GEOL 1301 - Lab 03 - Igneous Rocks (1)
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University of Texas, Arlington *
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1301
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Geology
Date
Feb 20, 2024
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GEOL1301 Name: Jonathan Venegas Igneous Rock Labs
Learning and Lab objectives:
Igneous rocks form from magma, lava, or pyroclastic material and are classified according to their
composition and texture. In this lab, you are learning to identify a set of common igneous rocks, like
the way you identified minerals in Lab 1. However, for Lab 2 your samples are rocks, which are
formed of several different minerals instead of one isolated mineral. Nevertheless, you will see
minerals that you recognize from last week so keep an eye out for familiar names.
The categorization of igneous rocks relies on both texture and color of the sample. In the case of
igneous rocks, the color of the rock (the grayscale) is an excellent indicator of the history of the
molten rock. This is separated into three categories (mafic, intermediate, felsic). The simple
classification of the color of an igneous rock can be used to determine critical facets of the history of
the molten rock that it crystallized from, such as the plate tectonic setting the magma moved through
or the type of volcano that extruded the lava.
Terminology and lab instructions:
At the beginning of the lab your lab instructor will review the important terminology below, which was
gone over in lecture last week. They will also introduce some of the common igneous rocks and their
formation mechanisms. Please complete Table 1 on page 2 of this lab and submit it to your instructor.
Don’t forget to put your name on the worksheet!
List of textures
A list of adjectives used to describe the
overall composition
Intrusive
Extrusive
Porphyritic
Glassy
Pyroclastic/fragmental
Vesicular/frothy
Felsic (light)
Intermediate (between light and dark)
Mafic (dark)
We have also included two good, online identification keys:
http://geology.about.com/od/rocks/a/Rock-Tables.htm
https://australian.museum/learn/minerals/shaping-earth/classification-of-igneous-rocks/
Samples included in this lab are:
Basalt
Basalt Porphyry
Gabbro
Granite
Obsidian
Rhyolite
Scoria
Volcanic Tuff
1
Name: Jonathan Venegas
Table 1: Observations and classifications of rock samples. Sample
Number
Texture
Composition/
Grayscale
Other Observations (Visible
Minerals, Special Features…
Rock Name
Origin (How did
the rock form?)
1
Glassy
Mafic/Dark
Deep black with no visible
crystals
Obsidian
Extrusive formed
by rapid cooling
of lava on the
volcano
2
Aphanitic
Felsic/Light
Light brown no air bubbles or
crystals.
Rhyolite
Extrusive formed
by rapid cooling
of magma
3
Porphyritic
Intermediate
Greyish Black, Small crystals,
No
air
bubbles,
small
fragments
Gabbro
Intrusive formed
by slow cooling of
magnesium and
iron-rich magma
deep in earth's
surface
4
Phaneritic
Felsic or Light
Pink with slight grey and black,
large crystals
Granite
Intrusive Product
if
melting
of
continental rocks
smoothness is a
result of its area
being
near
subduction zones
5
Aphanitic
Mafic/Dark
Black, no crystals or rock
fragments and air bubbles.
Basalt
Extrusive formed
of rapid cooling of
basaltic
lava
formed near the
interior of the
crust
and
2
exposed at the
very tip of the
earth’s surface 6
Porphyritic
Mafic/Dark
Black, visible large crystals,
No rock fragments, or bubbles
Basalt Porphyry
Intrusive formed
from
molten
rock/lava
cools
underground and
then erupts onto
earths surface
7
Pyroclastic/
Fragmental
Felsic/Dark
Light brown, visible crystals,
visible rock fragments, and no
air bubbles
Volcanic Tuff
Extrusive made
from volcanic ash
that ejects during
volcanic eruption
essentially
compact
and
cemented
volcanic ash
8
Vesicular
Frothy
Intermediate/
Light and dark
Reddish Brown in color, no
crystals no rock fragments and
visible air bubbles
Scoria
Extrusive magma
contains
abundant
dissolved
gas
from volcano
3
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