GEDIS REFID: 11099; SOURCE MAP: G11099_quartersheet_23SW_31k_400dpi_colour.tif; SUBJECT: DAINTREE, R., 1862. Quarter sheet 23 SW. Point Henry (Portions of the parishes of Moolap and Bellarine; surveyed 1860) 1:31,680 (40 chains:1 inch) geological map. Geological Survey of Victoria.

GEDIS REFID: 26471; SOURCE MAP: G26471_geology_Bendigo-Mitiamo_100k_200dpi_colour.tif; SUBJECT: WILKINSON, H.E., CHERRY, D.P., KING, R.L., MALONE, M.P., WILLMAN, C.E. & BYRNE, D.R., 1995. Bendigo, and part of Mitiamo 1:100,000 geological map. Geological Survey of Victoria.

GEDIS REFID: 11156; SOURCE MAP: G11156_quartersheet_9SW_31k_400dpi_colour.tif; SUBJECT: APLIN, C.D.H. & ULRICH, G., Undated. Quarter Sheet 9 SW. Holcombe (Portions of the parishes of Holcombe, Burke, Fryers, Drummond, Edgecombe, Lauriston, and Glenlyon) 1:31,680 (40 chains:1 inch) geological map. Geological Survey of Victoria.

GEDIS REFID: 107269; SOURCE MAP: G107269_goldfield_Creswick_31k_600dpi_colour_master.tif; SUBJECT: KRAUSE, F.M., 1981. Creswick Goldfield, geological map, showing the locations of quartz reefs, auriferous leads and shafts. Parish of Creswick 1:31,680 (40 chains:1 inch) geological map. Plan No 587/G/1 (reissue).

Projection data is described in the gridcode column of the attribute table. This number is 1000 times the actual value (retained in this form to capture significant figures through map processing). For example, "Gridcode -23599" equates to -24% (rainfall) and "Gridcode 1986" equates to 2.0 degrees Celsius (temperature). The results are from 23 climate models that were available for the IPCC Fourth Assessment Report (2007). It is assumed that that the model results give a representation of the real world response to a specific emissions scenario. The IPCC (2007) estimates of global warming are relative to the period 1980-1999. For convenience, the baseline is often called 1990. Projections are given for 2030 and 2070 but, of course, individual years can vary markedly within any climate period, so the values can be taken as representative of the decade around the single year stated, i.e. projections for 2030 are representative of 2026-2035. Natural variability (independent of greenhouse gas forcing) can cause decadal means to vary and estimates of this effect are included in the estimates of uncertainties. The projections comprise a central estimate and a range of uncertainty. The central estimate is the median – or 50th percentile - of the model results, while the uncertainty range is based on two extreme values – the 10th and 90th percentiles. 10% of values fall below the 10th percentile and 10% of values lie above the 90th percentile. Greater emphasis is given to projections from models that best simulate the present climate. The weightings are based on statistical measures of how well each model can simulate the 1975-2004 average patterns of rainfall, temperature, and sea level pressure over Australia. Subregions of Victoria are indicated. Victoria has an integrated catchment management system established under the Catchment and Land Protection Act 1994 (the CaLP Act). Under the CaLP Act, Victoria is divided into ten catchment regions, with a Catchment Management Authority (CMA) established for each region. (See: http://www.water.vic.gov.au/governance/catchment_management_authorities)

GEDIS REFID: 11112; SOURCE MAP: G11112_quartersheet_2SW_31k_400dpi_colour.tif; SUBJECT: SELWYN, A.R.C., 1858. Quarter Sheet 2 SW Broadmeadows (Portions of the parishes of Tullamarine, Bulla Bulla, Yuroke, Will-Will-Rook and Wollert) 1:31,680 (40 chains:1 inch) geological map. Department of Mines, Victoria.

This is a pseudocolour image of the Decompensative Anomaly Victorian state-wide gravity grid data generated using a histogram-equalised colour-stretch draped over a sun illuminated intensity surface. ‘Cooler’ colours indicate lower values and ‘warmer’ colours represent increasingly higher Decompensative Anomaly values, in micrometres per second squared (mm/s^2). The Decompensative Anomaly grid includes a correction that accounts for the long-wavelength anomalies remaining in the Isostatic Residual Anomaly associated with lateral density variations within the lithosphere. Colour: 2009 Decompensative Anomaly Victorian state-wide 250x250m grid. Intensity: 2009 Decompensative Anomaly Victorian state-wide 250x250m grid. Sun illumination was set at 45 degrees azimuth and 60 degrees altitude.

GEDIS REFID: 29378; SOURCE MAP: G29378_geology_Murchison_50k_600dpi_colour_master.tif; SUBJECT: EDWARDS, J., 1998. Murchison 1:50,000 geological map. Geological Survey of Victoria.

GEDIS REFID: 31498; SOURCE MAP: G31498_geology_Myrtleford_50k_colour_ed1.tif; SUBJECT: VANDENBERG, A.H.M., MORAND, V.J., QUINN, C., EDWARDS, J. & WOHLT, K.E., 2004. Myrtleford 1:50,000 geological map. Geological Survey of Victoria.