Answer:
Relative humidity
Explanation:
Relative humidity -
It is the value of the ratio of partial pressure of water vapor to the vapor pressure at the equilibrium stage of water at a particular temperature , is called the relative humidity .
The value of relative humidity depends on the pressure and temperature of the system .
It helps to determine the amount of wet air in comparison to the the amount of water the air can hold to .
Lava flows are the least hazardous of all processes in volcanic eruptions. How far a lava flow travels depends on the flows temperature, silica content, extrusion rate, and slope of the land. A cold lava flow will not travel far and neither will one that has a high silica content. Such a flow would have a high viscosity<span> (a high resistance to flow). A basalt flow like those in Hawai'i have low silica contents and low viscosities so they can flow long distances. Such a flow can move as far away as 4 km from its source and have a thickness of 10 m (Bryant, 1991). These flows can move at rates of several kilometers per hour (Scott, 1989). </span><span>More silica-rich flows can move as far away as 1.3 km from their sources and have thicknesses of 100 m (Bryant, 1991). These flows can move at rates of a few to hundreds of meters per hour (Scott, 1989). If a lava flow is channelized or travels underground in a lava tube then the distance it travels is greatly extended.</span>
By the mid 2030's. You can find it on their website.
Those coordinates fall on Australia.
Aye mate.
Answer: The glacial-interglacial cycle is triggered by changes in Earth's orbit around the Sun, and, as a result, there is approximately 100,000 years between interglacials (or glacials).
Explanation: