GEY1112_L06_EnvironmentsDeposition_JElyWasinger
docx
keyboard_arrow_up
School
Front Range Community College *
*We aren’t endorsed by this school
Course
1112
Subject
Geology
Date
Dec 6, 2023
Type
docx
Pages
6
Uploaded by CountAlligator3653
GEY1112
Name: Jay Ely-Wasinger
Date: October 4
th
, 2023
Class/section: GEY1112-C11
Instructor: Kristin Quadracci
Lab Partner(s): Kenzie, Tesla, Ryder
(emotional support)
Lab 6 – Environments of Deposition
Original, completed Lab Notebook pages for the following are included in this
Lab submission:
I. Pre-lab questions
II. Experiment 1
III. Post-lab questions
Environments of Deposition
Please note: for any questions that require additional research, consider using Google
Scholar instead of Google. Also, any information taken/used from a source should be
properly cited.
PRE-LAB QUESTIONS
1.
What does grain size, sorting, and rounding tell you about a depositional environment?
2.
Imagine a climate change event transformed a sea into an arid, hot environment. What
sort of deposits might you see in the resulting strata?
3.
A bed is dark grey or black. What might this indicate about the composition of the parent
material?
Environments of Deposition
EXPERIMENT 1: RECONSTRUCTING ENVIRONMENT OF
DEPOSITION
Data Sheet
Table 1. Sedimentary Rock Classification
Sample
Clast Shape
Grain Size
Composition
Other Observations
Rock Name
E
G
H
I
J
K
Environments of Deposition
Your preview ends here
Eager to read complete document? Join bartleby learn and gain access to the full version
- Access to all documents
- Unlimited textbook solutions
- 24/7 expert homework help
Table 2. Common Sedimentary Rocks
Rock Type
Particle Size
Composition
Comments
Rock Name
Clastic
Very coarse–Coarse
(> 2.0 mm)
Any rock or
mineral
Rounded clasts; poorly- to well-
sorted
Conglomerate
Clastic
Very coarse–Coarse
(> 2.0 mm)
Any rock or
mineral
Angular clasts; poorly- to well-
sorted
Breccia
Clastic
Coarse–Medium
(0.06—2.0 mm)
Quartz, feldspars
Feels sandy; some grains
visible to the naked eye; poorly-
to well-sorted
Quartz
Sandstone
Clastic
Fine
(0.004—0.06 mm)
Clays, quartz
Feels gritty; some grains visible
through a hand lens; well sorted
Siltstone
Clastic
Very Fine
(< 0.004 mm)
Clays, quartz
May be foliated; no visible
grains; well-sorted
Shale
Chemical
Varies
Halite
Tastes like salt; individual
mineral crystals form three right
angles
Rock Salt
Chemical
Varies
Gypsum
Softer than fingernail; can be
pink, white, or transparent
Rock Gypsum
Chemical
Varies
Dolomite
Reacts in dilute acid only when
powdered
Dolostone
Chemical
or Biogenic
Microcrystalline
Quartz and/or
quartz-based
fossils
Exhibits sharp edges and
breaks like glass; smooth to the
touch
Chert
Biogenic
Varies
Calcite and
calcite-based
fossils
Small fossils or impressions are
present; reacts with dilute acid
Fossiliferous
Limestone
Biogenic
Varies
Carbon-based
material
Plant remains may be visible;
black-brown color
Bituminous
Coal
Environments of Deposition
Table 3: Sedimentary Rock Characteristics
Sampl
e
Clast
Shape
Grain Size
Sorting
Color
Rock Name
E
G
H
I
J
K
Table 4: Environment of Deposition Characteristics
Sample
Rock Name
Mineral
Composition
Near/Far from
Source
High/Low Energy of
Deposition
E
G
H
I
J
K
Environments of Deposition
Post-Lab Questions
1.
Write a full description of the environment of deposition for each rock. Include details
such as climate, wildlife, landforms, and surface water features. Include any details you
can infer about the rock’s weathering history and its journey prior to deposition.
a.
Rock E:
b.
Rock G:
c.
Rock H:
d.
Rock I:
e.
Rock J:
f.
Rock K:
4.
Did any of the rocks exhibit evidence of an organism-rich environment? If so, indicate
the rock(s) and explain the evidence.
5.
What is the parent material for Rock G? Explain your reasoning.
6.
Field examinations are often more useful in determining environment of deposition than
hand samples. Why do think this is true? Give one example of a sedimentary structure
you might see in the field but would not see in this lab. Explain how this structure is
formed.
Your preview ends here
Eager to read complete document? Join bartleby learn and gain access to the full version
- Access to all documents
- Unlimited textbook solutions
- 24/7 expert homework help