Middle School Science/Earth and Space Science

Physical Geology Processes of mineral and rock formation Igneous - Magma at 600 – 1200 deg C. from 30 Km under earth (Plutonic), magma cools and crystallizes slowly within crust. Through volcanic action the magma reaches surface as lava or fragmental ejecta.

Weathering - Rocks and minerals crystallize on surface, and are transformed through chemical reactions between other minerals and conditions

Sedimentary - Compaction and cementation after deposition of either rocks by weathering and erosion (detrital), organic matter, or chemical precipitates (evaporites). Occurs at or near surface as in carbonate-rich sediments.

Metamorphic - Rock types subjected to temperature and pressure conditions different than those in which the it was formed, including previously-formed metamorphic rock. The pressure and temperature must be sufficiently high so as to change the original minerals into other mineral types or other forms such as by recrystallisation.

Methods used to identify and classify different types of minerals, rocks, and soils Classify Rocks: Hardness - 1 Talc, 2 Gypsum, 3 Calcite, 4 Fluorite, 5 Apatite, 6 Potassium feldspar, 7 Quartz, 8 Topaz, 9 Corundum, 10 Diamond

Density -- heavy gold and platinum (20), Silicates between 2.5 and 3.5, ores between 4 and 8

Cleavage -- how it breaks depends on crystal structure; some break in a predictable manner others don't. Cleavage is defined as a smooth break with a shiny surface. Cleavage can be perfect, good, or incipient. Highest cleavage can leave thin sheets; the thinnest are flakes of mica.

Fracture - When rocks are broken open, fracture surfaces are formed; fracture surfaces can be conchoidal (rounded), smooth, splintery, hackly, fibrous, even or uneven.

Twinning - appearance of fine parallel lines, called striations, on the cleavage planes. Striations change with respect to the direction it was, or is, growing.

Transparency - Can be water-clear, transparent, translucent, or opaque.

Lustre - A reflective property, not color. Can be metallic, glassy (vitreous), pearly, silky, resinous, greasy, waxy and earthy. The degree of luster is described as spleandent, shining, glistening, glimmering, matt, or dull.

Color - Natural colour such yellow for sulfur, red for cinnabar, green for malachite, or blue for azurite. Contamination in small quantities can cause changes.

Special light effects - Regularly intercalated foreign substances, by fine fractures or twinning such as Labradorescence, or Opalescence.

Streak - colour of powdered mineral on a white underlay.

Classification of common rocks - Native elements (gold), Oxides, Hydroxides, Carbonates (limestone), Sulfides (pyrite), Sulfates (gypsum), Phosphates, Halides (rock salt), Silicates (mica, clay)

The structure of the Earth and the nature of the various layers Four layers: crust, mantle, inner core, and outer core, plus the lithosphere Crust

thinnest layer, 35 - 70 km thick on the continents, and 5 - 10 km thick under the oceans
thinner than any of the other layers,
calcium, sodium, and aluminum-silicate minerals.
cold, and brittle, fractures to cause earthquakes

Mantle

1800 miles thick
Most of the Earth's mass
Iron, magnesium, aluminum, silicon, and oxygen silicate compounds.
1000 degrees C, solid but plastic; deforms slowly with convective heat from the outer core

Outer core

2900 miles thick and the
liquid Fe (Iron), 3700 deg C

Inner core

5200 km to the Center of the earth
4300 deg C, remains solid from pressure

Lithosphere

crust and the upper part of the mantle, 5 to 30 miles deep
Earthquakes start at the lithosphere

Formation

Earth formed with the Sun, and the other planets 4.54 billion years ago from rotating disk of dust and gas.
Heat released from gravitational energy and radioactive decay melted planet, still cooling
Iron (Fe) sank into the core of the Earth, lighter materials such as silicates, oxygen compounds, and water rose to the surface

Soils Three basic types: sand, silt, and clay made from finely ground rock particles, and grouped according to size Sand, the largest particle, determines aeration and drainage characteristics, Clay particles, microscopic and chemically active, bind with water and plant nutrients Ratio of particle sizes determines type.

