Answer:
i. by water seeping through the ocean floor and welling up into the lake
Explanation:
Oceans the lowest unit of deposition of all continental materials. It is also known that all the water on land drains into the oceans. Oceans receives large volume of fresh water because they are down the gradient and base level of the continent.
It is near impossible for water from oceans to flow landward.
Lake Okeechobee in Florida will empty into the ocean at the Gulf of Mexico. For an exchange of water to occur between these two bodies of water, we must consider infiltration through the ocean floor into the land. Water can seep into pore spaces in form of salt water intrusion which can be carried into the lake body. This is the most reasonable way water from the Gulf of Mexico can move into the lake.
Answer:
Option (C)
Explanation:
Charts and graphs are the most common features that are used in order to show and highlight data in a preferred and simple way. It helps in a clear understanding of any topic, as the charts are comprised of figures and graphs show the relationship between two things. It provides accurate and valuable information. These are also considered to be a simple, meaningful and attractive design and are widely used during the presentation of any topic.
These graphs and charts are made using different colors, and the number of colors are not fixed. It has a wide range of colors.
Thus, the correct answer is option (C).
Answer: Physical maps use color most dramatically to show changes in elevation. A palette of greens often displays elevations. Dark green usually represents low-lying land, with lighter shades of green used for higher elevations. In the next higher elevations, physical maps often use a palette of light brown to dark brown.
Answer:
Conglomerate rock
Explanation:
This is a type of sediment rock that has a coarse-grained texture. It is made up of small pieces of gravel-sized clasts, such as pebbles and cobbles. The mechanism of conglomerate rock formation is by consolidation and lithification.
Conglomerates are found in a variety of sedimentary environments such as, Deepwater marine, Shallow marine, Fluvial, Alluvial, and Glacial environments.
These deep-ocean<span> currents are driven by differences in the </span>water's<span> density, which is controlled by temperature (thermo) and salinity (haline). This process is known as thermohaline </span>circulation<span>. In the Earth's polar regions </span>ocean water<span> gets very cold, forming </span>sea<span> ice.</span>
