No. Pyroclastic flows are a result of volcanic eruptions.
A small area of a country or state where earthquakes occur frequently.
Earthquakes can happen, but on small scales, the country does not lie on a tectonic plate, so they will not occur
On average, there are roughly 20,000 - 30,000 recorded earthquakes every year.The USGS estimates that several million earthquakes occur in the world each year but many go undetected because they hit remote areas or have very small magnitudes.
Extremely few. Most earthquakes happen in the ocean, or too far below the crust for us to feel them, but hundreds happen every week.
Not all they can occur inside plates due to slip on a fault or fracture, they can also occur after mass wasting events (landslides) and due to volcanic activity where as magma shifts underground it breaks up rocks causing small earthquakes often refered to as magmatic tremor.
The US Geological Survey estimate that there are several million earthquakes each year, but the vast majority of these will not be detected because they are too small in magnitude to detect or are larger, but occur to far away from a seismometer station. From this number, they estimate that there are 500,000 detectable earthquakes in the world each year. 100,000 of these will be felt by humans and 100 of them will be large enough to cause damage.
Thousands occur every year, most of which are too small to notice.
That is impossible to tell. Smaller earthquakes occur more frequently, to the extent that the majority of earthquakes are too small to event be felt. Without a sophisticated seismic network, many earthquakes will not even be detected.
The type of pyroclastic material known as 'little stones' is lapilli. Lapilli are small rock fragments ranging from 2 to 64 mm in diameter that are ejected during volcanic eruptions.
Pelean volcanic eruptions feature pyroclastic flows, which are fast-moving currents of hot gas, ash, and volcanic rock fragments. Plinian eruptions also produce pyroclastic flows, but they are characterized by massive vertical columns of ash and gas rising high into the atmosphere.
1,000 - 3,000, though almost all are too small to be felt by humans.
Most small earthquakes are just background seismicity. There is no way to tell whether a small event will be followed by a larger one. But if there is a larger earthquake afterwards, the first earthquake is called a "foreshock"