Soil ingredients

regolith minerals and weathered rock fragments
humus organic matter
gases
water
living organisms

Effecting formation

climate
parent rock
organisms
relief (slope, topography)
time

Horizons: soil layers

O horizon - layer of humus on the ground surface
A horizon (zone of leaching) - Top soil with rich organic matter, usually has dark color
B horizon (zone of accumulation) - Subsoil, may contain soluble minerals such as calcite in arid climates (caliche)
C horizon - Weathered bedrock or saprolite (chemically weathered rotten rock)
Bedrock - lies below the soil profile

Soil types:

Pedalfer - humid climates, rich in Al and Fe
Pedocal (caliche) - arid climates such as in the Southwestern U.S; called caliche (or hardpan) it is a calcium carbonate deposit
Laterite - tropical climates with very high rainfall iron and aluminum oxides, all other elements virtually depleted It is derived from the weathering of basalt in high rainfall conditions, which has caused leaching of elements and nutrients. When used for agriculture, the small amount of nutrients is quickly depleted, and the soil dries to become as hard
Bauxite - Rich in Al oxides, intense tropical weathering depletes of nearly all other elements. Derived from weathered of granite; the more soluble Ca, Na, K, and Si have been leached leaving Al. It is the principle ore of aluminum.
Loam - farm soil; sand, silt, manure, and clay with humus
Humus - organic soil material that has broken down to a point of stability that will not change if conditions don't. In agriculture it means compost.

Internal processes and resulting features of the Earth, including folding, faulting, earthquakes, and volcanoes

Folding - the bending of rocks from compressional tectonic forces such as continental collisions.
Faulting - fracturing of rock structures causing breakage and slip that is parallel to the fracture. The rocks have been subjected to compressional, extensional, and shearing forces; and they are found close to surface of the Earth.
Earthquakes - release of elastic strain energy that radiates seismic waves. It causes the movement of faults, and creates planar zones of deformation within upper crust. Highest stress most often found at the boundaries of the tectonic plates / volcanic regions and anthropogenic sources
Volcanoes - magma erupts through the surface often occurs near the boundaries of the continental plates

Plate tectonic theory and the evidence that supports this theory

Major plates African, Antarctic, Australian, Eurasian, North American, South American, Pacific, Cocos, Nazca, and the Indian plates

Two observations:

continental drift
sea-floor spreading

Motion - Lithosphere is rigid, and asthenosphere is plastic. Convection currents in the mantle are transmitted through the asthenosphere; and the motion is driven by friction between the asthenosphere and the lithosphere. Since continental and oceanic lithospheres differ appreciably in thickness, the effects are proportionately different.

Boundary zones - earthquakes and volcanoes; mountains and oceanic trenches.

Types of Boundaries

Transform boundaries plates grind past each other along transform faults
Divergent boundaries (oceanic rifts) plates slide apart from each other.
Convergent boundaries (active margins) where two plates slide towards each. Either one is pushed down, a subduction zone, or there is collision and compression forming an anorogenic belt

Other forces in plate motion:

Trench suction - Local convection currents pull down on plates in subduction zones at ocean trenches.

Gravity - Ridge-push, plate motion driven by higher elevation of plates at mid-ocean ridges, slides downhill / higher elevation caused by low density of hot material upwelling in the mantle

Slab-pull -Plate motion is driven by weight of cold, dense plates sinking into the mantle at trenches strongest force directly operating on plates / trench suction plays important role / driving force and its energy source are still debatable subjects

Water: the hydrologic cycle and the processes by which water moves through the cycle The Earth's Water Budget - the distribution of water among the oceans, land and atmosphere.

Evaporation (evapotranspiration) - water forms into a gas and rises into the atmosphere from solar radiation, some comes from plants (transpiration), most comes from oceans.

Condensation - Vapor forms into liquid and possibly solid within the atmosphere to produce clouds and fog

Transport (advection): The movement of water through the atmosphere, water storage in the atmosphere

convection in unstable air
atmospheric motions in the vertical direction
convergence
associated with cyclones
lifting of air by fronts
lifting over elevated topography such as mountains

Precipitation - The transfer of water from the atmosphere to land. Rain, snow, hail, sleet, and freezing rain are discussed

Foliage (canopy) interception - Precipitation intercepted by plants re-evaporates into the atmosphere

Infiltration - Water is stored in the ground

Runoff - Rivers, lake, and streams transport water from land to the oceans. Too much rainfall can cause excess runoff, or flooding

Groundwater - located below ground and how it returns to the surface

Sub-surface flow - Water may return to the surface, or flow to the oceans

Weathering, erosion, and deposition

Weathering - the decomposition of rock.

Erosion - the displacement of solids (soil, mud, rock, and so forth) by the agents of wind, water, ice, movement in response to gravity, or living organisms

Deposition (sedimentation) - the process by which material is added to a landform, by which wind, water, or ice create a sediment deposit through the laying down of granular material that has been eroded and transported from another geographical location.

Historic Geology

Uniformitarianism -- geologic processes same all through time, past geologic events can be explained by phenomena and forces of today.

