Earth Materials and the Cycle of Rock Transformation Flashcards
(35 cards)
______ the outermost layer of the planet
earths crust
Crust’s thickness ranges between
n 8 to 80 km and comprises the continents and ocean basin
the thickness of the oceanic crust is generally
less than 10 k
continental crust
averages about 40 km
About 10 percent of the crust exceeds 50 km, with the greatest thickness reported in the ________, where it is about 80 km
Himalayas
mineral definition
A mineralcan be defined as a naturally occurring, inorganic substance that has a definite chemical composition and a characteristic atomic structure. This gives each mineral its distinctive properties, such as colour, lustre, and hardness. Most minerals have a crystalline structure that reflects the internal arrangement of its composing atoms
When minerals are combined they form
rock
are solidified from mineral matter in a high temperature molten state. The mineral grains in igneous rocks are tightly interlocked, and the rock is normally very strong
igneous rock
magma
cools and solidifies between about 600 and 1,200 °C, either below the surface as intrusive rocks, such as granite, or on the surface as extrusive rocks, such as volcanic lava
Layered accumulations of mineral particles which are derived mostly by weathering and erosion of pre-existing rock lead to the formation of
sedimentery rock
Diagenesis
reveals the various chemical, physical, and biological changes that occur as layers of sediment transform into rocks. The resulting rock layers are called strata.
s are the most common exposed rock types and cover about 75 percent of the Earth’s surface. However, they account for only about 5 percent of the total mass of the Earth’s rocks because they are only found within a comparatively thin layer over igneous and metamorphic rock
sedimentery rocks
Unlike igneous and metamorphic rocks, sedimentary rocks often contain______
fosils
When igneous or sedimentary rocks are physically or chemically changed, due to the subsequent application of heat and pressure during episodes of significant crustal movement, they turn intto
metamorphic rocks
The process of metamorphismcreates new minerals and rock structures
formation of igneou rock
Igneous rock crystallizes from hot, molten magma that originates deep below the surface of the Earth. The molten rock migrates upward from the magma chambers through fractures in older solid rock and eventually solidifies within (igneous intrusive rock; intrusion) or on top (extrusive igneous rock; lava) of the Earth’s crust
The _________ and ______are the main determinants of rock composition and crystal size
chemical composition of the magma and the rate of cooling
the _____________ that form igneous rocks are chemical compounds that contain silicon and oxygen atoms, combined with various proportions of other elements, particularly aluminum, iron, calcium, sodium, potassium, and magnesium
silicate minerals
quartz
) is one of the most common minerals. It is quite hard and resists chemical breakdow
silicate aluminim minerals
feldspars
Quartz and feldspar form the ______mineral group
felsic
These minerals are light in colour (white, pink, or grayish) and lower in density than the other silicate minerals; they form at comparatively low temperatures.
Other common silicate minerals include the biotite, amphibole, and pyroxene groups. All three contain aluminum, magnesium, iron, and potassium or calcium. These minerals are described as __________
mafic
(“ma” for magnesium; “f ” from the chemical symbol Fe for iron).
All of these mafic minerals are dark in colour(usually black) and are denser than the felsicminerals. The mafic minerals are characteristically found in rocks that solidify at high temperature
Granite is one of the most common intrusive igneous rocks. Typical graniteconsists mainly of potassium feldspar, with lesser amounts of quartz and Na-plagioclase, and some mica and amphibole. Because most of the volume of granite is of felsicminerals, granite is classified as _________
felsic igneou rock
rocks cool very slowly — over hundreds or thousands of years — and, as a result, develop large, readily seen crystals (granite and diorite are good examples of coarse-textured intrusive igneous rocks).
intruive rocks
which cools rapidly, is fine-textured, and the individual crystals can only be seen through a microscope. Most lava solidifies as a dense, uniform rock with a dark, dull surface. Sometimes lava cools to form shiny obsidian or volcanic glass. If the lava contains dissolved gases, it may solidify to form scoria, a rock with a frothy, bubble-filled texture.
extrusive rocks