Low water level Plenty River in Greensborough. A River bank stabilisation project along the Plenty River at Greensborough was conducted by Melbourne Water in 2015.Digital copy of colour photographplenty river, melbourne water

Consists of two photographs, one an enlargement of the smaller print.lal lal falls., low water level., parents with children

Also a second black and white postcard showing two rowboats on river at wide bend 05350.1 8.5 x 13.5 cmBlack and white postcard showing view of Upper Nicholson River with three women shown, water level low Nicholson VictoriaNicholson River waterways, boats and boating

This photograph was taken in the 1960s at Lake Sambell and is a view across the lake from the east side, the photo was taken during a period of improvements to the lake and surrounding area. Lake Sambell is an artificial lake that was created on the site of the old Rocky Mountain Mining Company workings and was officially opened by Minister for Lands, Mr Baily, on October 5, 1928. The disused and unattractive remains of the mine were converted into a recreational area intended for swimming, boating, and fishing. The lake is named after Mr L.H. Sambell, shire engineer and secretary of the Forward Beechworth Committee, who advocated for the enhancement of Beechworth into a tourist destination and was central to the planning and establishment of the lake. Funding for the project was raised through both competition funds and donations. Since the construction in 1928 several engineering issues have arisen. In 1939 the water levels were low, and the lake was considered both an eyesore and ‘mudhole’, Beechworth Shire Council sort funding to raise the height of the lake six feet to improve the quality of water. Throughout the 1940s the Beechworth Swimming Club sort to address the structural engineering issues and improve swimming facilities at the lake. R.E. Carter, similar to L.H. Sambell, was a shire engineer who advocated the importance of positioning Beechworth as a tourist destination. Carter held the position of shire engineer from 1954-63 and organised many improvements to the Lake Sambell area including the caravan park in 1959, the lake swimming pool in 1961, water skiing and boating facilities, and increased the lake surface area in 1964. These improvements to the lake also reflect an increase in leisure time and access to travel during a period of post-war prosperity in Australia during the 1950s and 60s. This photograph is of historical significance as it documents Lake Sambell in the 1960s after a series of enhancements to the lake area to improve its appearance and usability for both the people of Beechworth and tourists. It is also of social significance in providing an insight into the increase in leisure time and access to travel during a period of post-war prosperity. Black and white rectangle photograph printed on photographic paper and unmounted.Reverse: 3534 C798lake sambell, l.h. sambell, r.e. carter, rocky mountain mining company, forward beechworth committee, beechworth swimming club, wallace park lake sambell development scheme, lake sambell caravan park, beechworth 1960s, lake sambell swimming pool, lake sambell boating, lake sambell fishing, swimming, boating, water skiing, fishing, post-war prosperity, minister of lands, artificial lake, open cut sluice mine, lake

This photo was taken in the 1960s from a northeast position looking down towards Lake Sambell, the caravan park, and the surrounding area. This photo was taken during a period of rejuvenation for the lake area including the opening of the caravan park in 1959 and the swimming pool area in 1961 (this pool is just visible in the centre of the photo). The popularity of caravanning in Australia exploded during this post-war period of the late 1950s and 1960’s. This popularity was driven by multiple factors, including: the stopping of fuel rations, the accessibility of car ownership through the manufacturing of affordable cars, technological developments in caravan design, and the increase in prosperity and leisure time for many Australians. Lake Sambell is an artificial lake that was developed on the previous site of the Rocky Mountain Mining Company workings and was officially opened by Minister for Lands, Mr Baily, on October 5, 1928. The disused and unattractive remains of the mine were converted into a recreational area intended for swimming, boating, and fishing. The lake is named after Mr L.H. Sambell, shire engineer and secretary of the Forward Beechworth Committee, who advocated for the enhancement of Beechworth into a tourist destination and was central to the planning and establishment of the lake. Funding for the project was raised by both competition funds and donations. Since the construction in 1928 several engineering issues have arisen. In 1939 the water levels were low, and the lake was considered both an eyesore and ‘mudhole’, Beechworth Shire Council sort funding to raise the height of the lake six feet to improve the quality of water. Throughout the 1940s the Beechworth Swimming Club tried to raise awareness and funds to address the structural engineering issues and improve swimming facilities at the lake. R.E. Carter, similar to L.H. Sambell, was a shire engineer who advocated the importance of positioning Beechworth as a tourist destination. Carter held the position from 1954-63 and organised many improvements to the Lake Sambell area including the caravan park in 1959, the lake swimming pool in 1961, water skiing and boating facilities, and increased the lake surface are in 1964. These improvements were financed mainly by grants from the Tourist Development Authority. This photograph is of historical significance as it documents Lake Sambell and the surrounding area in the 1960s after a phase of enhancements to improve the appearance and usability for both the people of Beechworth and tourists. It is also of social significance in providing an insight into the increase in leisure time and access to travel during a period of post-war prosperity.Black and white rectangle photograph printed on matte photographic paper and unmounted.Reverse: 1 / [logo KODAK/ VELOX/ PAPER] / C798 / 3535lake sambell, lake sambell caravan park, lake sambell swimming pool, caravan park, caravanning 1960s, rocky mountain mining company, l.h. sambell, r.e. carter, beechworth swimming club, forward beechworth committee, minister of lands, tourist development authority, lake swimming, swimming, boating, fishing, water skiing, beechworth 1960s, lake sambell fishing, lake sambell boating

