Landforms and Oceans. Topics Fun Facts Natural Process Ocean Floor Continental/Oceanic Landforms Ocean Shore Zone Movement of Water Conservation Efforts.

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Presentation transcript:

Landforms and Oceans

Topics Fun Facts Natural Process Ocean Floor Continental/Oceanic Landforms Ocean Shore Zone Movement of Water Conservation Efforts / Pollution

Facts about Oceans Area: about 140 million square miles (362 million sq km), ore nearly 71% of the Earth's surface. Average Depth: 12,200 feet (3,720 m). Deepest point: 36,198 feet (11,033 m) in the Mariana Trench in the western Pacific. 4 Main Oceans: Atlantic, Pacific, Indian, Arctic

71% of the Earth is Water

Pacific Ocean Fraction of world ocean: 48% Average depth: 13,740 feet (4,188 m)

Atlantic Ocean Fraction of world ocean: 28% Average depth: 12,254 feet (3,872 m) Deepest point: 28,374 feet (8,648 m) in the Puerto Rico Trench

Indian Ocean Fraction of world ocean: 20% Average depth: 12,740 feet (3,872 m) Deepest point: 25,344 feet (7,725 m) in the Java Trench

Arctic Ocean Fraction of world ocean: 4% Average depth: 3,407 feet (1,038 m) Deepest point: 17,881 feet (5,450 m) in the Eurasian Basin

Natural Process that affect Oceans and Land Constructive/Destructive Weathering Erosion Deposition Landslides Volcanic Eruptions Earthquakes Floods

Constructive: process that create landforms Destructive: process that destroy landforms.

Weathering Weathering is a general term used to describe processes that break down rocks at or near the surface of the earth. Weathering can be either physical or chemical. These processes cause the surface of the earth to dissolve, decompose, and break into smaller pieces. Water is an important cause of weathering. Plants cause weathering when roots break apart rock. Changes in temperature can break rock, as well as ice forming inside cracks in the rock causing it to break even more. Anything that causes rocks to wear down or break apart is a cause of weathering.

Erosion Erosion is the movement of sediments and soil by wind, water, ice, and gravity.

Deposition Deposition is the dropping, or depositing, of sediments by water, wind, or ice. Deposition builds up new land on Earth’s surface, like a delta at the end of a river or the pileup of a sand dune in the desert. Shells on the beach are deposition by ocean waves.

Landslides Landslides are mass movements of land due to gravity. Landslides can cause buildings to fall, or power and gas lines to break. Landslides even occur on the continental slope in the ocean.

Volcanic eruptions Volcanoes are mountains with openings in Earth’s crust through which magma, gases, and ash reach Earth’s surface. When the magma erupts from the volcano the top of the mountain can be changed, either built up or exploded off. The lava and ash can destroy forests and bury fields. Volcanic eruptions can even change Earth’s weather patterns. Volcanic eruptions also occur under the oceans; these volcanoes that are built up are called seamounts. If the seamount rises above the ocean surface it is called a volcanic island (for example Hawaii or Japan).

Earthquakes Earthquakes are vibrations on Earth’s surface caused by sudden movement in Earth, often along a fault, a break in Earth’s surface. Some earthquakes cause little damage and some cause a lot of damage. Large earthquakes can cause landslides. Earthquakes under the ocean can cause huge waves, called tsunamis that destroy land and cause great damage if they come ashore.

Floods Floods occur when a large amount of water covers land that is usually dry. When the flood occurs, rapid erosion can take place and move soil and sediments away. When the flood recedes, new sediment is left behind and can build up rich soil deposits.

Ocean Floor Continental Shelf Slope Mid-Ocean Ridge Rift Zone Trench Ocean Basin

Continental shelf Surrounding all continents is a shallow area of land that slopes down from the shore into the ocean. The part of the continent located under the water is known as the continental shelf. The width of the shelf varies around the edges of the continent. In some places the shelf is shallow in other it becomes deep, but is not the deepest part of the ocean.

Continental Slope The steep slope where the continental shelf drops to the bottom of the ocean floor. The depth of the ocean increases greatly here.

Mid Ocean Ridge Underwater volcanic mountains. On the bottom of the ocean, there is a central ridge, or mountain range, that divides the ocean floor into two parts.

Rift Zone A narrow trench in the center of the highest part of the mid ocean ridge.

