Answer:
<u>Rising and falling of tides, Winds and thermohaline circulation in oceans.</u>
Explanation:
- As oceanic mass is always defined as a body of water which has commonly formed with the chemical and physical properties. Like temperature salinity and common water mass in the world are Atlantic bottoms, Deepwater basins.
- Depth of the oceanic water can be measured through the salinity or dissolved salt content in water, this affects the amount of freshwater in oceans. Deeper zones of water bodies are found near the trenches and valley bottoms.
- Winds are responsible for raising and falling of tidal waters in oceans and movement of currents produced in water masses affects the direction and flow of water bodies.
- Winds have a direct impact on the ocean warm water upwelling and other factors being the flow of debris etc.
Answer:
<em>Seismic Gap</em>
Explanation:
Seismic Gap<em> is a kind of an active fault that has not suffered with any of the significant earth-quaked from a long duration of time.
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And Seismic Gap is the lack of large as well as big earthquakes in a particular place with a tectonic front. It is also an active fault which generally becomes the reason for other earthquakes.
Plz add more deatils im very confusrd i still look forward to helping yoh though
Answer:Fossil records
Explanation: fossil records are records which contains or provides proofs of the existence of man and the level of evolution which has taking place millions of years ago. Fossil record are archeological records which are obtained from the layers and strata of rocks, archeological records such as fossil records tend to contain components of the organic materials or organic make up of early,primitive or ancestral organisms though which study is conducted to determine diversity and evolution.
Answer:
WagonR use Fossil evidence to support his continental drift hypothesis the Fossil of this organism are found on less that are now for apart groups and rock deposits left by insteon Glacier are found today on different continents very close to the equator
