Focus
differences in earthquake intensity; differences in demographics at/near the earthquake site
The initial site for respiration is in the lungs, where oxygen is inhaled and carbon dioxide is exhaled. Oxygen enters the bloodstream through tiny air sacs called alveoli in the lungs, where it is then transported to cells throughout the body to support cellular respiration.
The initial site of respiration in humans is the nose or mouth, where air is inhaled and oxygen is taken in. From there, the oxygen travels down the trachea into the lungs where it is absorbed into the bloodstream and exchanged for carbon dioxide.
Energy is stored in rocks adjacent to the site of a future earthquake as elastic potential energy due to the stress and strain built up in the rocks. This stored energy is released suddenly when the rocks undergo sudden movement along a fault line, resulting in an earthquake.
The total amount spent on relief efforts for the Haiti earthquake is difficult to determine exactly as it involves contributions from multiple sources, including governments, non-profit organizations, and individuals. However, it is estimated to be in the billions of dollars over the years since the earthquake occurred in 2010.
differences in earthquake intensity; differences in demographics at/near the earthquake site
Diaphragm
Charleston
The initial site for respiration is in the lungs, where oxygen is inhaled and carbon dioxide is exhaled. Oxygen enters the bloodstream through tiny air sacs called alveoli in the lungs, where it is then transported to cells throughout the body to support cellular respiration.
Initial and annual refresher training
Earthquakes can pressure highly stressed fault lines and trigger subsequent seismic events. If correct, so-called stress triggering theory could help scientists pinpoint areas where earthquakes are imminent. The earthquakes immediately following one earthquake are called aftershocks. Tectonic plates are moving all the time. The aftershocks can occur because the initial earthquake may have moved things into another position. Then the plates will make additional small adjustments (the aftershocks) to release new pressures that the initial earthquake caused between tectonic plates when they moved. The fault line between the plates may become less stable and then later an entirely new earthquake may occur at the same or at a close by site. It is the instability of the tectonic plates left after one earthquake that can cause others.
The initial site of respiration in humans is the nose or mouth, where air is inhaled and oxygen is taken in. From there, the oxygen travels down the trachea into the lungs where it is absorbed into the bloodstream and exchanged for carbon dioxide.
rough E.R.
It will come in a few days because of the earthquake and tsunami
The magnitude 9.0 Japan earthquake in 2011 was not felt in Florida but the waves from the tsunami did reach the coast of Hawaii.You can visit the USGS Did-you-feel-it web site to check if people reported an earthquake in your area.
Energy is stored in rocks adjacent to the site of a future earthquake as elastic potential energy due to the stress and strain built up in the rocks. This stored energy is released suddenly when the rocks undergo sudden movement along a fault line, resulting in an earthquake.
Other than potential bruising at the puncture site, and/or dizziness, there are no complications associated with this test