23 5 Oceans
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Oceans are comprised of saltwater with varying salinity levels. The continental shelf is a shallow, sloping plain along coastlines that transitions into a continual slope further from shore, cut through in places by trenches. Pressure increases and light/temperature decrease with depth in the ocean, while surface currents are driven by wind patterns and deep currents are caused by density differences in water. Waves erode coastlines through hydraulic action and abrasion, carrying sediment that is deposited to form beaches through longshore drift.
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- Waves are formed by wind across ocean surfaces, with larger waves forming in storms and tsunamis from undersea events.
- Coastal landforms like sea arches, stacks, and barrier islands are formed through erosion from wave action.
Earth’S Ocean
The document provides an overview of key facts about Earth's oceans:
- Oceans cover 71% of the planet and are composed primarily of sodium chloride, making ocean water undrinkable.
- Ocean currents are driven by global winds and the Coriolis effect, influencing climate by transporting warm and cold waters.
- Deep ocean currents are driven by differences in water density from temperature and salinity, not winds at the surface.
Class 7 ch 5 water-pdf
This is PPT of class -7 ,Geography, Chapter -5, Water
Reference book is NCERT, .
This is useful for teachers who teach in CBSE and Chhattisgarh board.
so download and use online and offline teaching.
Erosion and Deposition
TRUE OR FALSE: The Earth’s surface has stayed the same for thousands of years
FALSE: the Earth’s surface is always changing
EXAMPLE
EROSION & DEPOSITION
EROSION
Is the process by which natural forces move weathered rock and soil from one place to another.
Sediment – material moved by erosion .
DEPOSITION
Occurs where the agents of erosion lay down sediment.
Mass Movement
Any one of several processes that move sediment downhill.
Different types of Mass Movement
Landslide
- occurs when rock and soil slide quickly down a steep slope.
Different types of Mass Movement
Mudflow
- mudflow is a rapid downhill movement of a mixture of water, rock, and soil.
Different types of Mass Movement
Slump
- a mass of rock and soil suddenly slips down a slope.
Different types of Mass Movement
Creep
- very slow downhill movement of rock and soil.
Water Erosion
Rills and Gullies
Rills
- tiny grooves in the soil.
Gully
- a large groove , or channel, in the soil that carries runoff after a rainstorm
Streams and Rivers
Stream
- a channel along which water is continually flowing down a slope.
River
- a large stream
Amount of Runoff
In an area depends on five main factors:
1st – amount of rain
2nd – vegetation
3rd – type of soil
4th – shape of the land
5th – how people use the land
Erosion by River
Through erosion, a river creates a waterfalls, flood plains, meanders, and oxbow lakes.
Waterfall
May occur where a river meets an area of rock that is very hard and erodes slowly.
Flood plain
Flat, wide area of land along a river.
Meander
A loop like bend in the course of the river
Oxbow lake
A meander that has been cut off from the river.
Deposits by River
Deposition creates landforms such as alluvial fans and deltas. It can also add soil to a river’s flood plain.
Alluvial Fans
A wide, sloping deposit of sediment formed where a stream leaves a mountain range.
Deltas
Sediment deposited where a river flows into an ocean or lake.
Groundwater Erosion
Groundwater can cause erosion through a process of chemical weathering.
Stalactite – hangs down from the roof of a cave.
Stalagmite – pointed piece of rock that sticks u p from the floor.
How Water Erode and Carries Sediment
Most sediment washes or falls into the river as a result of mass movement and runoff. Other sediment erodes from the bottom or sides of the river.
Abrasion- is the wearing away of rock by grinding action.
- occurs when particles of sediment in flowing water bumped into the steam again and again.
Erosion and Sediment Load
A river’s slope, volume of flow, and the shape of its trembled all affect how fast the river flows and how much sediment it can erode.
Slope
Is the amount the river drops toward sea level over a give distance.
Volume of Flow
A river’s flow is the volume of water that moves past a point on the river on a given time.
Streambed Shape
Affects the
Surface current meteo group 5
Surface currents are horizontal movements of water near the ocean surface that can reach depths of hundreds of meters. They are primarily driven by winds and the Coriolis effect. Additional factors like continental shapes, temperature and salinity gradients also influence ocean currents. Warm currents transport equatorial waters poleward while cold currents move polar waters toward the equator. Upwelling and downwelling occur when surface waters are moved away from or toward coastal regions.
