Final answer:
Air pressure decreases with altitude, and the air pressure at the top of Algonquin Peak at 1560 meters would be significantly less than the 760 mm Hg found at sea level. The pressure at Algonquin Peak can be estimated using the altitude-pressure relationship, considering the pressure at higher elevations like Mount Everest.
Step-by-step explanation:
The air pressure at the top of Algonquin Peak, which is approximately 1560 meters tall, would be lower than at sea level due to the decrease in atmospheric pressure with altitude.
At sea level, atmospheric pressure is about 760 mm Hg, and it decreases as the altitude increases. Since Mount Everest at 8848 meters has an air pressure of about 253 mm Hg, we can estimate the pressure at the top of Algonquin Peak by using a proportional relationship between the altitude and pressure change.
If air pressure drops to roughly one-third of its initial value for every 8800 meters climbed, we can calculate the approximate pressure at the elevation of Algonquin Peak. However, it's important to use a more accurate method or data for a precise figure since this is a simplification that assumes constant temperature and gravitational pull.