Basic principles of stratigraphy - study of rock layers, sedimentary and layered volcanic rocks

Sequence, spacing, composition, and spatial distribution of sedimentary deposits and rocks
Geology reconstructs the history of the Earth
Geologic processes that change the Earth's surface and subsurface
used with structural geology and paleontology to tell the sequence of events
evolution of plants and animals
radiometric dating derives absolute versus relative ages of geologic history

Lithologic stratigraphy - study of sedimentary and layered volcanic rocks, where the lowest layers are the oldest

Superposition -,the oldest strata occur at the base of the sequence in an undeformed stratigraphic sequence,

Chemostratigraphy - relative proportions of trace elements and isotopes within and between lithologic units

Cyclostratigraphy - relative proportions of minerals, carbonates and fossil diversity related to changes in palaeoclimates (cyclic)

Biostratigraphy (paleontologic) - fossil evidence in the rock layers / Strata from widespread locations containing the same fossil fauna and flora are correlatable in time

Relative and absolute time

Relative time (chronostratic) - relative age relationships (most commonly, vertical/stratigraphic position). These subdivisions are given names, most of which can be recognized globally, usually on the basis of fossils.

Absolute time (chronometric) - numerical ages in "millions of years" or some other measurement. These are most commonly obtained via radiometric dating methods performed on appropriate rock types.

Formation of fossils

Permineralization - pores of the plant or animal remains are impregnated by minerals / original shape not changed.

Casts and molds - fossils where the organisms shape has been impressed onto rocks

Impressions - two dimensional imprints of an organism which contain no organic matter.

Whole organism preservation - petrified forest; eggs of dinosaurs, by desiccation or freezing

Types of information fossils provide Both animals and plants

past environments
physiology
diet
adaptations
behavior
evolution, and extinction
determining ages of rocks in which fossils are found

Geologic time scale and how it was developed Phanerozoic (544 million years ago to present), includes Paleozoic, Mesozoic, and Cenozoic eras

era of abundant animal life
545 million years ago to present
starts with diverse hard-shelled animals

Paleozoic (542 mya to 251 mya)

begins with hard shelled fossils
sophisticated reptiles and modern plants develop
dinosaurs became extinct at end

Mesozoic Era (248 to 65 million years ago)

created modern life
continents drifted apart
warm climate and rifting influenced evolution

Cenozoic Era (65 million years ago to present)

continents moved to their present positions
co-dependent flowering plants and species
mammals become dominant species

Precambrian (4500 to 544 million years ago) includes Proterozoic, Archaen, and Precambrian

Proterozoic Era (2500 to 544 million years ago)

90% of all geologic time
continents first appeared /
bacteria and archaeans as oldest abundant fossils ,
eukaryotic cells appear 1.8 billion years ago

Archaean Era (3800 to 2500 million years ago)

earliest life, bacteria microfossils,
reducing atmosphere of methane, ammonia, and other gases

Hadean Time (4500 to 3800 million years ago)

pre-geological
Solar System was forming

Geologic time was developed when after fossils are found buried in a definite order

Outline the sequence of important events in the Earth’s history

First human beings 1 mya
Ice Age 2 mya
Mass extinction (destroyed dinosaurs and many species of marine life) 65 mya
First flowers 136 mya
First mammals and birds 200 mya
First dinosaurs 210 mya
Mass extinction (destroyed 75% of all marine species on planet) 225 mya
First reptiles, trees and insects 330 mya
First land plants, first amphibians 395 mya
First fish 400 mya
Oldest life forms on Earth 3400 mya
Formation of Earth 4600 mya

Historical Periods

Precambrian 650Ma - The Late Precambrian was an "Ice House" World, much like the present-day.

Cambrian 514ma - Animals with hard-shells appeared

Ordovician 458ma - coldest times in Earth history

Silurian 425ma - Coral reefs expand and land plants begin to colonize the barren continents

Devonian 390ma - Freshwater fish migrate from southern hemisphere continent to North America and Europe. Forests grew for the first time in the equatorial regions of Artic Canada.

Early Carboniferous 356ma - Paleozoic oceans between Euramerica and Gondwana began to close

Late Carboniferous 306ma - Euramerica and Gondwana began to close, forming the Appalachian and Variscan mountains / ice cap grew at the South Pole / four-legged vertebrates evolved

Permian 255ma - deserts covered western Pangea / reptiles spread across the face of the supercontinent. 99% of all life perished at end of the Paleozoic Era.

Triassic 237ma - supercontinent of Pangea allowed land animals to migrate from the South Pole to the North Pole. Life began to rediversify / warm-water faunas spread across

Jurassic 195ma - south-central Asia had assembled, Pangea begins break up

Late Jurassic 152ma - Pangea break apart Middle Jurassic / Late Jurassic Central Atlantic Ocean narrow ocean separating Africa from eastern North America. (Africa) Eastern Gondwana separate form (South America) Western Gondwana

Cretaceous 94ma - India separated from Madagascar

K/T extinction 66ma - comet global climate changes killed the dinosaurs / oceans had widened

Eocene 50ma - India collide Asia Tibetan plateau / Australia move rapidly northward.

