Hi, let us know what your list of countries is!
In the meantime, I will give you some information, hopefully it will help:
In constitutional monarchies the Head of state, the monarch is only ceremonial. this includes for example all the European monarchies, all the countries in which the British Monarch is the head of state and Japan.
Also, in parliamentary systems the head of state, the president is also ceremonial. This includes The central European democracies (Germany, Austria) and India and Pakistan)
Answer: Tropical Rain-forests
Explanation:
Tropical Rain-forests specifically those in Central Africa, Latin America and South-East Asia are considered the most diverse areas in the world with over half of animal species in the world as well as countless fauna calling these areas home even these forests cover less than 7% of the Earth's land mass.
For this reason Tropical Rain-forests are usually called the Cradle of life/biodiversity and surpass any other environment when it comes to biodiversity. Even the second which are Coral Reefs are known as Tropical Rain-forests of the sea which is a nod to just how diverse these forests are.
It’s would all just be land-
-Why idk
Answer:
Falso.
Explicación:
América está más lejos del Polo Sur que del Polo Norte porque América está ubicada en el hemisferio norte, que está más cerca del polo norte. América está presente en el lado norte del ecuador, mientras que el polo sur está ubicado en el sur del ecuador, lo que indica que América está más cerca del polo norte, mientras que más lejos del polo sur, por lo que la afirmación de la pregunta es falsa.
On the West coast of North America, the coast ranges and the coastal plain form the margin. Most of the land is made of terranes that have been accreted onto the margin. In the north, the insular belt is an accreted terrane, forming the margin. This belt extends from the Wrangellia Terrane in Alaska to the Chilliwack group of Canada.
A rupture in Rodinia 750 million years ago formed a passive margin in the eastern Pacific Northwest. The breakup of Pangea 200 million years ago began the westward movement of the North American plate, creating an active margin on the western continent. As the continent drifted West, terranes were accreted onto the west coast. The timing of the accretion of the insular belt is uncertain, although the closure did not occur until at least 115 million years ago.Other Mesozoic terranes that accreted onto the continent include the Klamath Mountains, the Sierra Nevada, and the Guerrero super-terrane of western Mexico.80 to 90 million years ago the subducting Farallon plate split and formed the Kula Plate to the North. This formed an area in what is now Northern California, where the plates converged forming a Mélange. North of this was the Columbia Embayment, where the continental margin was east of the surrounding areas.Many of the major batholiths date from the late Cretaceous. As the Laramide Orogeny ended around 48 million years ago, the accretion of the Siletzia terrane began in the Pacific Northwest. This began the volcanic activity in the Cascadia subduction zone, forming the modern Cascade Range, and lasted into the Miocene. Events here may relate to the ignimbrite flare-up of the southern Basin and Range. As extension in the Basin and Range Province slowed by a change in North American Plate movement circa 7 to 8 Million years ago, rifting began on the Gulf of California.
