Minerals form when water evaporates. Like when salt water evaporates it makes halite.
Answer:
1/3 gallon
Explanation:
Gallon of honey remaining = 3/4 gallons
Gallon of honey needed for bread = 1/6
Gallon of honey needed for cookies = 1/4
Total gallon of honey used for loaves of bread and cookies
= 1/6 + 1/4
= (4+6)/24
= 10/24
= 5/12
Total gallons of honey left over = Gallon of honey remaining - gallon of honey used
= 3/4 - 5/12
= 9-5/12
= 4/12
= 1/3 gallon
Gallon of honey leftover = 1/3 gallon
Answer:
glass like.
Explanation:
Like obsidian, if you break it it will be really sharp.
B) Materials in Solution is NOT a process of a stream load
Streams must start somewhere. Streams are formed by having
sufficient water supply. The supply comes from rainfall and
underground reservoirs. The area that initiates the stream
supply is called the headwaters. Many times headwaters start
in the high elevations. As the water moves down through the
mountains, the stream’s pathway is formed. As streams evolve, the path of the stream starts to curve. The
curving of a stream channel is known as a meander. As meanders
develop, they become broader and larger. Eventually,
there are enough material deposits to form a blockage of two
meanders. This development causes the formation of an
oxbow lake.
<u>Answer:
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The ranking of common igneous silicate minerals based on the temperature at which crystallization occurs is called Bowen’s reaction series.
<u>
Explanation:
</u>
In Bowen’s reaction series the minerals with high crystallization temperature are present at the top layer. This means these minerals are the first to crystallize from the magma and they are mostly unstable. The Bowen's reaction series is represented in the Y shape. The left branch of this Y has minerals containing iron and magnesium. They are called as Ferromagnesium minerals.
The right branch of the Y contains plagioclase feldspars minerals. Temperature gradually decreases down along the Bowen’s reaction series from 
to 
. At certain low temperature, the two branches combine forming minerals similar to felsic rocks such as orthoclase feldspar, quartz and muscovite mica.
