spray zone is the rocky intertidal zone, also called the super tidal zone, is only covered by water during strong storms.
The topmost region where the marine ecology and terrestrial ecosystem converge is known as the Spray Zone. It is a transitional area, and the breadth and height vary from one location to the next. In the image above, a rock with a few weakly growing terrestrial plants meets a pine forest. The water is close to the bottom of the grey rock wall.
The organisms that dwell in the Spray Zone must be resilient to desiccation (drying out), salt spray, wind, and sporadic surf action. The terrestrial plants that you can see growing between the pine forest and the rock can withstand salt and set roots in fissures and fractures where soil has been trapped and stabilized. Low species diversity can be seen in this area. Do you recall the dominant organism in the spray zone? Let's get to know this plant, hint.
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Canal irrigation is when people use canals to transport water to places that need to be supplied with water.
Answer: Individuals can help in the earthquake disaster by 3 rules. The first rule is looking out for there neighbor if they see that they are stuck within the rubble of the earthquake . The second rule would to get yourself and your family out of the Quake zone. The third rule is always helping in a dire need like this one here if you are not able to help then please provide supplies to the teams that are willing to go searching for people. A community can not thrive on one man or woman they need all arms say if your home was destroyed in the quake I would hope your Community would be there to patch you up with there volunteers nobody can stand alone in this quake disaster if you do so then there is no Community .
Air cools as it rises. Water vapor condenses and creates cumulus clouds, when condensation occurs, heat is released and helps create and grow a thunderstorm. Does this answer your question?
Answer:
The answer is Option B: plate tectonics.
Explanation:
Plate tectonics is a theory about the structure of the earth's crust. In plate tectonics, the continents are viewed as a part of a system of rigid lithospheric plates which move slowly over the underlying mantle of the Earth. The model for plate tectonics builds on the concept of continental drift, which is an idea developed during the first decades of the 20th century. In continental drift theory, all the world's continents were once joined into a land mass that geologists have called Pangea during the late Paleozoic and early Mesozoic eras. It began to break up about 175 million years ago. In the beginning in the late Triassic, the continents began to break up with Laurasia comprising with what is North America and Eurasia and Gondwanaland which was South America and Africa, India, Arabia, Antarctica, and Australia. The shift in plates and their movement create mountain ranges and continents form and move to different latitudes that change the climate as these land masses moved.
