It depends on your primary focus and geological knowledge (and I don't have the two maps side by side to compare so this is a generalization). Every one of the old maps I showed earlier had contours on them (as is common from the 1940s onward with the advent of aerial photography). Keep in mind that if you are GIS-trained it is easy to register an old map and then superimpose modern topographic contours on it.
Also, there are different types of Cenozoic (Tertiary) and Holocene sediments - shown here as 4 different groupings such as Pliocene and Recent - and the old maps give additional info as to what you can expect of any gold distribution (they can all look much the same in the field). But that is probably more than most people want - it increases chances of success, but in most cases people just want to get out there - and spend a lot of some days searching where there is unlikely to be any gold at all. Unfortunately it requires some geological understanding. For example, if you go back to my post #25, the 2nd (Gordon) and 3rd (Mt Egerton) map examples, they show Tpg (in yellow) and large areas of Qro. I would not personally waste a minute running my detector over any such areas (eg Tpg on these maps is probably sand from an old sea, unlikely to show any gold concentrations). But they look much like sand and gravel in the area deposited by ancient rivers, that do contain gold. It is one reason I favour detecting gold shed down hillsides from reefs, as WalnLiz describe (I can tell the differences between gravels but it really requires knowledge of the area you are in - e.g. those deposited in the sea tend to have well-rounded quartz pebbles and a polished, pearly look to pebbles - I think it was Hawkeye who posted an example).
I will give an example of application of the old maps - you have a broad area of green alluvium on the old Dunolly map with a dotted area shown within it.
View attachment 4854
Shafts do not indicate where gold occurred, they indicate where old-timers dug when looking for gold, which is not always the same thing. The gold was not in the "green" alluvium, it was in an older channel beneath it. The dots usually indicate that position - shafts not sunk on the dotted area were those not thought to have yielded gold (on this map positions of nuggets are shown I think, as well as depths to bedrock in feet). There was no point in showing shafts on the old maps (although most would have been on the actual lead positions once the old-timers got into slightly deeper ground). Often individual shafts were shown on old maps if deeper workings were present, as with "deep lead" shafts. but they were not good indicators of the lead position because they tended to be sunk off to one side of the lead, a drive being put towards the lead at depth).
So positions of recognizable shafts nowadays on modern maps can be meaningless (or worse, quite misleading) as to where the lead was at depth) - they are simply a feature of where a shaft can still be recognized, which may or may not have been a shaft correctly sunk on the lead. Claims were tiny - in shallow leads (the best ones to detect dumps on) you could almost jump the distance between shafts, so there was no point in the old-time geologists mapping them all. Most old shafts are often obliterated by dozing, ploughing and floods nowadays.
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