Friday, June 14, 2013

How was the Regent this year?

Now you've taken the Test this morning...

Compare this year to the past regents you took for practice... was it harder, the same or easier?

Comment below....

Thursday, June 13, 2013

are you ready for the Regent? 6/14/13 @ 8:45 am


***************************************************************************
We gave this sheet out in the beginning of the school year....
If you can answer these questions then you are ready...
IF you still can't.... better study http://www.regentsearth.com/Interactive%20Regents/Interactive%20Regents.htm



Friday weather Forecast : Raining


  • Rain ends early in New England.  
  • Occasional wind gusts from 40-50 mph may persist in the morning from southeast New England to Long Island and the Jersey Shore, before tapering off in the afternoon.


An additional inch or two of rain from central New York to southern New England may trigger additional flash flooding, due to saturated ground.


 

Friday, June 7, 2013

Review on June 8, Saturday 9:30 to 11:30

Earth Science Regents Review    

                                    for June 14, 2013 @ 8:30 am


The following is a list of the important concepts that you will need to know for the upcoming Regents exam in Earth Science. Use this list as a review guide.
Vocabulary is underlined and bold. If you don’t know what a word means LOOK IT UP!
 (Select the word then right-click and search)

Unit One: Observation, Measurement, and Graphing and Change
* Observations use the senses. Inferences are interpretations based on observations.
Anything in the future or the distant past is an inference.
* A uniform substance always has the same density.
* As pressure increases, density increases.
* Most substances are most dense in the solid state, least dense in the gaseous state.
* Water is most dense (smallest volume) at 3.98°C, when it is a liquid.
* Water expands when it freezes.
* As temperature increases, density decreases.
* Direct Relationship = both variables increase or decrease.
* Inverse Relationship = one variable increases while the other decreases.
* Scalar values: magnitude (size) only.
* Vector values: magnitude & direction (wind & magnetic fields)
* Most environmental changes are cyclic.
* Change occurs at interfaces and always involves energy transfers.
* Dynamic Equilibrium = changes are occurring, but are balanced, so overall
conditions stay the same.

Unit Two: Astronomy
* Universe: everything. Began with big bang approximately 12 billion years ago
* Evidence for big bang: Expansion (red shift) & cosmic background radiation.
* Galaxies: collections of billions of stars. Our galaxy - the Milky Way
* Stars: powered by hydrogen fusion. Hydrogen is the fuel. Helium is the product.
* Star color depends on temp. Hot = blue. Red = cool. Sun = yellow (medium)
* Planets: non-luminous. Orbit stars. The closer to the star, the faster the orbital velocity
and the shorter the period of revolution.
* Moons: orbit planets.
* Luminosity: Brightness independent of distance.
* Meteor, asteroid: Space rocks.
* Comet: Ice, dust, & rock in orbit around sun
* Nebula: cloud of gas & dust
* Supernova: exploding star.
* Orbits are ellipses. Know formula.
* Keppler’s law of ‘equal swept area in equal time

Unit Three: Measuring the Earth
* The true shape of the Earth is an oblate spheroid.
* The best model of the Earth's shape is a sphere.
* To determine the earth's circumference, we need the altitude of the sun at two locations and the distance between those locations. (Eratosthenes)
* The altitude of Polaris equals your latitude.(Northern Hemisphere)
* Latitude lines go east - west. (Equator = 0° Lat., Poles = 90° Lat.)
* Maximum Latitude is 90°.
* Longitude is based on observations of the sun (solar noon).
* Longitude lines go north - south. (Prime Meridian = 0° Long. - through
Greenwich, England)
* Maximum Longitude is 180°.
* Atmosphere = gasses, Hydrosphere = water, Lithosphere = rock (crust)
* Isolines connect points of equal value.(Isotherms, Isobars, Contour Lines)
* Closer isolines mean a steeper gradient.




