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ESO Y4B · Biology and Geology
The dynamic Earth · The history of the Earth

Geological cross-sections

Sedimentary rocks build up layer by layer, like the pages of a book written from the bottom up. A geological cross-section is, in that sense, the open book: a small number of simple principles is enough to read the order in which everything happened.

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 of stratigraphy

If you look at a roadside cutting you can see layers of limestone tilted at $40^\circ$, yet if you look today at the bed of any lake or bay, the sediments always lie flat: how did those layers come to lose their horizontal arrangement?

Cross-section of an outcrop with four horizontal sedimentary strata stacked on top of one another, numbered from 1 (oldest, at the base) to 4 (youngest, at the top); an arrow shows that the order of deposition runs from bottom to top. 4th, youngest 3º 2º 1st, oldest order of deposition Undisturbed series: the strata remain 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 geological cross-section in full

Geological cross-section with three horizontal strata numbered from 1 (bottom, oldest) to 3 (top). A normal fault cuts through them and moves the right-hand block downwards. A dyke of magmatic rock cuts through the three strata and the fault without being displaced, 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

In cliffs such as those at Siccar Point (Scotland), almost horizontal strata rest on top of completely vertical layers that have been cut off at an angle: what geological event explains why 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 are folded, erosion trims the crests until a truncated surface is left, and a new horizontal layer is deposited on top, ending with the unconformity shown in the figure. unconformity older 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

Two cliffs thousands of kilometres apart show identical sandstones, but one contains ammonite shells and the other trilobite remains: how can we know which was deposited first if there is no physical continuity between them?

Two very distant geological cross-sections, A and B, with different strata. In both there is a stratum containing the same index fossil, an ammonite, although it is sandstone in one and limestone in the other. A dashed band joins the two strata and shows that they are the same age, with no physical continuity between the outcrops. same index fossil same age sandstone limestone thousands of km no physical continuity section A section B
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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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