Miocene 14ma - Antarctica was coverd by ice and the northern continents were cooling rapidly.

Last Ice Age 18K - "Ice House" climate mode, there is ice at the poles; polar ice sheet expands contracts variations in the Earth's orbit

Modern World - Global climate is warming / new Pangea supercontinent forming

Oceanography

Formation and movement of ocean waves Wind blows across the smooth water surface, the friction or drag between the air and the water tends to stretch the surface, resulting in wrinkles surface tension acts on these wrinkles to restore the smooth surface

Tides: causes and factors Gravitational pull from the Moon and Sun; the force increases and decreases with changing distance of the Earth from them.

Major surface and deep-water currents in the oceans and the causes of these currents Surface currents 10% of ocean water, 400 meters deep Deep currents gravity driven because of differences in salinity and temperature, colder northern air causes temperature decreases and hence sinking

Forces: Primary - starts water moving Secondary - influence direction of currents

Solar Heating - warming water rises at equator and sinks in northern waters
Winds - Long term winds will driver water 2% of wind speed
Gravity - Sea slope, surface 8 cm higher at equator from expansion causing a slope, and density
Coriolis - Controls direction of large streams

Topography and landforms of the ocean floor and shorelines

Continental Shelf - a few hundred feet deep with an average width of 70 kilometers (43 miles), gentle slope

Continental Slope and Rise - starts with shelf break beyond which slope increases to 4° slope. Average width of 16 kilometers (10 miles), and descends to 2.4 kilometers (1.5 miles)

Abyssal plain (no light) - where the continental rise ends has an average depth 4 kilometers (2.5 miles)

Abyssal hills - small extinct volcanoes all over abyssal plains; flat-topped hills are submerged islands.

Mid-Ocean Ridge - undersea mountain chain along the middle of the ocean where plates are being pulled apart

Rift Valley - deep depressions along the center of the mid-ocean ridge whose sides are faults; hot material is constantly being extruded from Earth's mantle

Seawater

The physical and chemical properties of seawater Freezing 1.910 °C / Boiling 100.56 °C

Components of Seawater Litre H2O

Oxygen 857.8g
Hydrogen 107.2
Chloride (Cl-) 19.0
Sodium (Na+) 10.5
Sulfate(SO4-) 2.7
Magnesium (Mg2+) 1.3
Calcium(Ca2+) 0.4
Potassium(K+) 0.38
Bicarbonate(HCO3-) 0.14
Trace elements (0.52 g)
Nutrients (trace elements) Phosphate (PO4)
Nitrate (NO3)

Source of salts (ions) - Weathering, hydrothermal fluxes, dissolution from crust, and volcanic eruptions,

Nutrient cycles of the ocean Nutrients

phosphates (PO4)
nitrates (NO3)
Ammonia (NH4)
Silica (SiO2)

Photosynthesis or Chemosynthesis (produces oxygen) - 6CO2+6H2O+energy=C6H12O6+O2 Respiration - C6H12O6+O2=6CO2+6H2O+energy

Nitrogen Cycle - Compounds: N2, NO3, NH3

Nitrates enter the oceans from the atmosphere and rivers
Bacteria and plants absorb these and form carbohydrates and ammonia
Other bacteria and animals breakdown carbohydrates and recycle nutrients
Nutrients are rapidly used and recycled in the marine environment

http://www.ocean.uni-bremen.de/EInfo http://www.ocean.uni-bremen.de/EInfo/materialien/elemOc/top12-17/topic15.html

Meteorology

Structure of the atmosphere and thermal and chemical properties of atmospheric layers

Troposphere - to 10km, layer closest to the planet, has largest percentage of the mass, much vertical mixing from the radiation of solar heat absorbed by the Earth's surface. Temperature deceases with height.

Stratosphere - between 10 and 50 km / temperature increases with height

Ozone layer - or ozonosphere, within stratosphere

Mesosphere - 50 km to 80 km, temperature decreases with height

Thermosphere - 100-200 km nitrogen and oxygen / temperature increases to 1500 K

Ionosphere - lower thermopshere; has particles that are ionized by the sun; responsible for auroras , the region containing ions: approximately the mesosphere and thermosphere up to 550 km.

Exosphere - 1000 km where the atmosphere thins out into space; has free moving particles that may migrate into the solar wind or down into the lower layers.