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The document describes the key features of the four major oceans: the Atlantic Ocean formed as the Americas spread away from Europe and Africa, features few trenches and island arcs; the Pacific Ocean is the largest and oldest ocean basin with an asymmetrical shape and features the Ring of Fire of trenches, island arcs, and volcanic ranges; the Indian Ocean is similar to the Atlantic but symmetrical around a triple junction and features trenches and island arcs like Java; the Arctic Ocean is the smallest ocean basin almost entirely landlocked except for its connection to the North Atlantic and contains the continental shelf dividing Lomonosov Ridge.
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The document summarizes key aspects of plate tectonics theory, including Earth's structure of a solid inner core, liquid outer core, rigid upper mantle and plates of lithosphere. Plates move due to convection currents in the asthenosphere, and interact at boundaries. There are three main boundary types - constructive where plates diverge and new crust forms, destructive where one plate subducts under another leading to volcanoes and mountains, and conservative where plates slide past each other along faults. Hotspots also cause volcanic chains independent of plate boundaries.
The sea floor
The Earth is made up of four ocean basins - Pacific, Atlantic, Indian, Arctic - which cover 71% of the planet. The ocean floor is composed of tectonic plates that are constantly shifting and spreading at mid-ocean ridges. As new crust is formed at ridges, old crust is destroyed through subduction at trenches. This process of sea floor spreading and plate tectonics explains continental drift over millions of years, from the single supercontinent Pangaea to the current configuration of lands and oceans.
The sea floor
The Earth is made up primarily of oceans that cover 71% of the planet. The oceans are divided into four major basins - Pacific, Atlantic, Indian, Arctic - as well as smaller connected seas. The structure of the Earth includes a dense iron core, swirling liquid outer core, mantle, and thin crust atop the mantle. There are differences between the oceanic crust, made of basalt, and continental crust, made of granite. Plate tectonics explains how the Earth's crust is broken into plates that move over time, causing continents to drift apart.
The sea floor
The Earth is made up of four ocean basins - Pacific, Atlantic, Indian, Arctic - which cover 71% of the planet. The ocean floor is composed of tectonic plates that are constantly shifting and spreading at mid-ocean ridges. As new crust is formed at ridges, old crust is destroyed through subduction at trenches. This process of sea floor spreading and plate tectonics explains continental drift over millions of years, from the single supercontinent Pangaea to the current configuration of lands and oceans.
Physical Features
Latin America is divided into three main regions - Mexico and Central America, the Caribbean, and South America. Mexico and Central America feature mountainous terrain like the Sierra Madre mountains. Central America is an isthmus connecting North and South America crossed by the important Panama Canal. The Caribbean is composed of islands, both volcanic and atop sunken mountains, surrounded by the Caribbean Sea, an important trade route. South America is defined by the Andes Mountains along the western coast and the immense Amazon River basin and rainforest in the center.
Physical Features of Latin America
Latin America is divided into three main regions - Mexico and Central America, the Caribbean, and South America. Mexico and Central America feature mountain ranges like the Sierra Madre mountains. Central America is an isthmus with fertile soil from volcanic activity. The Panama Canal connects the Pacific and Atlantic oceans across the isthmus of Panama. The Caribbean is made up of islands, both large and small. South America features the Andes Mountains along the western coast and the massive Amazon Rainforest basin. Major physical features also include the Atacama Desert in Chile and rivers like the Amazon.
Physical Features Of Latin America
Latin America is divided into three main regions - Mexico and Central America, the Caribbean, and South America. Mexico and Central America feature mountain ranges like the Sierra Madre and a central plateau in Mexico. Central America is an isthmus with fertile soil from volcanic activity. The Panama Canal allows shipping to pass between the Pacific and Atlantic oceans. The Caribbean is made up of islands, both large and small. South America features the Andes Mountains along the west coast and the massive Amazon Rainforest basin to the east.
Physical Features Of Latin America
Latin America is divided into three main regions - Mexico and Central America, the Caribbean, and South America. Mexico and Central America feature mountain ranges like the Sierra Madre mountains. Central America is an isthmus with fertile soil from volcanic activity. The Panama Canal connects the Pacific and Atlantic oceans across the isthmus of Panama. The Caribbean is made up of islands, both large and small. South America features the Andes Mountains along the western coast and the massive Amazon Rainforest basin. Major physical features also include the Atacama Desert in Chile and rivers like the Amazon.
Europa 150201023941-conversion-gate01
The relief in Europe has three main features: young mountain ranges like the Alps, old eroded mountain massifs like the Urales, and vast plains where long rivers flow. The European coasts are irregular with many seas like the Mediterranean and Baltic. There are also numerous islands in the Mediterranean Sea. Rivers in Europe flow into these seas and oceans, with those flowing into the Atlantic and Baltic having abundant flows. The climates in Europe are mainly temperate due to the latitude, with some continental, Mediterranean, oceanic, polar and mountain climates.
Seafloor Features
The document summarizes various seafloor features including:
- The continental shelf, slope, and rise that make up the continental margin. Submarine canyons cut into the continental slope.
- The abyssal plain, the broad, flat deepest part of the ocean.
- Three types of coral reefs: fringing reefs along coastlines, barrier reefs separated from land by lagoons, and coral atolls formed from sunken volcanic islands.
- Mid-ocean ridges and rift valleys formed by sea floor spreading. Other seafloor features include seamounts, guyots, trenches, volcanoes and hydrothermal vents.
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