What best describes the manner in which you, as a BLS provider, will activate a response for higher levels of care?

The ways in which BLS providers activate higher levels of care vary  activation is usually defined by an emergency response protocol . To be an effective BLS provider, know and understand your protocols on calling for additional help.

Explanation:

The BLS certification is practically indistinguishable from a CPR class yet it is at last outfitted towards human services suppliers. BLS regularly represents Basic Life Support as opposed to Advanced Life Support. Fundamental Life Support signifies level consideration in which patients will get in a crisis. Therefore, the creators of the rule changed the suggestion from a pressure ventilation proportion of 15:2 to 30:2 for grown-ups until a propelled aviation route is set up, and 15:2 for two-rescuer CPR controlled to newborn children or youngsters.

As a BLS provider, I would activate a response for higher levels of care by calling for more help and by following the emergency response protocol.

Explanation:

answer; collective security;

the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)