'Drop Zone', is set in an imagined future where decreasing water availability has affected us more dramatically than anyone predicted. The water shortage has become so severe that we have to access water on a first-come first-serve basis, from military-like water ‘drop zones’, like this one, made from modified rain water tanks. These tanks function on three levels: Collected rain water causes the totem sculptures to rise and bloom; evaporation causes the totem sculptures to fall; and an anemometer (device that measures wind speed) drives a process that plays the tank like a giant drum, tuned by the amount of water contained within. This artwork envisions a future for Australia where the impact of decreasing water availability has had a more dramatic effect than any of the predictions. The shortage is so severe that military-like water ‘drop zones’, constructed of modified rainfall storage tanks have been established across the public parks of the City of Yarra for access on a first come, first serve basis. However, as the water is only replenished through rain catchment the tanks may only offer infrequent relief for the City of Yarra residents, standing as hollow reminders of the effects of inaction on the shaping of sustainable national water use.'Drop Zone' was one of three public art works installed in Yarra, in 2011, under the banner of The Environmental Public Arts Project which responded to key features of Council's Environment Strategy: 'Towards Local Sustainability 2008-2020.' The aims of this project included activating public spaces in new and creative ways through the creation of artworks which act as catalysts for further engagement and discussion around environmental themes and issues.Copyright the Artists. Ready-made corrugated water tanks arranged on a site. Situated within the tanks are small totemic sculptures that float on top of the water within the tank.Accompanying plaquesustainability, water, environment, climate change

Wattle Gully, at Chewton was first worked in 1853 albeit initially only to a depth of 10 metres. An exploratory drilling in 1934, that deflected off course, discovered new rich gold seams and by 1937 large amounts of gold were being extracted. The mine closed in 1969 because high water levels and the low price of gold made it unprofitable at the time. It has operated intermittently since then.Horwood Collection - Wattle Gully. Wattle Gully Mine, Chewton. Much of the buildings and other structures still remain. Markings Wattle Gully Chewton. DEC65MKodakmine, gold, walltle gully, horwood collection - wattle gully. wattle gully mine, chewton. much of the buildings and other structures still remain

This small green bottle has been handmade by a glassblower and is the typical shape of a carbonated soda or mineral water bottle. It was made from 1840s-1870s. The bottle was found in the coastal waters of Victoria about 100 years from when it was made. It is part of the John Chance Collection. Glassblowers made bottles like this one by blowing air through a long pipe and into molten glass at the end of it. The shape of the glass would be blown out to fit into the shape of the cylindrical dip mould. Once it set, the glass was removed from the mould and the glassblower would continue using the pipe to create the neck and another ponty tool to push up and form the base. The bottle would be cracked off the end of the glassblower’s pipe and a blob of molten glass would be wrapped around the top of the neck and shaped to finish the lip of the bottle. The seal was usually a cork, held in place with a ball-wire fitting attached between the upper and lower parts of the neck finish. This style of handmade bottles usually had thick glass so that it could be heat-sterilised, then re-filled. The bottles would often have horizontal bubbles in the applied finish, caused by twisting the glass, and vertical bubbles and diagonal lines in the body from it being blown, and a pontil mark in the base where the ponty tool had been attached. Although the bottle is not linked to a particular shipwreck, it is recognised as being historically significant as an example of bottles imported for use in Colonial Victoria in the mid-to-late 1800s. The bottle is also significant as it was recovered by John Chance, a diver in Victoria’s coastal waters in the late 1960s to early 1970s. Items that come from several wrecks have since been donated to the Flagstaff Hill Maritime Village’s museum collection by his family, illustrating this item’s level of historical value. Bottle; green glass, soda or mineral water style, handmade. Double ring collar blob finish on neck; upper is wide and rounded, lower is a thin ring. Diagonal lines in glass on neck, low shoulder mould seam, rippled texture around body. Push-up base with pontil mark, rectangular impression in heel. Uneven base. Sediment on inside surfaces.flagstaff hill, warrnambool, flagstaff hill maritime museum, maritime museum, shipwreck coast, flagstaff hill maritime village, great ocean road, shipwreck artefact, john chance, glass bottle, antique bottle, handmade, dip mould, mouth blown, pontil mark, 19th century bottle, collectable, soda bottle, mineral water bottle, green glass, blob finish, push-up base