Ocean Water and Currents PPT LESSON
Explore the dynamic world of ocean water and currents with this engaging PPT lesson by IAS Next. Dive deep into the intricate mechanisms governing ocean currents, their impact on climate, marine life, and more. Gain insights into the significance of understanding oceanic processes for various competitive exams, including IAS. This comprehensive presentation combines visuals and informative content to make learning about oceanography both educational and enjoyable.
waves and currents
geological action of waves and currents, and the features that is morphological features forming as a result of its action is explained
Chapter 9- water erosion
This document provides an overview of various types of water erosion and movement. It discusses factors that influence runoff and how rills and gullies are formed through water erosion over time. It also summarizes different stages of stream development from young to mature to old streams and how river systems are formed. Groundwater movement and the formation of wells, springs, caves, sinkholes and geysers are also summarized briefly.
ocean water
This document discusses several topics related to oceanography: 1) It describes how ocean currents are influenced by winds, the Coriolis effect, and continents. 2) It explains how density currents cause ocean water below the surface to circulate. 3) It defines parts of a wave and describes how waves are created by wind energy and gravitational forces.
Plates of the earth
actually thanks for the slideshare !!!!! i took a little help from yhis website so i log in to this to help others
How waves, tides and currents are formed ?
This document discusses waves, currents, tides and how they are formed. It explains that waves are created by energy passing through water and are caused by wind or disturbances like storms, earthquakes or volcanic eruptions. Currents are driven by factors like wind, density differences, gravity and tides. There are surface currents in the top layers and deep currents caused by temperature and salinity differences. Tides are caused by the gravitational pull of the moon which bulges the Earth's oceans on the side facing the moon and opposite the moon, creating high and low tides as the Earth rotates.
Ocean floor topography
This document discusses various topics related to ocean floor topography including continental margins, oceanic divisions, submarine canyons, ocean currents, the Coriolis effect, tidal currents, ocean waves, and how waves can cause coastal erosion. It describes key features of passive and active continental margins and how the ocean floor transitions from the continental shelf to deeper ocean basins and trenches.
a7kXImOPZCYbj5962SdaKwzrsdGjXqauxsBW6lJn (1) (1) (1) (1).pptx
This presentation discusses the causes and types of ocean currents. It begins by defining ocean currents as masses of ocean water that flow from one place to another. The main causes are then outlined as solar heating, wind, gravity, salinity, temperature, the Coriolis effect, and underwater earthquakes. The presentation goes on to describe different types of currents including surface vs deep currents, upwelling vs downwelling currents, and western vs eastern boundary currents. Western boundary currents are faster and move warm water poleward while eastern boundary currents are slower and transport colder water toward the equator.
Processes of River
The document summarizes various river, wind, and glacier processes. It discusses the three main types of processes that occur in rivers - erosion, transportation, and deposition. Erosion involves wearing away material from the river bed and banks. Transportation moves eroded material downstream, gradually reducing its size. Deposition occurs when energy levels drop and material is dropped from the river. Similar processes of erosion, transportation, and deposition occur for wind and glaciers.
Ocean currents ppt cscope
Ocean currents are influenced by factors like the sun, wind, Coriolis effect, and gravity. Warm currents generally flow away from the equator while cold currents flow toward it. The sun heats water in the tropics, making it less dense and causing it to rise and flow poleward. Wind pushes surface water and the Coriolis effect causes it to curve, forming giant circular gyres in ocean basins. Examples are the Gulf Stream, which brings warmer water to northwest Europe. Upwelling occurs when offshore winds pull surface waters, causing deeper cold water to rise.
Unit iv-chapter-16-ocean-circulation
An ocean current is a continuous movement of ocean water generated by forces acting on the ocean. There are two main types of ocean currents: surface currents, which are parts of large rotating systems influenced by factors like wind and Coriolis effect; and deep water currents, also called thermohaline circulation, which are density driven and move more slowly in a north-south direction. Ocean waves are the forward movement of water caused by oscillation, with characteristics like crest, trough, wavelength and period. Coastlines are shaped by erosion processes from ocean waves and currents, forming features such as wave-cut cliffs and platforms.
Chemical and physical features of seawater and the
The document summarizes key aspects of ocean water including its unique properties, states, heat absorption, role as a solvent, and composition of seawater. It also discusses ocean circulation patterns driven by wind and thermohaline circulation, as well as waves and tides. Surface currents are formed through wind patterns and deflected by the Coriolis effect, while deep circulation is driven by water density variations from temperature and salinity changes.
The Water Cycle
The water cycle describes the continuous movement of water on, above, and below the Earth's surface. Water can exist as a solid, liquid, and gas and is constantly changing forms as it moves through this cyclic process. The sun provides energy for evaporation and precipitation to occur as water circulates between bodies such as oceans, atmosphere, and land through processes like evaporation, condensation, precipitation, and runoff. This cycle is crucial as it replenishes and purifies the water supply on Earth.
