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Earth Science Regents Concepts

Jun 5, 2025

Overview

This lecture covers key Earth Science Regents concepts, including density, mapping, rock types, weathering, plate tectonics, atmospheric conditions, and climate, emphasizing definitions, foundational processes, and exam-relevant relationships.

Density & Physical Properties

  • Density is how tightly packed molecules are.
  • As temperature increases, density decreases due to molecular expansion.
  • As pressure increases, density increases as molecules get closer.
  • Objects have the same density regardless of size.

Mapping & Coordinates

  • Latitude lines run horizontally, measuring distance north or south of the Equator.
  • Longitude lines run vertically, measuring east-west of the Prime Meridian.
  • The altitude of Polaris equals an observer’s northern latitude.
  • Time zones are 15° of longitude apart, equaling 1 hour difference.
  • Moving west makes time earlier; moving east makes time later.
  • Closer isolines mean steeper gradients on maps.
  • Water flows downhill, opposite the bends in contour lines.

Minerals, Rocks, & Weathering

  • Calcite and limestone react with acid.
  • Properties of minerals depend on atomic arrangement.
  • Rocks are classified by how they formed: igneous (cooling magma), sedimentary (compaction/cementation), metamorphic (heat/pressure).
  • Igneous rocks: large crystals (slow cooling), small crystals (fast cooling), vesicular (gas pockets).
  • Sedimentary rocks: formed from particles, may contain fossils.
  • Metamorphic rocks: formed by heat and pressure; look for foliation.
  • Smaller particles weather faster due to higher surface area.
  • Warm, moist climates favor chemical weathering; cold, moist climates favor physical weathering.

Erosion, Deposition, & Landscapes

  • Streams form V-shaped valleys; glaciers form U-shaped valleys.
  • Fastest stream velocity is on the outside of bends; slowest on the inside, where deposition occurs.
  • Gravity and glaciers leave unsorted, unlayered deposits; wind and water deposits are sorted.
  • Deltas form where rivers slow and deposit sediment entering the ocean.

Plate Tectonics & Earth's Structure

  • Plate tectonics are caused by convection currents in the mantle (asthenosphere).
  • Earthquakes and volcanoes are concentrated at plate boundaries.
  • Ocean crust is dense, young, thin, and basaltic; continental crust is thick, old, and granitic.
  • Outer core is liquid—S waves can't travel through it.
  • Plate boundaries: divergent (apart), convergent (together), transform (sliding).
  • P waves are faster and travel through solids and liquids; S waves move slower and only through solids.

Geologic Time & Fossils

  • Law of superposition: bottom layers are oldest in undisturbed strata.
  • Contact metamorphism shows interactions between intrusion and surrounding rock.
  • Index fossils spread widely but lived briefly; unconformities indicate missing geologic time.
  • Radioactive half-life is constant.
  • Carbon-14 dates recent remains; Uranium-238 dates ancient rocks.

Weather & Climate

  • Barometers measure air pressure; anemometers measure wind speed; wind vanes show direction.
  • Wind is caused by air pressure differences and flows high to low pressure.
  • High pressure means clear weather; low pressure brings clouds and rain.
  • Coriolis effect deflects winds rightward in the Northern Hemisphere.
  • Humidity and dew point are measured with a sling psychrometer.
  • Clouds form when warm air rises, cools, and condenses at the dew point.
  • US weather generally moves west to east.
  • Warm air rises (less dense); cold air sinks (more dense).
  • Hurricanes form over warm oceans, weaken over land or cool water.

Water Cycle & Soil

  • Infiltration occurs on permeable, unsaturated, gentle, unfrozen land; runoff when impermeable, saturated, steep, frozen.
  • Porosity is the percentage of empty space in soil and doesn't depend on particle size.
  • Permeability measures water flow through soil; larger particles increase permeability.
  • Capillarity is upward water movement; decreases with larger particles.

Key Terms & Definitions

  • Density — mass per unit volume, indicating compactness.
  • Latitude/Longitude — geographic coordinates for location.
  • Polaris — North Star, used to determine latitude in the Northern Hemisphere.
  • Isolines — lines of equal value on maps (e.g., elevation, pressure).
  • Igneous/Sedimentary/Metamorphic — three rock types, based on formation.
  • Weathering — breakdown of rocks; chemical or physical.
  • Delta — landform where river meets ocean and deposits sediment.
  • Convection Current — movement in mantle causing plate tectonics.
  • Half-life — time for half a radioactive substance to decay.
  • Barometer/Anemometer/Wind Vane — instruments for air pressure, wind speed, and direction.
  • Coriolis Effect — deflection of moving fluids due to Earth’s rotation.

Action Items / Next Steps

  • Review ESRT for identifying rocks and interpreting maps.
  • Practice calculating half-life using provided charts.
  • Prepare flashcards for key terms and rock identification features.