Unit Four: Earth Motions
* The Earth rotates west to east at a rate of 15° per hour (one rotation in 24 hours).
* The Earth revolves counterclockwise around the sun (one revolution in 365 1/4 days or
about 1° per day).
* All celestial objects appear to move to the west.
* Geocentric = Earth centered / Heliocentric = sun centered.
* Evidence that the Earth rotates: Foucault Pendulum - appears to change direction.
* Coriolis Effect - deflects to the right in the northern hemisphere.
* The sun is never, ever, ever directly overhead in New York State !
* Summer Solstice - June 21 - 16 hours of daylight - sun rises north of due
east - sun is directly overhead at the Tropic of Cancer, 23 1/2 degrees north latitude.
* Winter Solstice - December 21 - 8 hours of daylight - sun rises south of due east,
sun is directly overhead at the Tropic of Capricorn, 23 1/2 degrees south latitude.
* Equinoxes - March 21 (vernal) and September 23 (autumnal) - 12 hours of daylight -
sun rises due east - sun is directly overhead at the equator.
* Earth is closer to the sun in winter - December. (perihelion)
* The equator always has 12 hours of daylight.
* The closer a planet is to the sun, the faster it orbits.
* Planets appear to go backwards (retrograde motion) as the Earth passes them in space.
* Cycle of moon phases = 29.5 days. One lunar revolution around Earth = 27 1/3 days

Units Five and Six: Energy and Insolation
* Kinetic Energy = energy of motion, increases with velocity.
* Potential Energy = stored energy, increases with height (energy of position).
* Good absorbers of energy are also good radiators of energy.
* Dark, rough surfaces absorb more energy than light, smooth surfaces.
* Conduction = energy transferred from molecule to molecule (solid, liquid, and gas) by collisions.
* Convection = energy is transferred by moving molecules (liquid and gas) due to density differences.
* Radiation = energy is transferred by waves, needs no medium (vacuum, space).
* Energy moves from Source to Sink.
* Specific Heat = energy needed to raise 1 gram of a substance 1° Celsius.
* Water has the highest specific heat.
* calorie = specific heat of water.
* Temperature does not change during a phase change. (Latent Heat)
* Know the water phase change graph.

Unit Seven: Weather
* Bodies of water moderate temperatures.
* Atmosphere is heated by infrared energy re-radiated from the Earth.
* Atmosphere gets moisture from evapotranspiration.
* The more moisture in the air the slower the evaporation rate.
* Warm air is less dense, Moist air is less dense.
* Convection = air movement due to differences in density (and pressure).
* Wind blows from high pressure to low pressure. (Note: Coriolis effect)
* Winds are named for the direction they come from.
* As altitude increases: pressure decreases, temperature decreases.
* Adiabatic Temperature Change = results from a change in pressure - direct relationship
* Expanding gasses cool, compressing gasses warm.
* Warm air can hold more water than cold air.
* Condensation = water vapor turning into liquid water.
* Relative Humidity = % of moisture in the air compared to the air’s capacity.
Warm air = greater capacity, cool air = smaller capacity.
* Dew Point = temperature at which air becomes saturated (R.H. = 100%).
* The smaller the difference between air temp. and Dew Point = the greater the chance of precipitation.
* Know how to find Dew Point and Relative Humidity.
* Condensation Nuclei = surfaces on which condensation can occur (dust, pollen).
* Cloud = collection of water droplets too small to fall.
* Precipitation = any form of water that falls from the atmosphere.
* Snow - only precipitation that does not begin as a liquid.
* Sublimation: solid to vapor or vapor to solid without going through the liquid phase.
* Air masses are classified based on their source region.
* High pressure systems = cool and dry, Low pressure systems = warm and moist.
* Weather in the US moves from SW to NE or W to E (storm track)
* Cold fronts are faster than warm fronts.
* Wind direction around Lows (counterclockwise, towards the center) and
   Highs (clockwise away from the center) in Northern Hemisphere.
* Know how to read Station Models, isotherms and isobars on a weather map.

Unit Eight: Groundwater
* Infiltration depends on permeability, permeability depends on porosity.
* Porosity is independent of particle size. (unless particles are mixed!!!)
* As particle size increases, permeability increases, capillarity decreases.
* Ep (potential evapotranspiration) depends on temperature.
* Climates are determined by P/Ep ratio.
* Aquifer: layer of porous rock or soil
* Water table: Interface between zones of aeration & saturation.
* Evapotranspiration: Combination of evaporation & transpiration.

Units Nine and Ten: Weathering, Erosion and Deposition
* Weathering = breakdown of rock
* Rate of weathering depends on climate, particles size, and mineral composition.
* Smaller particles have more surface area.(weather faster)
* Mature soils have several identifiable layers (horizons).
* Most sediments are "transported" sediments.
* Some soils are residual: formed in place from the bedrock below.
* Sediments have characteristics that identify their transporting agent.
* Gravity is the driving force behind most erosion.
* Running water is the most dominant agent of erosion on Earth.
* Stream velocity depends on slope and discharge and shape of channel.
* Streams transport sediments in solution, suspension, and rolling (saltation).
* In a straight section of stream, velocity is greatest in the middle just under the surface.
* In a curved section of stream, velocity is greatest on the outside just under the surface.
* Streams: sediments are sorted, round and smooth, and form V-shaped valleys.
* Glaciers: sediments are unsorted, striated (scratched), and form U-shaped valleys.
* Sorting = separation of particles during deposition based on size & density & shape.
* The largest, roundest, densest particles are deposited first.