6th Grade Chapter 16- water cycle
The document discusses the water cycle and various components of Earth's hydrosphere. It explains that water evaporates from bodies of water due to the sun's energy, rises into the atmosphere as vapor, cools and condenses to form clouds, and falls back to Earth as precipitation. The cycle involves surface water runoff into streams, rivers and oceans. Groundwater is water that soaks into the ground and collects in soil and rock pores. Tides are caused by the gravitational pull of the moon and sun, forming bulges in the oceans.
Landforms along rivers
Weathering and erosion shape landforms through natural processes. Running water, ice, wind, and gravity cause weathering that breaks down rocks. Erosion then transports eroded material. This degradation and deposition forms many landforms along rivers, including headwaters, valleys, canyons, rapids, waterfalls, meanders, oxbow lakes, floodplains, natural levees, river mouths, and deltas.
Similar to 23 5 Oceans (20)
Works Of The Sea And Development Of The Related Landforms For Presentation
Works Of The Sea And Development Of The Related Landforms For Presentation
a7kXImOPZCYbj5962SdaKwzrsdGjXqauxsBW6lJn (1) (1) (1) (1).pptx
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Chemical and physical features of seawater and the
Chemical and physical features of seawater and the
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24 1 the atmosphere
The atmosphere is composed primarily of nitrogen, oxygen, and other gases that surround the Earth. It protects the Earth from harmful rays from the sun while trapping heat, and provides conditions suitable for life. The atmosphere consists of four main layers - the troposphere, stratosphere, mesosphere, and thermosphere - with decreasing air pressure and density at higher altitudes. The stratosphere contains the ozone layer which absorbs UV rays.
Ch 18 5 sources of light
There are several sources of light described in the document. Incandescent light bulbs produce light as electrons flow through a heated filament. Fluorescent lights emit light by causing a phosphor to emit photons through a series of collisions that change wavelengths into visible light. Laser light is a beam of coherent light emitted when excited atoms release photons; it maintains a constant intensity. Sodium-vapor lights ionize gas mixtures in a bulb, causing sodium to emit light as electrons move between energy levels upon heating.
Ch 18 4 colors
White light separates into colors when passing through a prism due to different wavelengths refracting at different angles, called dispersion. An object's color depends on both its composition and the color of light illuminating it. Primary colors are red, green, and blue, which when mixed in different amounts can create all other colors. Secondary colors are cyan, yellow, and magenta, which are combinations of two primary colors. Complimentary colors of light combine to form white light. Primary pigment colors are cyan, yellow, and magenta.
Ch 18 2 electromagnetic spectrum
The electromagnetic spectrum includes various types of waves ranging from radio waves to gamma rays. Radio waves are used for radio, television, radar, and microwaves, which can be used to cook food. The electromagnetic spectrum also includes infrared rays, visible light, ultraviolet rays, X-rays, and gamma rays, each with their own characteristics and applications such as medicine, agriculture, imaging internal structures, and cancer treatment.
Ch 18 1 electromagnetic waves
Electromagnetic waves consist of changing electric and magnetic fields that can travel through matter or empty space, transferring energy. They are produced when electric charges vibrate or accelerate and all travel at the same speed in a vacuum, as measured by Michelson. While wavelength and frequency vary inversely, electromagnetic radiation behaves both as waves and particles, with intensity decreasing with distance from the source as photons disperse.
15.1 notes
The document discusses different forms of energy including kinetic energy, which depends on an object's mass and speed, and potential energy, which can be gravitational or elastic. It provides examples of calculating kinetic energy for a flying bird and gravitational potential energy for a diver. The document also categorizes the main forms of energy as mechanical, thermal, chemical, electrical, electromagnetic, and nuclear, and notes that nuclear power plants use nuclear energy to generate electricity by splitting atoms to heat water and spin turbines.
11 3 acceleration section
Acceleration is defined as a change in an object's speed or direction over a period of time. It can be calculated by taking the change in velocity (final velocity minus initial velocity) divided by the time taken. Acceleration is measured in meters per second squared. Slowing down is considered deceleration or negative acceleration. Constant acceleration results in a steady change in velocity at the same rate over time and is represented by a straight line on a graph where the slope equals the acceleration.
3.1 notes
The document discusses the differences between solids, liquids, and gases. Solids have a definite shape and volume, do not compress, and do not assume the shape of their container. Liquids have no definite shape but a definite volume, cannot be compressed, and assume the shape of their container. Gases have no definite shape or volume, can be compressed, and assume the shape of their container. The kinetic theory states that particles in all matter are in constant motion and the behavior of gases is due to the fast, random motion of particles which overcome attractive forces between them.
