Uhh,, are you crazy?? It's got an atmosphere with clouds of pure acid that snows lead sulfide on a surface that'll melt you face in 5 seconds.
So, this is not only wrong, but it'd actually be more convenient if it were true ;)
Venus's middle cloud layer (the one in question) is actually more like vog (volcanic fog) on Earth. It's not an acid bath, it's a sparse aerosol, with visibility measured in kilometers. The particulates are higher molar than on Earth, but otherwise, it's not a very aggressive environment, and if not for the molarity difference it would be on the order of standard worker PEL levels. You could be out in shirtsleeves for quite a while before you started getting dermatitis (but you would need face protection, both for breathing, and to protect your eyes - not just from the aerosols, but also e.g. carbon monoxide).
(Here I should add the caveat that we don't know if there's any precipitation or dew/frost in Venus's middle cloud layer; it's still a debated topic. We've put so damned little resources into studying Venus, unfortunately, and as a result there's still massive unanswered questions)
Lead sulfide has absolutely nothing to do with Venus's middle cloud layer. It is a (probable) surface phenomenon in Venus's highest regions. The fact that Venus's surface is a natural chemical vapor deposition lab (plus has some interesting volcanic fractionalization / selective thermal erosion possibilities) does, however, raise interesting resource possibilities. The surface, though hostile, was accessible even to Soviet tech developed in the 1960s; much of what we build for industry has to endure vastly more hostile conditions than Venus's surface. The air is so dense that it makes landing much easier than on Mars - it's been calculated that with the right trajectory, you could fire a hollow titanium sphere at Venus, have it enter the atmosphere, decelerate from orbital velocity, and land intact on the surface, without any entry/descent system whatsoever). One probe lost its parachute during descent and still landed intact. The atmosphere is dense enough that you can "dredge" loose material, and fly around with a small metal bellows balloon (controlling flight with small winglets), and return to altitude with a phase-change balloon.
(There is - probably - a metal in Venus's middle cloud layer, but it's small amounts of iron chloride, a soluble salt)
As for the comment I made earlier about how it would be easier if the middle cloud layer had more acid: sulfuric acid is a resource to a Venus habitat. While it's not needed for lift (lift on Venus can be done with just normal, breathable Earth air, with about half the lift of helium on Earth - you can live inside your envelope, with N2 straight from the atmosphere and O2 made from CO2), H2SO4 is your main source of *hydrogen*. Specifically, heating the aerosols first releases free water vapour. Further heating splits it into SO3 and more H2O. You can then further heat the SO3 over a vanadium pentoxide catalyst to split it to SO2 and O2, or you can inject the SO3 into the front of your scrubber to help extract more free water vapour (it's not all in the aerosols) .
Hydrogen is needed not just for your habitats's water needs (note: gases will always slowly permeate in and out of your envelope, it's not a closed system), but also for propulsion for ascent stages and for producing polymers (including the envelope itself). Ascent stages need lots of hydrogen, unless you go hydrogen-free (carbon monoxide, cyanogen, etc), but these have either poor ISP or big problems with things like toxicity, stability, and/or esp. combustion chamber temperature); even "low hydrogen" fuels like acetylene, diacetylene, H additives to hydrogen-free props, etc still need massive amounts of hydrogen to reach orbit. Chemical rockets would need to be at least two stages, be recovered by balloons, hang and be manipulated from the bottom of the envelope, and would take up the majority of your lift capacity. Far more realistic are nuclear thermal rockets - while they burn pure hydrogen, they're so efficient at it that they don't use that much, they give you SSTO capability, and a number of designs can allow for propellantless atmospheric flight / hover (for easier docking).
Your three limiting resources are hydrogen, fluorine (from HF in the atmosphere, but there's not that much HF in the atmosphere if you plan to use a lot of fluoropolymers), and "metals" - the latter being limited by how much you're dredging or digging the surface (with the exception of small amounts of iron from iron chloride).
BTW, hydrogen on Venus isn't the same as on Earth - it's over 2 orders of magnitude higher deuterium percentage (H+ was lost via the solar wind). Probably not high enough to be a health threat, but high enough to be a resource. If you store energy via reversible fual cells/electrolysis, you can wire them in a cascade to separate deuterium every time you charge and discharge. Fuel cells and electrolysis have quite high separation factors for deuterium. At about $1k per tonne, deuterium wouldn't be a viable export commodity at *current* launch pricing, but if launch costs get down enough, it certainly could become one. The other thing Venus has in abundance is power - both solar (though it depends on your latitude and altitude), and of particular note, wind between different altitudes. If you hang a winged wind turbine off a long cable from the main altitude, having it fly many km lower or higher than the habitat, you have a nonstop, quite intense wind differential to generate from.