This small green bottle has been handmade by a glassblower and is the typical shape of a carbonated soda or mineral water bottle. It was made from 1840s-1870s. The bottle was found in the coastal waters of Victoria about 100 years from when it was made. It is part of the John Chance Collection. Glassblowers made bottles like this one by blowing air through a long pipe and into molten glass at the end of it. The shape of the glass would be blown out to fit into the shape of the cylindrical dip mould. Once it set, the glass was removed from the mould and the glassblower would continue using the pipe to create the neck and another ponty tool to push up and form the base. The bottle would be cracked off the end of the glassblower’s pipe and a blob of molten glass would be wrapped around the top of the neck and shaped to finish the lip of the bottle. The seal was usually a cork, held in place with a ball-wire fitting attached between the upper and lower parts of the neck finish. This style of handmade bottles usually had thick glass so that it could be heat-sterilised, then re-filled. The bottles would often have horizontal bubbles in the applied finish, caused by twisting the glass, and vertical bubbles and diagonal lines in the body from it being blown, and a pontil mark in the base where the ponty tool had been attached. Although the bottle is not linked to a particular shipwreck, it is recognised as being historically significant as an example of bottles imported for use in Colonial Victoria in the mid-to-late 1800s. The bottle is also significant as it was recovered by John Chance, a diver in Victoria’s coastal waters in the late 1960s to early 1970s. Items that come from several wrecks have since been donated to the Flagstaff Hill Maritime Village’s museum collection by his family, illustrating this item’s level of historical value. Bottle; green glass, soda or mineral water style, handmade. Applied finish, blob double ring collar; upper is wide and rounded, lower is a narrow ring. Diagonal lines in glass on neck and shoulder. Low shoulder mould seam. Body is matt and tapers inward towards base. Shoulder and neck are shiny. Push-up base with pontil mark. Uneven base. Bubble on top of lip. Sediment on inside surfaces. White rubbing line and scratches on outside. flagstaff hill, warrnambool, flagstaff hill maritime museum, maritime museum, shipwreck coast, flagstaff hill maritime village, great ocean road, shipwreck artefact, john chance, glass bottle, antique bottle, handmade, dip mould, mouth blown, pontil mark, 19th century bottle, collectable, soda bottle, mineral water bottle, green glass, blob finish, push-up base

This small green bottle has been handmade by a glassblower and is the typical shape of a carbonated soda or mineral water bottle. It was made from 1840s-1870s. The bottle was found in the coastal waters of Victoria about 100 years from when it was made. It is part of the John Chance Collection. Glassblowers made bottles like this one by blowing air through a long pipe and into molten glass at the end of it. The shape of the glass would be blown out to fit into the shape of the cylindrical dip mould. Once it set, the glass was removed from the mould and the glassblower would continue using the pipe to create the neck and another ponty tool to push up and form the base. The bottle would be cracked off the end of the glassblower’s pipe and a blob of molten glass would be wrapped around the top of the neck and shaped to finish the lip of the bottle. The seal was usually a cork, held in place with a ball-wire fitting attached between the upper and lower parts of the neck finish. This style of handmade bottles usually had thick glass so that it could be heat-sterilised, then re-filled. The bottles would often have horizontal bubbles in the applied finish, caused by twisting the glass, and vertical bubbles and diagonal lines in the body from it being blown, and a pontil mark in the base where the ponty tool had been attached. Although the bottle is not linked to a particular shipwreck, it is recognised as being historically significant as an example of bottles imported for use in Colonial Victoria in the mid-to-late 1800s. The bottle is also significant as it was recovered by John Chance, a diver in Victoria’s coastal waters in the late 1960s to early 1970s. Items that come from several wrecks have since been donated to the Flagstaff Hill Maritime Village’s museum collection by his family, illustrating this item’s level of historical value. Bottle; green glass, soda or mineral water style, handmade. Applied finish, blob double ring collar; upper is wide and rounded, lower is a narrow ring. Diagonal lines in glass on neck and shoulder. Low shoulder mould seam. Body is matt with ripples in glass, tapers inward towards base. Shoulder and neck are shiny. Push-up base with pontil mark, visible through glass. Marks on heel. Uneven base. Bubble on side and top of lip. Sediment on inside surfaces. Two score lines, one half way down body, one near base. flagstaff hill, warrnambool, flagstaff hill maritime museum, maritime museum, shipwreck coast, flagstaff hill maritime village, great ocean road, shipwreck artefact, john chance, glass bottle, antique bottle, handmade, dip mould, mouth blown, pontil mark, 19th century bottle, collectable, soda bottle, mineral water bottle, green glass, blob finish, push-up base