2.2 notes
Physical properties are characteristics that can be observed or measured without changing a substance's composition, and include viscosity, conductivity, malleability, hardness, melting point, boiling point, and density. These properties can be used to identify materials, determine which are best for specific uses, and separate mixtures through processes like filtration and distillation.
2.1 notes
This document classifies matter as either pure substances or mixtures. Pure substances are uniform throughout and can be elements, which contain only one type of atom, or compounds, which contain two or more elements joined together. Mixtures are not uniform and can be either heterogeneous, with noticeably different parts, or homogeneous, with evenly distributed parts. Mixtures are further classified as solutions, suspensions, or colloids based on the size of particles in the mixture.
2.2 notes
Physical properties are characteristics that can be observed or measured without changing the composition of a substance. Some key physical properties include viscosity, conductivity, malleability, hardness, melting point, boiling point, and density. Physical properties can be used to identify materials, determine which are best suited for specific uses, and separate mixtures using techniques like filtration and distillation.
1.2 notes
The document outlines the scientific method which involves making observations, conducting research to form a hypothesis, testing the hypothesis through controlled experiments and data collection, drawing a conclusion, and potentially developing a new theory. It also discusses key aspects of the scientific method including forming testable hypotheses with manipulated and responding variables, controlling outside factors, revising hypotheses not supported by evidence, and how scientific laws summarize patterns in nature while theories aim to explain them. Scientific models are also mentioned as tools to visualize complex concepts.
How to make a good graph
To make a good graph, include a title, labels for the axes, and consistent scales. The x-axis should include the independent variable like time, while the y-axis includes the dependent variable measured. Data points can be connected with a smooth curve to show patterns, and less ink allows easier readability. Key details like calculations or uncertainties should be indicated on the graph as needed.
1.4 notes
Scientists use various visual formats like tables, line graphs, bar graphs, and circle graphs to organize and present data. Tables relate variables and display values in rows and columns. Line graphs show changes over time or between variables with slope indicating relationships. Bar graphs compare measurements, while circle graphs illustrate proportions of a whole.
1.3 notes
Scientific notation and SI units are used in measurement to help scientists communicate measurements clearly across countries. The basic SI units include meters, kilograms, seconds, amperes, moles, candelas, and kelvins. Derived units are calculated from the basic units, such as newtons from kilograms and meters/seconds. SI prefixes modify the scale of units, from centi to giga. The precision of calculations is limited by the measurement with the fewest significant figures. Temperature in kelvins is calculated by adding 273 to degrees Celsius.
1.2 notes
The document outlines the scientific method which involves making observations, conducting research to form a hypothesis, testing the hypothesis through controlled experiments and data collection, drawing a conclusion, and potentially developing a new theory. It also discusses key aspects of the scientific method including forming testable hypotheses with manipulated and responding variables, controlling outside factors, revising hypotheses not supported by evidence, and how scientific laws summarize patterns in nature while theories aim to explain them and cannot be proven. Scientific models are also mentioned as helping visualize complex concepts.
Ch 1 1 notes
Science begins with curiosity and uses methods to discover knowledge. It includes natural sciences like physical science, chemistry, physics, earth and space science, as well as life sciences concerning living things. Physical science covers big ideas like space and time, matter and change, forces and motion, and energy.
Ch 26-1 The sun
The document summarizes key aspects of energy from the sun and its atmospheric features. The sun's energy comes from nuclear fusion reactions in its core that convert hydrogen into helium. This outward pressure is balanced by the sun's inward gravitational force, maintaining stability. The sun's atmosphere has three layers - the visible photosphere, the middle chromosphere, and the outer corona containing hot gases that flow out as solar winds. Sunspots, prominences, and solar flares are prominent atmospheric features.
Groups of stars 26.4
Star systems consist of two or more stars held together by gravity, with over half of all stars existing in systems. Star clusters form when stars are born together in the same nebula, allowing their ages to be determined. The three types of star clusters are open clusters, associations, and globular clusters. Galaxies are classified into four main categories: spiral, barred-spiral, elliptical, and irregular galaxies, which can be distinguished by their shapes, presence of spiral arms, and stages of star formation.
Evolution of a star 26 3
Stars form from dense regions in nebulae where dust and gases heat up and contract to form a protostar with enough mass for nuclear fusion to begin. Most stars will spend around 90% of their life as a main sequence star stably fusing hydrogen into helium. A star's mass determines its place on the main sequence, with smaller, cooler red stars living the longest. Lower mass stars eventually become white dwarfs as their cores grow without outward pressure, while higher mass stars explode as supernovae, leaving behind neutron stars or black holes if the core is massive enough for its surface gravity to trap even light.
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