Wiki User
∙ 13y ago"...human prospect. We are biological and our souls cannot fly free." - Wilson
Wiki User
∙ 13y agoChanges in the electrical tracings may indicate damage to or degeneration of nerve pathways to the brain from the eyes, ears, or limbs. Absence of any activity may mean complete loss of nerve function in that pathway. Other.
Experiment
pre sale activity carried out in new car sales delearship?
7500
Ndbxbxx
Yes. It is the electrical activity that stimulates the mechanical activity.
earthquakes, volcanic activity, landslides, and avalanches.
All boundaries produce seismic activity, however convergent and transform boundaries have the most activity.
No, electrical activity in the heart moves from proximal to distal.
usually it is mountains
The edges of moving crustal plates are often defined by tectonic plate boundaries. There are three main types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where plates collide, and transform boundaries where plates slide past each other. These boundaries are important in understanding the processes of earthquakes, volcanic activity, and mountain building.
Both measure electrical activity -- the ECG in the heart and the EEG in the brain.An EEG is an electroencephalogram and an ECG also known as an EKG is an electrocardiogram. An EEG records brainwave/electrical activity. An ECG records the electrical activity that the heart produces.
maximizing happiness
The symbols used on a map are explained in the legend.
plate boundaries
Earthquakes are produced at all types of plate boundaries: convergent boundaries, where plates collide; divergent boundaries, where plates separate; and transform boundaries, where plates slide past each other. The release of stress along these boundaries can result in seismic activity.
The three types of plate boundaries are divergent, convergent, and transform. At divergent boundaries, tectonic plates move apart, leading to the formation of new crust through volcanic activity. At convergent boundaries, plates collide, causing subduction zones where one plate descends beneath the other, leading to earthquakes and volcanic activity. At transform boundaries, plates slide past each other horizontally, causing earthquakes.