WorksheetsESS Unit 1 Review
Total questions: 25
Worksheet time: 29mins
What is potential renewable?
Potential renewable is the fixed quantity in earth's crust that takes thousands-millions of years to produce.
Potential renewable is a resource that on a human time scale is inexhaustible.
Potential renewable is a resource that can be replenished fairly rapidly through natural processes.
What is an example of non-depletable?
An example of non-depletable is wind.
An example of non-depletable is wood.
An example of non-depletable is natural gas.
An example of non-depletable is coal.
Explain the difference between non-renewable and renewable
(a)
Fill in the blanks. (start with magma going clockwise)
(a)
How can we save nonrenewable resources?
(a)
Explain the difference between energy conservation and energy efficiency.
(a)
Distinguish the difference between photovoltaic systems and concentration solar electricity generation?
(a)
Identify a characteristic of silicates.
A characteristic of silicates is it contains silicon.
A characteristic of silicates is it's less complex.
A characteristic of silicates is it doesn't contain silicon.
How to identify minerals by luster?
Variety of colors is a way to identify minerals by luster.
Resistance of being scratched is a way to identify minerals by luster.
Reflection of light is a way to identify minerals by luster.
How to identify minerals by hardness?
Reflection of light is a way to identify minerals by hardness.
Resistance of being scratched is a way to identify minerals by hardness.
Powdered color when rubbed against a hard surface is a way to identify minerals by hardness.
How do identify minerals by streak?
Powdered color when rubbed against a hard surface is a way to identify minerals by streak.
Reflection of light is a way to identify minerals by streak.
Resistance of being scratched is a way to identify minerals by streak.
How to identify minerals by density?
Reflection of light is a way to identify minerals by density.
Weight is a way to identify minerals by density.
Powdered color when rubbed against a hard surface is a way to identify minerals by density.
Choose the correct statement of reserve in minerals.
Reserve is accessible in minerals.
Reserve is inaccessible in minerals.
Reserve is unfound in minerals.
Reserve is not profitable in minerals.
Choose the correct statement for resources in minerals.
Resources are accessible in minerals.
Resources are unfound in minerals.
Resources are profitable in minerals.
What is another word for renewable?
Non-depletable is another word for renewable.
Potential renewable is another word for renewable.
Non-renewable is another word for renewable.
Where is sublimation from?
Sublimation is from lava.
Sublimation is from volcanic gases.
Sublimation is from aqueous solutions.
Where is crystallization from?
Crystallization is from lava.
Crystallization is from volcanic gases.
Crystallization is from aqueous solutions.
Where is deposition from?
Deposition is from lava.
Deposition is from volcanic gases.
Deposition is from aqueous solutions.
What is surface mining?
Surface mining is the removal of ores, sand, gravel, and stone my digging holes with machines.
Surface mining is the removal of minerals close to Earth's surface.
Surface mining is the removal of the tops of mountains to expose coal.
What is batholith in Igneous Rock?
Batholith is a large intrusion with an exposed area of over 100 square miles.
Batholith is a dome-like intrusion that forms between rock layers.
Batholith is a sheet-like intrusion that forms between rock layers.
What is a Dike in Igneous Rock?
Dike is similar to batholith but less than 100 square miles.
Dike is an upside-down Laccolith.
Dike is a narrow, vertical intrusion that cuts through rock layers.
Choose the correct definition for Metamorphic Rocks.
Metamorphic rocks has formed when lava cools quickly on earth's surface.
Metamorphic rocks has been changed by great heat and pressure.
Metamorphic rocks are composed of sediments that have been cemented and compacted together.
What is physical weathering?
Physical weathering is when rocks break apart without changing their chemical composition.
Physical weathering is when rocks slowly dissolve by chemical reactions.
Physical weathering is when rocks break down by plant and animal activity.
How are organic sedimentary rocks formed?
Organic sedimentary rocks are formed from sediment pieces of various sizes.
Organic sedimentary rocks are formed directly or indirectly from materials that were once living.
Organic sedimentary rocks are formed by various chemical means.
Where is the oldest layer of the rock located?
The oldest layer of rock is located at the top.
The oldest layer of rock is located in the middle.
The oldest layer of rock is located at the bottom.
