Along fault lines
They can't. Radio waves are used to transmit information about earthquakes and tsunamis, but cannot affect the events themselves.
Earthquakes themselves are natural disasters, and they can trigger secondary events such as tsunamis, landslides, and liquefaction. Volcanic eruptions can also be associated with earthquakes, especially in regions with active volcanic activity.
They emit a sound that bounces off surroundings and makes it's way back to the bat. It can then navigate itself around trees, other animals, and etc.
Earthquakes do not have a distinct smell. The shaking during an earthquake may create dust or release gases from the ground, but there is no specific scent associated with earthquakes themselves.
Humans adapt to earthquakes by planning and preparing. Those living on fault lines practice earthquake preparedness, have an evacuation plan, and know how to keep themselves safe indoors and outdoors.
Yes, parents often find themselves seeking help to navigate the challenges of raising children.
Humans can protect themselves by preventing damage to their head and neck. You should hide under a sturdy table and or other protective structure.
Melting rocks themselves do not directly cause earthquakes. However, the movement of molten rock beneath the Earth's surface, such as in a volcanic system, can create pressure changes that can trigger earthquakes. Additionally, the cooling and solidification of magma can cause rock to fracture, potentially leading to seismic activity.
Sunlight polarization can help certain animals, like birds and insects, navigate by providing them with directional information. These animals can detect the polarization pattern of sunlight and use it as a compass to orient themselves and navigate accurately.
Worms can not see, they just feel for moisture in the ground and navigate themselves to areas with high moisture. (This is why there are worms on the ground when it rains.)
Earthquakes occur most often along tectonic plate boundaries, specifically at convergent boundaries where one plate sinks beneath another (subduction zones) or at transform boundaries where two plates slide past each other horizontally. Additionally, earthquakes can also occur within plates themselves due to intraplate stress and faulting.
Landslides triggered by earthquakes often cause more destruction than the earthquakes themselves. During the 1964 Alaska quake, shock-induced landslides devastated the Turnagain Heights residential development and many downtown areas in Anchorage.