Unit Eleven: The Rock Cycle
* Mineral physical characteristics depend on their internal arrangement of atoms.
* Physical properties of minerals = color, streak, luster, hardness, cleavage, crystal form
* 90% of lithosphere is composed of only 12 minerals.
* Sedimentary Rocks - can be clastic (particles), chemical (evaporite), or organic (shells) found in strata, flat layers - only type of rock that contains fossils
* Igneous Rocks: intrusive (plutonic) = below surface, cooled slowly = large crystals
                             extrusive (volcanic) = above surface, cooled quickly = small (or no) crystals
* Large crystals = coarse grain (texture). Small = fine grain. No crystals = glassy
* Metamorphic Rocks: changed from heat and pressure, can be Regional or Contact.
May show banding, distortion of structure, mineral alignment
* A rock's characteristics indicate how (and where) it was formed.
* Sedimentary rocks are found as a thin veneer over large areas.
* Non-sedimentary rocks are usually found in areas of earthquake and volcanic activity.
* Know the Igneous, Sedimentary, and Igneous Rock Schemes in the Reference Tables!
* Know how to use the rock cycle chart in the reference tables!

Unit Twelve: Crustal Change
* Earthquake Zones = Volcano Zones (both occur in specific zones = plate boundaries)
* Boundaries: Convergent, Divergent, Transform
* Convection cells in the earth's mantle (Athenosphere) move the plates.
* Crust created at mid ocean ridges (sea floor spreading)
* Crust is being destroyed at ocean trenches (subduction).
* Fault = zone of weakness in crust
* Focus = point of origin of an earthquake
* Epicenter = point above focus on surface of earth.
* Energy from earthquake is released in Seismic waves (recorded in a seismogram
by a seismograph)
* p-waves: faster than s-waves - travel through solids, liquids, and gasses
* s-waves: slower - travel only through solids
* We need info from three seismograph locations to find the epicenter.
* Seismic data provides a model for the inside of the earth.
* Moho = bottom of crust (interface) where density suddenly changes
* Shadow zone = zone where no P or S waves received from a particular quake because
waves are refracted.
* Continental crust: thick - granite. Sea floor crust: thin - basalt
* Density, temperature, and pressure all increase with depth.
* Geosynclines = areas where crust appears to sink under weight of sediment.
* Isostasy = earth's crust in equilibrium
* Know how to use the Travel Time Chart in the Reference Tables!

Unit Thirteen: Geologic History
* Original Horizontality = rock strata are deposited in horizontal layers.
* Evidence of crustal movement: tilting, folding, faulting
* Principle of Superposition = profiles are built from the bottom up. (bottom = older)
* Intrusions and faults are relatively younger than the rock they are in.
* Unconformity = buried erosional surface
* Index fossils and Volcanic ash layers are good time markers.
* Good time marker fossil: species existed briefly but was widespread.
* Radioactive decay = breakdown of isotope into a more stable element.
* The rate of radioactive decay is constant. (unaffected by heat and pressure)
* Half life = time period in which one half of the remaining amount of isotope decays.
* Uranium-235 is used to date really old rocks.
* Carbon-14 is used to date recent organic material.
* Know how to use the Geologic Timescale in the Reference Tables!

Unit Fourteen: Landscapes
* Landscape characteristics = topography = relief (elevation)
* Landscape Regions are classified based on hill, slopes, stream patterns, and soil associations.
* There are three types of landscape regions: mountains, plateaus, and plains (lowlands).
* Know how to use the NY State maps in the Reference Tables !
* Uplift = constructive force, leveling (erosion)= destructive force.
* Uplift and leveling may be in dynamic equilibrium but one is usually dominant.
* Climate can affect landscape, landscape can affect climate.
* Wet climate = rounded features (NYS). Arid climate = angular features (American SW)
* Type of bedrock (resistance) can affect landscape.

