You’re very welcome jimc.
Yes, volcanoes are the first thing that comes to mind regarding atmospheric data collection but, as you can imagine, there is much more that could be detected (Raspberry Boom (RBOOM/ RS&BOOM) Infrasound Monitors):
Volcanic activity -per se- is not invisible to seismographs, but its detection (as it is for earthquakes) depends on the intensity and distance between you and the volcano. If the activity is weak/too distant, its signal may be lost in the overall background noise that every location on Earth has.
So, yes, volcanoes are sources of both infrasounds/vibrations, and if the activity is close/strong enough, you may record both, or one of them. To give you a practical example, when the Hunga-Tonga erupted, I was obviously too far away to detect any vibration (on the other side of the world), but my BOOM detected the released pressure wave twice (both short and long trips).
There are many possible factors that contribute to seismic signal detection, such as installation position, location, type of material upon which the Shake is positioned, soil type and density, depth to bedrock, structural footing and attachment to bedrock, bedrock type, and more.
When you’ll get yours, you will start to see what you can detect and learn about your location in more detail. It was the same for me after I bought my RS3D.
Ultimately, both infrasound and seismic data are very interesting, and if you are oriented in learning about both, then the RS&BOOM is the Shake for you.
On the other side, if instead you want to focus more on earthquake activity, the RS4D is the perfect choice for your location.
I don’t know if I was able to help you decide, and if not, I remain available for any other questions/chat you want to have on the subject.