EALS Midterms PDF
Document Details
Uploaded by GlimmeringParable
Escuela de Sophia of Caloocan, Inc.
Tags
Summary
This document covers the theories about the origin of the universe, the accretion hypothesis, and the layers of the atmosphere. It also discusses different types of rocks and their classifications. The document appears to be study notes or lecture content for an Earth and Life Science course at a tertiary level.
Full Transcript
Earth and Life Science FOUR SUBSYSTEMS OF THE EARTH System - interconnected set of components that WEEK 1 functions. THEORIES ABOUT THE ORIGIN OF THE UNIVERSE...
Earth and Life Science FOUR SUBSYSTEMS OF THE EARTH System - interconnected set of components that WEEK 1 functions. THEORIES ABOUT THE ORIGIN OF THE UNIVERSE How does Earth’s system work? Movement or transfer of matter and energy Big Bang Theory - galaxies increase but not expand because of the expanding universe. Close System - only energy is transferred. Open System - both energy and matter is Singularity - area predicted to be the core of a transferred. black hole with very high temperature and density. LAYERS OF THE ATMOSPHERE Steady State Theory - universe has always been Troposphere Stratosphere expanding. Mesosphere - Universe expands = new stars and galaxies Thermosphere are formed Exosphere Oscillating Universe Theory - universe contract Troposphere - clouds appear after all the energy are used up in expansion. - Lowest layer - “Pulsating theory” The Big Crunch - once the universe reverses and attains the point of singularity, another universe will be born Altitude Temperature ACCRETION HYPOTHESIS Accretion - gradual increase in the size of an Stratosphere - Converting the UV energy to heat object by the build up of matter due to gravity - Ozone layer Homogenous - accreted from materials of same composition after condensation Heterogenous - when Earth accreted during condensation, forming a differentiated planet as it Altitude Temperature grew in size. Mesosphere - meteors burn up Moh’s scale - used to determine hardness - Coldest temperature Color - clue to their identification - Can have impurities Streak - mineral’s color in powdered form - Can be different from the color of the mineral and can be colorless Crystal Form - Internal structure of mineral Bonding types: covalent, ionic, metallic Altitude Temperature Cleavage - property to break along specific planes of weakness Thermosphere - Northern and southern lights occur Fracture - irregular/ without definite pattern or - Ionosphere - layer of electrically charged atoms direction and molecules CHEMICAL COMPOSITION OF MINERAL AND ROCKS Silicates - contain silicon and oxygen Ex: quartz Carbonates - carbonate anion with other elements Altitude Temperature Ex: calcites Exosphere - air is thin Native elements - uncombined with anything - Satellites Ex: gold and diamond _________________________________________ TEMPERATURE IN EXOSPHERE _ Week 2 THREE CLASSIFICATIONS OF ROCKS Igneous - formed from cooling of magma Extrusive - expelled from earth - volcanic Intrusive - inside the earth’s crust Day Night - plutonic Sedimentary - preserves a record of the environment PHYSICAL PROPERTIES OF MINERALS AND that existed ROCKS Clastic - little pieces of broken shell Luster - ability of mineral to reflect light Chemical - dissolved materials precipitate Metallic - polished metal, shiny gold Organic - accumulation of plants or animal Non-Metallic - grassy, silky, transparent to debris translucent Hardness - resistance of mineral to abrasion Metamorphic rock - bonds or stripes Metamorphism - extreme heat and pressure Weathering - process that break up solid rocks Shearing - pushing in opposite directions Physical Weathering - mechanical weathering Continental Drift Theory - continents once been a - Breaks large masses of rock to smaller super-continent grains 1. Frost Wedging - break-up of rock by Pangea - “all earth” the pressure of water freezing in cracks. - 200 million years ago, all the continents on 2. Abrasion - breakdown of rocks caused Earth were actually one huge "supercontinent" by impact and friction. surrounded by one enormous ocean. 