"Standards without asterisks represent those that all students are expected to achieve in the course of their studies. Standards with asterisks represent those that all students should have the opportunity to learn."
Earth's Place in the Universe
1. Astronomy and planetary exploration reveal the structure, scale,
and change of the solar system over time.
As a basis for
understanding this concept, students know:
a. how the differences and similarities among the sun,
the terrestrial planets, and the gas planets may have
been established during the formation of the solar
system.
b. evidence from Earth and moon rocks for the solar
system's formation from a nebular cloud of dust and
gas approximately 4.6 billion years ago.
c. evidence from geological studies of the Earth and
other planets that the early Earth was very different
from today.
d. evidence that the planets are much
closer than the stars.
e. the sun is a typical star and is powered by nuclear
reactions, primarily the fusion of hydrogen to form
helium.
f. evidence for the dramatic effects of asteroid impacts
in shaping the surface of planets and their moons, and
in mass extinctions of life on Earth.
g.* evidence for the existence of planets
orbiting other stars.
2. Earth-based and space-based astronomy reveals the structure,
scale, and change over time of stars, galaxies and the universe.
As a
basis for understanding this concept, students know:
a. the solar system is located in an outer edge of the
disc-shaped Milky Way galaxy which spans 100,000
light years.
b. galaxies are made of billions of stars and form most
of the visible mass of the universe.
c. evidence that all elements with an atomic number
greater than that of Lithium have been formed by
nuclear fusion in stars.
d. stars differ in their life cycles, and visual, radio, and
X-ray telescopes collect data that reveal these
differences.
e.* accelerators boost subatomic particles to energy
levels that simulate conditions in the stars and in early
history of the universe before stars formed.
f.* evidence that the color, brightness and evolution of
a star are determined by a balance between
gravitational collapse and nuclear fusion.
g.* how the red-shift from distant galaxies and the
cosmic background radiation provide evidence for the
"big bang" model that suggests that the universe has
been expanding for 10 to 20 billion years.
Dynamic Earth Processes
3. Plate tectonics operating over geologic time has changed the
patterns of land, sea, and mountains on the Earth's surface.
As the
basis for understanding this concept, students know:
a. features of the ocean floor (magnetic patterns, age,
and sea floor topography) provide evidence for plate
tectonics.
b. the principal structures that form at the three different
kinds of plate boundaries.
c. how to explain the properties of rocks based on the
physical and chemical conditions in which they formed,
including plate tectonic processes.
d. why and how earthquakes occur, and the scales
used to measure their intensity and magnitude.
e. two kinds of volcanoes, one with violent eruptions
producing steep slopes and the other with voluminous
lava flows producing gentle slopes.
f.* explanation for the location and properties of
volcanoes that are due to hot spots and those that are
due to subduction.
Energy in the Earth System
4. Energy enters the Earth system primarily as solar radiation and
eventually escapes as heat.
As a basis for understanding this
concept, students know:
a. the relative amount of incoming solar energy
compared with EarthÕs internal energy and the energy
used by society.
b. the fate of incoming solar radiation in terms of
reflection, absorption, and photosynthesis.
c. the different atmospheric gases that absorb the
EarthÕs thermal radiation, and the mechanism and
significance of the greenhouse effect.
d.* the different greenhouse conditions on Earth, Mars,
and Venus, their origins and climatic consequences.
5. Heating of Earth's surface and atmosphere by the sun drives
convection within the atmosphere and oceans, producing winds and
ocean currents.
As a basis for understanding this concept, students
know:
a. how differential heating of the Earth results in
circulation patterns in the atmosphere and oceans that
globally distribute the heat.
b. the relationship between the rotation of the Earth
and the circular motion of ocean currents and air in
pressure centers.
c. the origin and effects of temperature
inversions.
d. properties of ocean water such as temperature and
salinity can be used to explain the layered structure of
the oceans, generation of horizontal and vertical ocean
currents, and the geographic distribution of marine
organisms.
e. the distribution of rain forests and deserts on Earth in
bands at specific latitudes.
f.* the interaction of wind patterns, ocean currents, and
mountain ranges that results in the global pattern of
latitudinal bands of rain forests and deserts.
g.* features of the ENSO cycle (El Ni–o) in terms of
sea-surface and air temperature variations across the
Pacific, and some climatic results of this cycle.
6. Climate is the long term average of a region's weather and
depends on many factors.
As a basis for understanding this concept,
students know:
a. weather (in the short run) and climate (in the long
run) involve the transfer of energy in and out of the
atmosphere.
b. effects on climate of latitude, elevation, topography,
as well as proximity to large bodies of water and cold
or warm ocean currents.
c. how the Earth's climate has changed over time,
corresponding to changes in the Earth's geography,
atmospheric composition and/or other factors (solar
radiation, plate movement, etc.).
d.* use of computer models to predict the effects of
increasing greenhouse gases on climate for the planet
as a whole and for specific regions.
Biogeochemical cycles
7. Each element on Earth moves among reservoirs in the solid Earth,
oceans, atmosphere, and organisms as part of biogeochemical
cycles.
As a basis for understanding this concept, students know:
a. the carbon cycle of photosynthesis and respiration,
and the nitrogen cycle.
b. the global carbon cycle in terms of the different
physical and chemical forms of carbon in the
atmosphere, oceans, biomass, and fossil fuels, and the
movement of carbon among these reservoirs.
c. movement of matter among reservoirs is driven by
the Earth's internal and external sources of energy.
d.* the relative residence times and flows of carbon in
and out of its different reservoirs.
Structure and Composition of the Atmosphere
8. Life has changed Earth's atmosphere and changes in the
atmosphere affect conditions for life.
As a basis for understanding this
concept, students know:
a. the thermal structure and chemical
composition of the atmosphere.
b. how the composition of the Earth's atmosphere has
evolved over geologic time including outgassing, the
origin of atmospheric oxygen, and variations in carbon
dioxide concentration.
c. the location of the ozone layer in the upper
atmosphere, its role in absorbing ultraviolet radiation
and how it varies both naturally and in response to
human activities.
California Geology
9. The geology of California underlies the state's wealth of natural
resources as well as its natural hazards.
As a basis for understanding
this concept, students know:
a. the resources of major economic importance in
California and their relation to California's geology.
b. the principal natural hazards in different California
regions, and the geological basis of those hazards.
c. the importance of water to society, the origins of
California's fresh water, and the relationship between
supply and need.
d.* how to analyze published geologic hazard maps of
California and use the map information to identify
evidence of geological events of the past and predict
geological changes in the future.