across what was then inner Melbourne, its surrounding and middle distance suburbs, including Kew. The MMBW was disbanded in 1991.The map collection of the Kew Historical Society has at its core the historic maps assembled and originally stored in the City Engineer's Department of the City of Kew. These include maps in a number of scales. The vast majority of maps were produced by the MMBW in the first two decades of the twentieth century, and are solid working maps, backed by linen for durability. These maps are historically significant to Kew, the City of Boroondara and to the history of the development of state utilities in Victoria. A number of the Kew maps have additional details added by former municipal officers, including the levels reached by various floods. As these were working documents, information was added to them long after the period of their initial production and distribution.Early map of part of the Borough of Kew, created in the first decade of the twentieth century, at a scale 160 ft to 1 inch. The map covers what was then the south western section of Kew, bordered on its north by Studley Park Road, in the west by Walmer Street and the River Yarra, by High Street South and Princess Street in the East and Barkers Road in the south. The map shows the extent of urban development by that time, prominent institutions and the outlines of built structures in the municipality. Contour lines and historic flood levels were added in ink to the map at a later stage.MELBOURNE AND METROPOLITAN BOARD OF WORKS / PLAN NO. 40 / COLLINGWOOD & KEWmelbourne & metropolitan board of works, mmbw maps, mmbw plans, borough of kew, cartography

In 1988, as part of a Defence of Mainland Australian policy, defence of facilities of strategic importance in northern Australia were allocated to Army Reserve units. ‘A’ Squadron was allocated the defence of Tindal Air Force base located 15 KM outside Katherine in Northern Territory. Consequently the Squadron deployed on Exercise ‘Northern Explorer’ to gain first-hand knowledge of operating conditions for mounted and dismounted patrolling in the area.Colour photograph of Captain C. Carrington, earing hat, and Sergeant Koschel of ' A ' Squadron 8/13 VMR during Exercise " Northern Explorer." Flood debris caught high in tree branches indicate water level during wet season on Ferguson River, Northern Territory.

In 1975 the Melton Fire Station opened in McKenzie Street. In the 1950s with the introduction two-way HF and later VHF very high frequency radio sets. Melton Rural Fire Brigade was part of the Bacchus Marsh Group. Radio sets where located in the Melton Fire Truck, and in the house of the Barrie family at Ferris Road. This was an ideal location to observe a 360 degree view in all directions when smoke appeared on the horizon. An antenna was erected beside the house. The set OX 7 was located in the kitchen and monitored 24 hours by the family. When an electrical fire occurred at the junction of the electricity to the house there was time to radio the fire station and summons the men working in the paddocks, thus saving the house from possible destruction. With the introduction of UHF – ultra high frequency Vinten Radios the signal was clearer and static and interference lessened and radio traffic became easier to read, and reduced noise levels in the household. In 1974 when the family moved to First Avenue, another antenna and a small building were erected adjacent to the residence and used to house the equipment, maps. Radio traffic consisted of regular schedule times and communication with adjoining groups of brigades such as Bacchus Marsh, Mt Macedon and Little River Groups. Many of the brigade and group base radios were situated in private residences and operated primarily by fire fighters wives who held the position of Communications Officer, either registered as a brigade member or informally.Regional News Gazette article about the construction of a new fire station in Melton and an Express article with brigade members at the opening of the station.emergency services

Black and white photograph showing P S Tanjil on Tambo River. Water level high in river, note bushes in water. Eucalypt hanging over the river on right. Thick vegetation on banks. Swan Reach VictoriaTambo Riverships and shipping, waterways

John Perry Collection. Laminated copy of photo of crowd watching flow of water from the opened valve at the wall of Lake Eppalock during its commissioning. March, 1964. Lake Eppalock was created by flooding to town of Wild Duck. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system.water, dam, reservoir, eppalock, wild duck

John Perry Collection. Laminated copy of map detailing Lake Eppalock shoreline when empty. Circa 1951. Has colored highlighter lines following roads leading to lake shoreline and various inundated old roads and tracks on lakebed. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system.map, eppalock, reservoir, lake, water

John Perry Collection. Laminated copy of map of Lake Eppalock at full capacity. Had highlighter markings of old roads which appear to be still in use. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system.map, water, dam, reservoir, eppalock

John Perry Collection. Laminated copy of worksheet identifying inundated artifacts at Lake Eppalock when at 10% capacity. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system.map, artifacts, eppalock, reservoir

John Perry Collection. Laminated copy of map pertaining to Lake Eppalock. Gives details of dwellings, bridges and ford crossings. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system.eppalock, map, water, dam, reservoir

John Perry collection. Map 'C'. Laminated map of overlay of Lake Eppalock at full capacity. Circa 1951. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system.map, water, eppalock, dam, reservoir

John Perry Collection. Laminated map of Lake Eppalock at full capacity. Black and white. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system.map, eppalock, water, dam, reservoir

John Perry Collection. Laminated map of Lake Eppalock empty. Map 'D'. Circa 1951. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system.map, water, dam, reservoir, eppalock

John Perry Collection. Laminated copy of 'Directions to Lake Eppalock'. Gives directions in relationship of Lake Eppalock to Bendigo, Kyneton and Heathcote. Undated. Gives basic descriptions of bridges on lakebed, ford crossings on lakebed and inundated dwellings on lakebed. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system.water, dam, directions, eppalock

John Perry Collection. Laminated 'legend' for Maps A, B and C for Lake Eppalock also in this collection. Black and White definitions and descriptions of objects and markers found on maps. Circa 1951. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system.map, water, dam, reservoir, eppalock

John Perry Collection. Laminated copy of page from 'Weekly Times' newspaper, February, 1962. Nine images relating to establishing and building Eppalock Reservoir, 15 miles from Bendigo. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system. dam, engineering, water, eppalock

John Perry Collection. Laminated copy black and white map. Map 'B'. Outline of Lake Eppalcok, overlayed on map. Circa 1951. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system.map, water, dam, reservoir, eppalock

John Perry Collection. Laminated copy of map relating to Lake Eppalock. Lists dwellings, ford crossings and bridges. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system.map, water, dam, reservoir, eppalock

John Perry Collection. Laminated map of proposed construction of Lake Eppalock. Map 'A'. Black and white map in laminate. Circa 1951. The dam was built by the State Rivers and Water Supply Commission of Victoria. The dam wall height is 45 metres (148 ft) and the main embankment is 1,041 metres (3,415 ft) long. At 100% capacity the dam wall was designed to hold back 304,651 megalitres (6.7014×1010 imp gal; 8.0480×1010 US gal) of water. The surface area of Lake Eppalock is 3,011 hectares (7,440 acres) and the catchment area is 2,124 square kilometres (820 sq mi). The controlled spillway is capable of discharging 8,040 cubic metres per second (284,000 cu ft/s). Lake Eppalock supplies both stock and domestic water to the Campaspe irrigation district. It also serves as a water supply to Bendigo and Heathcote and, in more recent times, Ballarat. The lake is a major attraction for those engaging in watersports, with a number of tourist parks and accommodation facilities available. Permissible activities on the lake include high-speed boating, water skiing, sailing, canoeing, fishing and swimming. The lake's water levels were low for approximately eight years between 2002 and 2010 during a prolonged drought, which restricted the amount of recreational activity until rainfall in the latter half of 2010 returned the lake to 100 percent capacity. Built between 1961 and 1964, Lake Eppalock remains the only water storage on the Campaspe River system.map, dam, water, weir, eppalock