This small green bottle has been handmade by a glassblower and is the typical shape of a carbonated soda or mineral water bottle. It was made from 1840s-1870s. The bottle was found in the coastal waters of Victoria about 100 years from when it was made. It is part of the John Chance Collection. Glassblowers made bottles like this one by blowing air through a long pipe and into molten glass at the end of it. The shape of the glass would be blown out to fit into the shape of the cylindrical dip mould. Once it set, the glass was removed from the mould and the glassblower would continue using the pipe to create the neck and another ponty tool to push up and form the base. The bottle would be cracked off the end of the glassblower’s pipe and a blob of molten glass would be wrapped around the top of the neck and shaped to finish the lip of the bottle. The seal was usually a cork, held in place with a ball-wire fitting attached between the upper and lower parts of the neck finish. This style of handmade bottles usually had thick glass so that it could be heat-sterilised, then re-filled. The bottles would often have horizontal bubbles in the applied finish, caused by twisting the glass, and vertical bubbles and diagonal lines in the body from it being blown, and a pontil mark in the base where the ponty tool had been attached. Although the bottle is not linked to a particular shipwreck, it is recognised as being historically significant as an example of bottles imported for use in Colonial Victoria in the mid-to-late 1800s. The bottle is also significant as it was recovered by John Chance, a diver in Victoria’s coastal waters in the late 1960s to early 1970s. Items that come from several wrecks have since been donated to the Flagstaff Hill Maritime Village’s museum collection by his family, illustrating this item’s level of historical value. Bottle; green glass, soda or mineral water style, handmade. Rough applied finish, blob double ring collar; upper is wide and rounded, lower is a narrow ring. Diagonal lines in glass on neck. Low shoulder mould seam. Body is matt, tapers inward towards base. Shoulder and neck are shiny. Push-up base with pontil mark, visible through glass. Marks on heel, glass thickness varies. Uneven base. Bubble in glass. Sediment on inside surfaces. flagstaff hill, warrnambool, flagstaff hill maritime museum, maritime museum, shipwreck coast, flagstaff hill maritime village, great ocean road, shipwreck artefact, john chance, glass bottle, antique bottle, handmade, dip mould, mouth blown, pontil mark, 19th century bottle, collectable, soda bottle, mineral water bottle, green glass, blob finish, push-up base

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 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 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

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 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 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 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 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 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 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

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

"In 1839 John Dight purchased Melbourne block 88, which included 26 acres of land along the Yarra River for £481 at the Port Phillip land sales held in Sydney. Dight was already in the business of flour milling and had a mill near Campbell Town in New South Wales called ‘Ceres’. In April 1840, he notified his customers through The Sydney Herald that he was leaving to go to Port Phillip. The first steam powered flour mill was constructed in Melbourne in 1841. Dight built his water powered mill, soon after, from bricks bought over from Tasmania. Dight used the river to power his mill: Water flowed along an inlet channel to turn an undershot water wheel. In order to regulate flow or to ensure flow for times when river levels were low, Dight constructed a rough stone weir." (Melbourne Water)Dights Mill. Reproduction of a book plate from an original wood engraving, showing Dights Mill and Falls on the River Yarra. The image was originally published in Sands & Kenny, Melbourne & Sydney.Annotation on reverse: "Dights Flour".dights mill, yarra river