Clearly they are in a line over the top of MacFarlane - that places them at least in line with Icarus - see my first photo to see the change in angle when viewing from the ascent gully.
Likewise - my shot was from high up in the ascent gully - well above the horizontal banding further down - and checking the different positions of the tops at/near Falling Mt - the old photo is taken from a spot higher than I was. [Falling Mt appears well above the ridge high point - whereas in my shot they are almost in line]
Check this shot also - the relative gap is only slightly bigger here than the old photo - but mine is also taken from a higher spot than the edge of the plateau next to Icarus.
Also note that whereas most of the dolerite on Ossa tends to be vertical columns, this section is flat with a high percentage of blocks fallen on their sides and covered in soil.

- Taken from just below the top of Ossa looking across top plateau - note the photo view gap of Falling Mt relative to the high point on the ridge. I suspect they were somewhere near the ringed area.
The old shot is a telephoto which compresses distance. For such a telephoto shot looking down on those tops, I am not sure how you can conclude anything about height relative to the Ducanes?
Maybe the fact that the shot is
angled slightly down is creating an illusion of being taken from a lower spot?
Finally - Is the lower horizontal band sandstone or siltstone? It would probably be the same band that appears on the side of Pelion East at Toad Rock.
Does your friend have a geological map of the area?
Edit - just checked an online resource - and the lower cliff face [with waterfall] is sandstone.