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The dynamic Earth · The history of the Earth

Geologic Cross-Sections

If you look at a road cut along the federal highway that climbs to the pyramids of Teotihuacan or into the Sierra Madre, you will see layers of rock stacked like the pages of a book. But some of them are tilted, even though the bottom of a lake or the Gulf of Mexico always builds up flat sediment. How did those layers end up tilted, and how do we know what happened first? A few simple principles are enough to read that book.

The Principles of Stratigraphy

Strata are the layers of sedimentary rock. To put their histories in order, geologists use three rules of relative dating: they tell us what is older and what is younger, without giving years.

Cross-section with four horizontal strata numbered from 1 (oldest, at the base) to 4 (youngest, on top); an arrow indicates that the order of deposition goes from bottom to top. 4th, youngest 3.º 2.º 1st, oldest order of deposition Undisturbed series: the strata are still horizontal
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State the principle of original horizontality and explain what must have happened if today we find tilted or folded strata.

State the principle of original horizontality and explain what must have happened if today we find tilted or folded strata.

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Four undisturbed horizontal strata appear in a cross-section: sandstone, mudstone, limestone and conglomerate, from bottom to top. Apply the principle of superposition…

Four undisturbed horizontal strata appear in a cross-section: sandstone, mudstone, limestone and conglomerate, from bottom to top. Apply the principle of superposition to state which is the oldest and which is the youngest, and justify your answer.

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Interpreting a Complete Geologic Cross-Section

Cross-section with three horizontal strata numbered from 1 (bottom, oldest) to 3 (top). A fault cuts through them and moves the right block downward. A dike of magmatic rock cuts through the three strata and the fault, so it is the most recent event. 3 2 1 stratum 3 youngest stratum 2 stratum 1 oldest 4 · fault 5 · magmatic intrusion Order: 1 → 2 → 3 → 4 → 5 superposition (1–3) · cross-cutting (4 and 5)
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In the geological cross-section shown in the diagram, five strata (A, B, C, D and E), an erosion surface (W) and a fault (X) are indicated. Order these events from…

In the geological cross-section shown in the diagram, five strata (A, B, C, D and E), an erosion surface (W) and a fault (X) are indicated. Order these events from oldest to youngest: formation of the five strata, erosion that caused W, and movement of fault X. State which principle you apply at each step.

A B C W D E X
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A fault cuts through a series of strata and, in turn, is cut by an igneous dyke. Apply the principle of cross-cutting relationships to order these three events:…

A fault cuts through a series of strata and, in turn, is cut by an igneous dyke. Apply the principle of cross-cutting relationships to order these three events: formation of the strata, movement of the fault, and intrusion of the dyke.

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A student examines a geological cross-section showing three folded strata (1, 2, and 3), an erosion surface over them, two upper horizontal strata (4 and 5), and a fault…

A student examines a geological cross-section showing three folded strata (1, 2, and 3), an erosion surface over them, two upper horizontal strata (4 and 5), and a fault that cuts across all strata from the base to the surface. In their report, they state:

"The fault is older than strata 4 and 5 because faults originate at great depth, and the folding occurred after stratum 5 was deposited, but only affected the lower ones because they are softer rocks."

  1. a) Refute the student's two errors in a justified manner by applying the principles of superposition of strata, original horizontality, and cross-cutting relationships.
  2. b) Deduce the actual geological history of the area by arranging all events in chronological order (stages of sedimentation, tectonic deformation, and erosion).
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Unconformities

Go back to the question at the beginning: sometimes horizontal strata appear resting on tilted layers that have been beveled off. What happened so that millions of years of record are missing between the two packages of rock?

Animation of the formation of an angular unconformity in an 18-second loop: the horizontal strata fold, erosion trims the crests until a truncated surface is left, and a new horizontal layer is deposited on top. unconformity oldest strata
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Explain what an angular unconformity is and describe, step by step, the sequence of processes (sedimentation, deformation, erosion and new sedimentation) required to…

Explain what an angular unconformity is and describe, step by step, the sequence of processes (sedimentation, deformation, erosion and new sedimentation) required to form it.

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The Principle of Correlation and Index Fossils

Imagine two identical sandstone outcrops, one in Oaxaca and another thousands of kilometers away: one contains ammonites and the other trilobites. There is no physical continuity between them. How can we tell which one was deposited first?

Two widely separated geologic cross-sections, A and B, with different strata. In both, a stratum with the same index fossil, an ammonite, appears, although in one it is sandstone and in the other limestone. A dashed band joins the two strata and indicates that they are the same age. same index fossil same age sandstone limestone thousands of km no physical continuity section A section B

Go back to the beginning: ammonites and trilobites cannot be put in order just because they are in different outcrops, but they can be by their position on the index fossil scale: trilobites are from the Paleozoic and ammonites from the Mesozoic, so ammonites are younger.

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What is an index fossil? Explain what conditions a fossil must satisfy to be useful as an index fossil, and how it is used to correlate strata from different regions.

What is an index fossil? Explain what conditions a fossil must satisfy to be useful as an index fossil, and how it is used to correlate strata from different regions.

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During a geological survey, a series of strata is found where a layer containing trilobite fossils is located geometrically above another layer containing ammonite…

During a geological survey, a series of strata is found where a layer containing trilobite fossils is located geometrically above another layer containing ammonite fossils. An amateur concludes that trilobites outlived ammonites and evolved during the Mesozoic.

  1. a) Refute the amateur's conclusion by explaining what the principle of faunal succession consists of and what role both groups play as index fossils.
  2. b) Propose and justify two different tectonic hypotheses (specific geological structures) that explain how the positions of these strata could have become inverted.
  3. c) What sedimentary structure or criterion would you look for in the strata to verify in the field whether the geological sequence is inverted or not?
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In two stratigraphic columns separated by $50\ \text{km}$, completely different lithologies are observed: column A is composed of massive marine limestones and column B…

In two stratigraphic columns separated by $50\ \text{km}$, completely different lithologies are observed: column A is composed of massive marine limestones and column B of dark shales. However, at one level in both columns the same ammonite species appears (Hildoceras bifrons).

  1. a) Justify why correlating these columns based solely on rock type (lithology) would have led to an error regarding their contemporaneity.
  2. b) Explain what two biological or taphonomic characteristics make Hildoceras bifrons a reliable index fossil to state that both strata are of the same age.
  3. c) If a sandstone layer identical to another in column A is detected in column B, but located $20\ \text{m}$ above the Hildoceras level, can it be deduced that both sandstones formed simultaneously? Justify your answer using the principles of stratigraphic correlation.
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Summary

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