The climate of Ghana is tropical. The eastern coastal belt is warm and comparatively dry, the south-west corner of Ghana is hot and humid, and the north of Ghana is hot and dry. Ghana is located on the Gulf of Guinea
Mexico's location, climate, and physical features can be seen as natural resources, a very important ones. The location gives it a perfect location between the two continents and makes a trading rout, also it's location gives it multiple climate types. The climate makes it a desirable tourist attraction, also in the south and the coastal region on the east it has a lot of rain, the water is one of the most important resources in the world, the rivers are full all over the year so they can be used for producing energy, irrigation, drinking, fishing, while the more central part and the northern part that is arid and very sunny are excellent for getting energy from the sunlight. The physical features also contribute to the tourism, the central plateau made out of volcanic rocks has a fertile soil excellent for agriculture, but it's elevation also makes it very suitable place for human settlements. <span />
Physical properties of a substance are characteristics that can be observed without altering the identity of the substance. Color, odor, density, melting temperature, boiling temperature, and solubility are examples of physical properties. Physical properties can be used to identify a pure substance.
Is this what you need?
Iron ore resource because it is the material of the steels and all its industrial products
<span>There has been a great deal of discussion about the extent to which climate change could influence thermohaline circulation and its turnover processes in the Atlantic. After all, convection at high latitudes could be weakened by anthropogenic (caused by humans) warming of the atmosphere and the accompanying decrease in surface-water density. Additionally the density will decrease as a result of lower salinity in the North Atlantic. Climate change will probably cause an increase in freshwater input through a number of pathways, which will affect convection and thermohaline circulation. One way would be by an increase in precipitation over both the continents and the ocean. Another would be the increase of freshwater run-off from the melting glaciers to the sea. Furthermore, because less ice forms when it is warmer, the salt concentration in the surface water would not be increased as much by this proces</span>