3. Burrowing Animals - animals excavate to the ground to create space Laurasia and Gondwana - pangaea was split into two for habitation. landmasses Chemical Weathering - process by which - 120 yrs ago rocks are broken down by chemical reactions. Oxidation - response of oxygen with minerals TYPES OF FAULTS Ex: rusting Normal Fault - hanging wall moves downward with respect to the foot wall Mass Waisting - the movement of rock and soil down - Extensional force “away” slope under the influence of gravity. _________________________________________ _ Week 3 Magmatism - the formation of magma under Earth's surface. Reverse Fault - hanging wall moves upward with respect to the foot wall. Decompression Melting - pressure decreases but - Compressional force temperature remains the same Flux Melting - when rock is close to its melting point - Water and carbon dioxide helps break chemical bond in chemicals Strike-slip Fault - slides past each other or moves Extrusion - the deeper the magma chamber, the opposite stronger the explosion - Shearing force TYPES OF STRESS WHICH AFFECTS THE BEHAVIOR OF ROCKS Compressional - squeezes and pushes rocks together Tensional - stretches and pulls rock apart _________________________________________ _ PLATE TECTONIC THEORY → explains how major landforms are created as a result of Earth's subterranean movements. Oceanic-Oceanic Convergent - the older plate goes Plate Boundaries - where plates meet under. - the lithosphere of the earth is divided into a - Forms volcanic arcs small number of moving plates whose 1. Sea Mounts - under sea level and no movements cause seismic activity longer active. 2. Volcanic Island arc - above sea level abd Divergent Boundary - spreading boundaries forming a chain of islands. - Plates move apart from one another - Below sea-level: mid-oceanic ridge - Above sea-level: rift valley Continental-Continental Convergent - two continental plates converging between a boundary - Collision of the plates pushed upward Convergent Boundary - the zone where two - Older plate slightly sink beneath the other plates meet - Himalaya mountain range - The convergence can be between: a) an oceanic plate and a continental plate, and b) two continental or c) two oceanic plates. Oceanic-Continental Convergent - the denser oceanic plate goes under the continental plate that sinks in the subduction zone Relative Dating - relative age relationships most commonly, vertical position Superposition - younger rocks lie over older rocks Half Life - how long it takes for half of a sample of UNCONFORMITIES the isotope to decay. Disconformity - place where a a parallel rock layer ______________________________________ is mislaid Week 5 - Sequence of rock layers is pushed up GEOLOGICAL PROCESS AND HAZARDS because of forces Earthquake - sudden movement of the earth’s lithosphere causes the ground surface to shake Focus - point inside where earthquake started Epicenter - vertically above the focus Magnitude - total amount of energy released - depicts the absolute or relative direction - Measured by seismograph Intensity - how much ground shakes at a specific Nonconformities - igneous or metamorphic place and decreases with distance from epicenter rocks were exposed to erosion before being covered - Measured by PHIVOLCS by younger sedimentary rock PHIVOLCS - Philippine Institute of Volcanology and Seismography Tsunami - giant waves caused by quakes and volcanic eruption - Low-lying coastal areas are most vulnerable Landslide - down-slope movement of earth material Angular Unconformities - horizontal rock layers lie on top of tilted or folded rock layers Fire - often linked with broken electrical and gas Constructive Wave - swash is stronger than lines backwash - Common byproducts of earthquake - Low energy waves HYDROMETEOROLOGICAL HAZARDS Destructive Wave - stronger backwashes → atmospheric hazards that could cause loss of life - Pulls material away from the shoreline and into the sea resulting in erosion Coastal Erosion - loss of displacement of land Flood - water overflows onto normally dry land along the coastline Inland Flood - far away from coast Flashflood - fast occurrence TYPES OF EROSION River Flood - bodies of water rise and Abrasion - rock fragments against the cliffs overflow Coastal Flood - along the coast by seawater Hydraulic pressure - trapping air into cracks Urban Flood - lack of drainage in city area Attrition - process of erosion during rock Storm Surge - “Daluyong ng bagyo” collision and transportation - the rise in seawater level caused solely by a storm. Waves scouring - waves breaking at the base of the cliffs swirl around the base and cause the Tornadoes - violently rotating column of air elimination of movable rock. touching the ground. Wave pounding - collapse of the cliff face because Rip Currents - currents of water flowing away of the absolute force of a wave the shore that can pull people. ______________________________________ Week 6 MARINE AND COASTAL PROCESSES AND HAZARDS Waves - occurs when the force of wind blows over surface of water. - Transports energy, not water Swash - wave washes up unto shoreline Backwash - water retreats back into the sea