EARTH SCI

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1
ATMOSPHERE
• consists of 78.1% nitrogen, 20.9% oxygen, 0.9% argon, 350 ppm carbon dioxides, and other components
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PERMITS LIFE ON EARTH
• The presence of oxygen and carbon dioxide
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CARBON DIOXIDE
used by photosynthetic organisms, such as plants and algae, to convert the energy from the sun to usable energy through the process of photosynthesis.
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OXYGEN
makes it livable for living organisms including humans for respiration and for our cells to function.
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ATMOSPHERE
protects us from the sun’s radiation
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OZONE OR O3
composed of three oxygen atoms
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OZONE OR O3
In the stratosphere, THIS is abundant in the form of the ozone layer
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OZONE LAYER OR O3
absorbs the ultraviolet wavelengths, and the absorption of this radiation heats up the air.
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SOIL
mixture of minerals, water, air, organic matter, and organisms. It is a living medium—a medium for growth of all kinds of vegetation.
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SOIL
promotes growth for plants by providing nutrients, water, and as a substrate for anchorage of roots
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VEGETATION
produces trees and forests cover, ensures the water and nutrient cycle, and prevents soil and wind erosion.
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SOIL AND VEGETATION
• The soil promotes growth for plants by providing nutrients, water, and as a substrate for anchorage of roots. In return, vegetation produces trees and forests cover, ensures the water and nutrient cycle, and prevents soil and wind erosion
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mutual relationship of the soil and vegetation
makes our planet livable
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HYDROSPHERE
contains all the water on our planet including ice and vapor.
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SEA AND OCEAN
• Nearly three-quarters of the earth’s surface
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OCEAN
houses many species of marine life and diverse mineral resources
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WATER FORMS
They also serve as thermostat and heat reservoir. They also serve as ways for transportation
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four major subsystems.
ATMOSPHERE
GEOSPHERE
HYDROSPHERE
BIOSPHERE
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FOUR MAJOR SUBSYSTEMS
called the “spheres of the Earth.”
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ATMOS - GAS & SPHAIRA - GLOBE OR BALL
ATMOSPHERE COMES FROM THE GREEK WORDS WHAT
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DIFFERENT LAYERS OF ATMOSPHERE
1. TROPOSPHERE
2. STRATOSPHERE
3. MESOSPHERE
4. THERMOSPHERE
5. EXOSPHERE
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TROPOSPHERE
- extends to about 14.5 km above the Earth's surface.
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STRATOSPHERE
The ozone layer that protects the Earth from the Sun's harmful UV radiation is found in this layer
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TROPOSPHERE
It is the lowest layer where the weather forms.
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MESOSPHERE
extends from 50 to 85 km above the Earth's surface.
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MESOSPHERE
It protects the Earth from the impact of space debris.
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THERMOSPHERE
- found 85 to 600 km above the Earth's surface.
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THERMOSPHERE
It has charged particles that are affected by the Earth's magnetic field. The particles create the Auroras or Northern and Southern lights.
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EXOSPHERE
- is the farthest layer.
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EXOSPHERE
It extends to about 10 000 km above the Earth's surface.
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GEO - means ground.
GEOSPHERE GREEK WORD
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GEOSPHERE
includes all the soil, rocks, and minerals present in the crust to the core of the Earth.
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3 LAYERS OF GEOSPHERE
CRUST
MANTLE
CORE
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CRUST
- the outermost layer of the geosphere.
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SILICATE MATERIALS
WHAT DOES CRUST MADE MOSTLY OF
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OCEANIC AND CONTINENTAL CRUST
two different types of crust
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THIN OCEANIC CRUST
lies beneath the oceanic floors is about 5 to 10 km thick.
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THICKER CONTINENTAL CRUST
makes up the continents is about 15 to 70 km thick.
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MANTLE
LIES JUST BELOW THE CRUST
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MANTLE
made mostly of silicate rocks rich in magnesium and iron.