Deep Sea Trenches Steep-sided canyons and deep narrow valleys in the bottom of the ocean. The deepest part of the oceans May exceed 10,000 m deep (30,000 feet, or nearly 5 miles) Deepest is Mariana trench in Pacific Ocean (more than 11,000 m or 33,000 ft) They are deeper than any valley found on land.

Ocean Basin The ocean floor on either side of the mid- ocean ridge. Made up of low hills and flat plains. Deepest part of the ocean floor, except for trench depths.

Continental and Oceanic Landforms Canyon Valley Volcano Mountain range Low Hills or plains Trench Rift Seamount Mid-Ocean Ridge Ocean basin and plains Compare the movement of water by waves, currents, and tides.

Movement of Water Waves Currents Tides Explain how waves, currents, tides, and storms affect the geologic features of the ocean shore zone (including beaches, barrier islands, estuaries, and inlets).

Waves Waves- the repeated movement of water. Crest- highest part Trough- lowest part Caused by winds blown across the surface of water· A wave changes shape when it reaches the shore. As the top of the wave curls over it forms a breaker. Tsunamis are caused by underwater earthquakes, volcanic eruptions, or landslides

Currents Currents- flowing streams of water that move continually through the ocean in a specific direction. Surface currents- causes by the movement of earth and by the force and direction of wind. Warm surface currents- driven by Earth’s rotation from the tropics to higher latitudes Cold surface currents- driven by Earth’s rotation from the polar latitudes toward the equator.

Warm Currents dark blue Cold surface currents light blue

Tides Tide- the regular rise and fall of waters in the ocean and seas Caused by a pull of the Moon’s gravity on Earth Tides rise and fall about twice a day. High tide- water is at its highest Low tide- water is at its lowest Neap tide-The Sun and Moon pull in different directions. First Quarter and Third Quarter Moon Phases –Little difference between high and low tides. Spring Tide-The Sun and the Moon are in line pulling on Earth in same direction. New and Full Moon phases. –Higher high tides, and lower low tides

Ocean Shore Zone Beaches Barrier Islands Estuaries Inlets Compare continental and oceanic landforms.

Barrier Island · Islands with sandy beaches are called barrier islands. · These barrier islands are naturally occurring and function to protect the mainland from the effects of waves on its shore. · As the waves deposit sand on the beaches, the shapes of the barrier islands change. · Currents can move the sand from one end of the island to the other.

Pawley’s Island

Estuaries · All rivers flow into the oceans. · The area where a river meets the ocean is known as an estuary. · Estuaries have a mixture of freshwater and saltwater. · Waves can deposit sand in the estuaries. · At high tide, ocean water brings in sediments and sea life that feed and nourish life in the estuary.

Beaches The shoreline, or coast, is the area where the land meets the ocean. Shorelines made of sand are called beaches. Waves that come in at an angle can move the sand. Currents, called longshore currents, along the shoreline can move sand from one location to another. Tides can bring in sand, shells, and ocean sediments at high tide and leave them behind when the tide goes out. Storms can cause wave action that removes sand from beaches.

Inlets Inlets are the water-filled spaces between the barrier islands. As the tides change, the amount of water in the inlet will change. Ocean currents and storms can change the shape of an inlet opening.

Conservation and Pollution What is it? How does it work? Why is it important? Explain how human activity (including conservation efforts and pollution) has affected the land and the oceans of Earth.

Conservation Efforts The wise use of natural resources is called conservation. Human activities that help to keep the natural resources of Earth available and clear of pollution are conservation efforts. Some efforts involve everyone trying remember and use the 3 R’s: Reduce, Reuse, Recycle. Other efforts involve trying to save the land and oceans through clean-up projects, installing things to help prevent erosion along shorelines. Beach re-nourishment projects help to restore sand on beaches. Planting trees, bushes, or grass is a way to improve air quality as well as keep erosion from carrying away soil.

Pollution Pollution is anything that harms the natural environment. When the taking or using of natural resources causes harm to Earth’s air, water including oceans, or land, then the human activity has caused pollution. Oceans are rich in food, minerals, and other resources and can be easily polluted. Human activities can also harm the land and oceans causing resources to be polluted or destroyed. Careless dumping of trash on land or in oceans smoke and fumes from burning fuels pollutes the air oil spills harm the ocean and can cause life there to be killed.