MOST IMPORTANT:
There are 16 pages of earth science reference table. You must be thoroughly familiar with what’s in them so that when you are asked a question, you will know to look for the answer. If you don’t know that the answer is in the tables, you won’t look for it! You must also know how to use the graphs and charts in the tables.




For video reviews - (c) Hommock Middle School
scroll down to different topics.
If you studied you should do well!                                                  06-14-2013@ 9:00 am

Reference Table:Page 13 - Temperature & PressureSeasonsChemical Weathering
Page 1 - EquationsPage 13 - Station ModelEnergy:Deposition
Page 1 - NYS FossilPage 14 - Layers of The AtmosphereEnergy TransferWind & Water Erosion
Page 1 - Properties of WaterPage 14 - Electromagnetic SpectrumGreenhouse EffectPhysical Weathering
Page 1 - Radioactive DecayPage 14 - Wind BeltsPhase Changes - Liquid - SolidRocks & Minerals:
Page 1 - RulerPage 15 - Solar System DataSpecific HeatIgneous Rocks
Page 1 - Specific HeatsPage 15 - Characteristics of StarsWeather:Sedimentary Rocks
Page 2 - Landscape MapPage 16 - Properties of MineralsHigh & Low PressureMetamorphic Rocks
Page 3 - Bedrock Geology MapIn The Beginning:Layers of the AtmosphereMineral Identification
Page 3 - NYS Lat. & Long.Prologue (Unit 1)Relative Humidity & Dew PointMinerals
Page 4 - Ocean CurrentsMeasuring The Earth:Weather RelationshipsThe Dynamic Crust:
Page 5 - Tectonic PlatesLatitude & LongitudeFrontsContinental Drift
Pageg 6 - Rock CycleShape of The EarthOceansConvergent Boundaries
Page 6 - Igneous Rock IDTopographic MapsWindDivergent Boundaries
Page 6 - Water VelocityTopo Maps - Finding GradientWater and Climate:Hot Spots
Page 7 - Metamorphic Rock IDEarth In The Universe:ClimateLayers of The Earth
Page 7 - Sedimentary Rock IDThe UniverseWater CycleEarthquakes
Page 8 - Geologic HistoryGalaxiesGround Water & SoilGeo. History & Landscapes:
Page 9 - Geologic HistoryThe MoonGround Water RelationshipsLandscapes
Linking ESRT pages 2,3,8 & 9The Solar SystemPorosity & PermeabilitySequence of Events
Page 10 - Earth's InteriorEarth's RotationWeathering, Eros. & Dep:Earth History
Page 11 - P & S Wave Travel TimesEllipsesGlaciersRadioactive Decay
Page 12 - Rel. Hum. & Dew PointThe Sun's PathGravity Erosion

Clock's on.... Layers of the Earth... who came first?

How old is that rock? Ch 6
try the virtual lab...
http://nemo.sciencecourseware.org/VirtualDating/files/1.0_ClocksInRocks.html

Worksheet CSI on Rock layers... who came first?

Geological History


Thursday, May 30, 2013

Performance Test INVITE and Prep session Saturday....

you should have received your Invitation with study guide today, if not pick it up by Friday....
If you do not have a ticket that means you are barred from the Regents due to lack of labs... you may be going to summer school.

The prep session on Saturday (June 1- 10 am to 12 pm) will help you master the performance test coming up.

Topic to go over are Lab#6 Eccentricity, Lab #13,14, Mineral and Rocks and #15- epicenter of the earthquake....

you alone have 3 stations to do: each in 9 minutes span only.
















Friday, May 24, 2013

Final- Mock regents on 5/30 and 5/31

Do your review from the green review book....in the back there are 3 regents for you to practice.... answer on a loose leaf  & do extra credit aside from HW #10 (ch 3 Plate tectonic worksheets) Ch 4 and 5 outlined....

Start reviewing with past topics....Physical setting foundations

4 States of Matter Song


Tuesday:  watch and sing along with Mr. Parr all credits goes to Mr. Parr
Basic energy transfer and astronomy topic 
heat transfer.... Heat song
 Spring / Neap Tide song
Moon Phases

Types of Stars Song

Layers of the Sun Song

Planets Around a Star Song



Wednesday: Meteorology concepts
storm clouds
weather fronts

Winds Blow Song


Thursday: Mock Regent  day 1
keep reviewing.... 


Friday day 2 short answer part....Mock Regent part 2...

Performance Test Prep Sat June 1, 2013 10am-12pm in Room 324

Next week don't be late....