The location of the earthquake's epicentre in relation to centres of population is important. A high magnitude earthquake that occurs far from a populated area will do less damage than a lower magnitude earthquake in very close proximity to a populated area.
Secondly, ground motion and the amplitude of seismic waves is strongly dependent on the medium through which they travel. Seismic waves in hard rock masses (e.g. granite) have lower amplitudes than those that travel through soft ground such as sediments and so a building constructed and founded on hard rock is less likely to be damaged. As such a lower magnitude earthquake affecting structures founded on softer sediments may ultimately cause more damage than a higher magnitude earthquake affecting structures founded on hard rock.
Further to this, sediments tend to undergo a process known as liquefaction during earthquakes which makes them behave as a liquid rather than a solid meaning they are very poor at supporting the load imposed by the building (they lose the majority of their bearing capacity) making it even more probable that the building will be damaged.
The construction techniques employed in the area and the enforcement of applicable construction codes or standards will affect how destructive an earthquake is (earthquake resistant designs will obviously reduce the damage caused by seismic waves, on the other hand, in countries or areas where poor building practices are followed - e.g. insufficient steel reinforcement in concrete, the use of cheap or poorly sourced aggregates which reduce the strength of concrete or the construction on poor founding materials without the requisite foundation engineering will all act to increase the damage caused by earthquakes).
Low intensity urban use refers to land or spaces in urban areas that are utilized in a way that generates minimal activity or density. This typically includes uses such as parks, small-scale residential areas, or single-story commercial establishments, which have a lower impact on infrastructure and resources compared to high-intensity uses like high-rise buildings or large shopping centers. Such areas promote a quieter, less congested environment and can enhance quality of life by providing open spaces and reducing urban heat.
Only if your entire walk is in the same straight line. Otherwise, no.Example:Start anywhere on the track at the high-school football field, and walk all the way around it.The distance you walk is 1/4 mile. Your displacement is zero, because you're now standingexactly where you began.
An experiment was conducted to investigate the effects of temperature on plant growth. Researchers divided plants into three groups, exposing each group to low, moderate, and high temperatures for a month. Results showed that plants in the moderate temperature group exhibited the highest growth rate, while those in extreme conditions (both low and high) showed stunted growth. This suggests that optimal temperature is crucial for maximizing plant growth.
Being creatures of acute hearing sense, they particularly hate high intensity sounds that are beyond the hearing level of the human ear. Supersonic sound emitters can accomodate this.
Sea contain very huge quantity of water. It takes lot of heat to raise the temperature of water. The land gets heated easily. In that case the hot air goes up. It is replaced by the relatively cool air from the sea. So the temperature near sea remains moderate.
A magnitude of 8.0 earthquake could be classified as a low intensity by descriptions of damage to buildings and terrain. The intensity is often greatest near the earthquakes epicenter.
An 8.0 magnitude earthquake is actually considered a very high intensity earthquake on the Richter scale. It can cause significant damage and devastation, depending on factors such as depth, proximity to populated areas, and local geology. Earthquakes above magnitude 7.0 are generally classified as major earthquakes.
a magnitude-8.0 earthquake can be classified as a low intensity earthquake because depending on where it occured, is realllyyy depends on how many people felt it and how bad it affected them by damaging things
Earthquake intensity is measured using the Modified Mercalli Scale. That is basically a 'subjective' scale (as opposed to the Richter scale, which measures magnitude), because intensity is measured by the impact is is reported to have on people and their property, as reported by them. So a big earthquake like 8 on the Richter scale can have a low intensity if it happens in an area where few people live. A small earthquake can be high-intensity if it happens in a crowded area with many ramshackle houses.
A low earthquake is 1-3 magnitude, a medium earthquake is 4-6 magnitude and a high earthquake is 7+ magnitude.No. A 7.0 magnitude quake would be considered a "major" quake.Here is the scale of earthquake magnitude classes:ClassMagnitudeGreat8 or moreMajor7 - 7.9Strong6 - 6.9Moderate5 - 5.9Light4 - 4.9Minor3 -3.9
the intensity was high reaching an 98 ftTsunami
The measure of energy released by an earthquake depends on its magnitude. If its a high magnitude earthquake, there is a lot of energy. If there is a low magnitude, then there is little energy.
Intervals
An earthquake's magnitude can go as high as 10 or above on the Richter scale. Magnitude 10 earthquakes are extremely rare and are considered to be the strongest earthquakes ever recorded. The majority of earthquakes are of lower magnitude, with the average being around magnitude 4.
Magnitude 7.0 on a scale that starts with 1 and exponentially goes as high as needed.
around 20m high [66ft] and an 9 magnitude earthquake started it.
The Earthquake in haiti was a magnitude 7.0 earthquake, following some very severe aftershocks including a magnitude 6.1 aftershock. This was the largest earthquake ever revocorded and had the largest aftershock also recorded