The Andes mountain range is more likely to have active volcanoes than the Rockies. The Andes have a higher concentration of active volcanoes due to tectonic activity along the South American plate boundary, whereas the Rockies are older and inactive in terms of volcanic activity.
If a deep ocean trench is located adjacent to a continent, active volcanoes would likely be found on the continent's edge or along the tectonic plate boundary. These volcanoes are often associated with subduction zones where one tectonic plate is being pulled beneath another, leading to magma generation and volcanic activity.
Active volcanoes are those which are liable to erupt or have shown frequent eruptions within recent history.They are ones that still erupt at (irregular) intervals, often gently emitting gases and steam during their quiescent spells.
Mountain ranges are often formed by tectonic plate movements that can also cause earthquakes and volcanic activity. Thus, areas with prominent mountain ranges are more likely to have earthquake epicenters and volcanoes due to the tectonic forces at work. The distribution of mountain ranges can serve as an indication of potential earthquake and volcanic activity in a region.
If a mountain range was not formed by subduction, it likely formed through other tectonic processes such as continental collision, volcanic activity, or uplift due to crustal stretching. The absence of subduction would suggest a different geological history and set of conditions in the region where the mountain range is located.
Explosive volcanoes are most likely to occur in subduction zones where one tectonic plate is forced beneath another, leading to the melting of rock and the buildup of pressure. Regions like the Ring of Fire in the Pacific Ocean are known for their explosive volcanic activity.
Active volcanoes and dormant volcanoes both have a likely chance to erupt and have erupted in the past.
Volcanoes are most likely to form at the edges of the tectonic plates.
Hawaii Hawaii was formed from a volcano that grew from deep on the ocean's floor. If it was on land it would be several times higher than the tallest mountain.
sea floor spreading
Active volcanoes are likely to erupt at any time where as inactive volcanoes are 'asleep' or haven't erupted much in the past and are unlikely to erupt in the near future.
Active mountain belts are likely to be found at tectonic plate boundaries where convergent or collisional forces are causing the Earth's crust to fold, uplift, and form mountain ranges. These regions typically include places like the Himalayas, the Andes, the Rocky Mountains, and the Alps.
Arabian Plate and Eurasian plate
Active volcanoes: are those that erupted lava,gases ,cinder,pumice,etc in the historic pass.Eg: Mt.St.Helena Dormant volcanoes: are those which erupted in the past and are likely to erupt again after remeaining inactive for fairly long periods. These are "sleeping" volcanoes which may become active once again. eg: Mt.vesuvius.Extinct volcanoes: are those volcanoes which were active in the remote geological periods. Eg: Mt.Kenya
Active mountain belts are most likely to be found along tectonic plate boundaries, particularly convergent boundaries where two plates collide. This collision forces the crust to buckle and fold, creating mountain ranges. Examples of active mountain belts include the Andes in South America and the Himalayas in Asia.
Active volcanoes are not likely to be located at convergent boundaries where an oceanic plate subducts beneath a continental plate because the melting point of the oceanic crust is lower, causing it to melt and create volcanic features before reaching the surface. Instead, active volcanoes are more commonly found at divergent boundaries where plates move apart.
because large continents are bigger so that means more mountains and some mountains are volcanoes.
Boundaries that are least likely to have active volcanoes are divergent boundaries where tectonic plates move away from each other, such as the Mid-Atlantic Ridge. At these boundaries, the magma rises to the surface in a more gentle manner, resulting in less explosive volcanic activity.