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MANTLE
about 2900 km thick.
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MANTLE
has increasing temperatures at increasing depths.
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BENEATH THE CRUST
the layer with the lowest temperature is the one
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HEAT PRODUCING CORE
- the layer with the highest temperature is found in contact with
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MANTLE
This layer, which is soft enough to flow, causes the plates of the crust to move.
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CORE
has a radius of 3400 km
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CORE
innermost layer of the Earth.
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made up of iron and nickel.
CORE IS MADE UP OF WHAT
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CORE
the source of internal heat because it contains radioactive materials that release energy as they decay into more stable substances.
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• Hydro is a Greek root which means water
HYDROSPHERE GREEK WORD
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HYDROSPHERE
composed of all the water on Earth in any form: water vapor, liquid water, and ice.
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HYDROSPHERE
It is comprised of 97.5% saltwater and 2.5% freshwater. It includes all bodies of water such as oceans, lakes, rivers, and marshes. Clouds and rain TOO
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WATER
on Earth is constantly moving. It moves through the oceans in currents. It can also move from the Earth’s surface to the air by evaporation and then fall back to Earth as precipitation. It even moves into and out of the bodies of organisms
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EARTH ~ WATER: 70% & LAND: 30%
EARTH COMPOSES OF
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BIO - LIFE
BIOSPHERE GREEK WORD
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BIOSPHERE
comprised of all living things. It includes all microbes, plants, and animals.
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BIOSPHERE
- It extends to the upper areas of the atmosphere where insects and birds can be found. It also reaches the deep parts of the oceans where marine organisms can still survive.
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INTERACTIONS OF BIOSPHERE
- Organisms interact with the other spheres to survive. Many organisms need oxygen and carbon dioxide from the atmosphere to carry out life processes. Water, which comprises the hydrosphere, is also important to organisms. Finally, the rocks, soil, and minerals constitute the geosphere also support life.
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SOIL
soil which can be considered as a part of hydrosphere, geosphere, and even biosphere. Since the soil is a complex material made up of air, soil particles, water, and organisms, it underscores that a clear division among subsystems cannot be drawn.
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THICK CONTINENTAL CRUST
makes up the land surface of the Earth and is composed primarily of dense materials such as granite.
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THIN OCEANIC CRUST
5–10 km and is made up of basalt which is less dense than granite.
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CRUST
can be broken down into plates which produce earthquakes when they move along each other.
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OCEANIC RIDGES
• formed at divergent boundaries, where plates move away from each other;
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TRENCHES
formed at subduction zones where plates collide with each other or at convergent boundaries.
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anticline structures.
• When blocks of rock are bent upwards, they form
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SYNCLINES
formed when blocks of rock bend downwards.
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MONOCLINE
slightly bent rock from the parallel undeformed layers forms
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STRIKE-SLIP FAULT
• involves a horizontal movement of blocks of rock and is caused by shear stress.
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REVERSE FAULT
wherein the hanging wall moves upward, is formed by compressional stress.
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NORMAL FAULT
caused by tensional stress it is characterized by the hanging wall moving downward with respect to the footwall.
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FOOTWALL
the one below the fault plane
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HANGING WALL
the block of rock that rests on the fault plane
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DIP SLIP FAULT
• involve the vertical movement of the blocks of rock.
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FAULT
a break in the rock where there is considerable movement on the fracture surface
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JOINT
a break where there is no considerable movement.
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COMPRESSIONAL STRESS
causes rocks to be squeezed to each other.
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TENSIONAL STRESS
pulls rocks apart and shear stress causes rocks to slide opposite each other.
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CONVERGENT BOUNDARY
the plates move or collide to each other.
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DIVERGENT BOUNDARY
When the plates move away from each other
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TRANSFORM BOUNDARY
when plates slide past each other.
