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ESO Y4A · Biology and Geology
The dynamic Earth · The history of the Earth

Geological cross-sections

If you cut a layered cake, you know that the bottom layer was put down first and the top one last. Sedimentary rocks pile up in a similar way, and this very simple idea is the basis of almost all historical geology.

Before you start, make sure you know: Rocks and the rock cycle (1st ESO)
Before you start, make sure you know: The shaping of relief (3rd ESO)

The principles for ordering strata

Looking at the walls of the Grand Canyon, we see hundreds of metres of rock divided into horizontal layers visible to the naked eye. How can we work out which of those layers formed first and which formed later without having been there to witness it?

Series of four horizontal superimposed strata, ordered from oldest at the bottom to youngest at the top. 1st, oldest 2º 3º 4th, youngest
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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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Reading a geological cross-section

Geological cross-section with three horizontal strata, number 1 the oldest at the bottom and number 3 the youngest at the top. A fault cuts them and drops the right-hand block. A magma dyke passes through the three strata and the fault without being displaced, so it is the most recent event. fault magmatic intrusion (dyke) stratum 3 (youngest) stratum 2 stratum 1 (oldest) Order of events stratum 1 → stratum 2 → stratum 3 → fault → intrusion
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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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Unconformities

On many coastal cliffs we can see a set of completely vertical strata and, right on top of them, another series of perfectly horizontal strata. What geological events could have caused such a change in orientation between one set of layers and the other?

Geological cross-section of an angular unconformity: old folded strata truncated by an irregular erosion surface, on which more recent horizontal strata rest. Angular unconformity horizontal strata (more recent) unconformity (erosion surface) folded strata (older)
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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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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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Index fossils

Two geology teams discover clay strata of almost identical appearance in Spain and in South America, but the Atlantic Ocean makes it impossible to follow the physical continuity of the rock. How can we find out whether both layers formed in the same period of the Earth's history?

Two distant stratigraphic cross-sections, in Spain and in South America, separated by the Atlantic Ocean: the same index fossil, an ammonite, appears in a limestone stratum in each cross-section and makes it possible to correlate them as strata of the same age. section A · Spain section B · South America same index fossil (ammonite) same age Atlantic Ocean (no physical continuity) sandstone clay limestone
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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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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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Summary

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