Answer:
I believe it was droughts or not enough drinking water
Explanation:
The weather most probably arriving at the station is a cool, dry air. This kind of weather matches the characteristics shown in the weather instruments. The dewpoint temperature and air temperature are getting farther apart means that the air is getting dry while the rising air pressure represents a decreasing temperature.
Answer:
The lower rocks are old while the overlying is newer.
Explanation:
- Red sandstone is overlain by a red shale with bedded gypsum sows the age of the rocks. The boundary in the rock bodies for about 1km marks the along the fault displaced the two rocks bodies.
- As 50 meters, thick red sandstone is found it shows the discontinuities in the rocks. The rocks formed at the bottom are oldest and with newer deposits of gypsum.
In July and August, the ITCZ lies well to <u>the</u><u> north of the equator </u><u>over Africa, Asia and Central America before going to south</u> into South America, central Africa and Australia by January and February.
<u>In January the </u><u>ITCZ</u><u> lies about at 15°S over</u><u> South America and Africa.</u><u> The</u><u> ITCZ</u><u> is less mobile over the oceans,</u> where it binds a stationary position just north of the equator.
<h3>What is the ITCZ ?</h3>
The Intertropical Convergence Zone, or ITCZ, is defined as a band of low pressure around the Earth which commonly lies near to the equator. The trade winds of the northern and southern hemispheres meet here, which takes them to the development of frequent thunderstorms and heavy rain.
<h3>What is the characteristics of ITCZ?</h3>
The ITCZ is characterized by low atmospheric pressures, as a result of the upward movement induced by the trade winds convergence. It forms a high atmospheric pressure in the upper troposphere.
Learn more about ITCZ:
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Two of the major approches to study geography are 1.)Systematic Approach &
2.) Regional Approach.