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PLATE MOVEMENTS
cause rocks to be deformed due to compressional stress at convergent boundaries, tensional stress at divergent boundaries, or shear stress at transform boundaries. Due to these stresses, rocks experience changes in volume and shape.
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TECTONIC PLATES
• The Earth’s crust is divided into plates, known as
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SOIL EROSION
• happens when the topsoil is removed and leaves the soil infertile. This is caused by wind or flood in an area.
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GLACIAL EROSION
• happens when the ice moves downhill and plucks out chunks of rocks and causes scraping between the ice and the rock.
• Plucking and scraping can lead to the development of other landforms if, for example, the glaciers hit a mountain and erode it.
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WIND EROSION
• happens when light materials, such as small rocks and pebbles, are carried by wind to different places.
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WATER EROSION
• a type of erosion where the water carries the sediments to different parts of the bodies of water such as rivers.
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EROSION
• is the transportation of weathered rocks.
• Agents like running water or rivers, wind, gravity, groundwater, wave currents, and glaciers contribute to erosion.
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BIOLOGICAL WEATHERING
• a process when living things, such as insects and roots of the trees, contribute to the disintegration of rock materials.
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CHEMICAL WEATHERING
a process wherein rock materials are changed into other substances that have different physical and chemical compositions.
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PANGAEA
• According to the Continental Drift Theory proposed by Alfred Wegener, the Earth was once a giant landmass called
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WEATHERING
• Shaping the Earth’s surface involves a geological process called . Weathering is the process of breaking down rocks into smaller pieces called sediments
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MECHANICAL WEATHERING
• is a process wherein rocks are broken down into smaller pieces without changing its chemical composition due to different temperatures and water.
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MELTING POINT
• refers to the temperature at which solid turns into liquid.
• Minerals composed of atoms that are tightly bonded within the crystal structure have high melting points.
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SOLUBILITY
• refers to the ability of a substance to dissolve in a solvent at a specified temperature
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STREAK
• the color of the mineral in its powdered form.
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LUSTER
• the relative differences in the opacity and transparency of a mineral as light is reflected on its surface.
• This describes the 'sparkles' of the mineral surfaces.
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SPECIFIC GRAVITY
• the ratio of the weight of the mineral to the weight of the water with an equal volume.
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HARDNESS
• the measure of the resistance of a surface to abrasions or scratches.
• It is generally measured using Mohs Scale of Hardness.
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CLEAVAGE
• the tendency of the mineral to be split or broken along flat surfaces.
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FRACTURE
• refers to the texture or shape of the mineral’s surface when the mineral breaks into forms other than flat surfaces.
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TENACITY
• refers to the behavior of the mineral under deformation or stress such as cutting, crushing, bending, or hitting.
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CRYSTAL HABIT
• refers to the growth crystal pattern of a mineral as single or aggregated.
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MAGMATISM
• the activity or the motion of the magma.
• Rocks that are subjected to high temperature and pressure melt and become the magma.
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MAGMA
a semi-liquid molten rock mixture that can be found in the lower portion of the crust and the upper part of the mantle.
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intrusive or plutonic rocks
are igneous rocks formed underneath the earth. They are coarse-grained due to the slow cooling of magma allowing crystal growth.
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extrusive or volcanic rocks
are igneous rocks formed on the surface of the earth. They are cooled lava, which are molten rocks ejected on the surface through volcanic eruptions. They are fine-grained due to abrupt cooling on the surface.
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clastic sedimentary rocks
• are made up of sediments from preexisting rocks. When pre-existing rocks are physically weathered, and eroded, they form sediments.
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biological sedimentary rocks
are lithified accumulation of dead organisms.
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chemical sedimentary rocks
are from chemical precipitation. An example is rock salt formed when dissolved salts precipitate from a solution.
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foliated metamorphic rocks
• have layered or banded appearance produced by exposure to high temperatures and pressures.
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non foliated metamorphic rocks
• do not have a layered appearance.
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deposition
• the laying down of sediments to its depositional environment or destination.
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