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The dynamic Earth · The history of the Earth

Geological cross-sections

Before you start, make sure you know: Rocks and the rock cycle (Grade 6 Science (middle school))
Before you start, make sure you know: Landform shaping (Grade 7 Science (middle school))

Sedimentary rocks build up layer by layer, like the pages of a book written from the bottom up. Scientists use this layered evidence to build the geologic time scale (NGSS MS-ESS1-4). 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.

The principles of stratigraphy

If you look at a road cut along a highway in the Appalachians you can see layers of limestone tilted at $40^\circ$, yet if you look today at the bed of Lake Michigan or Chesapeake 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 3rd 2nd 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 dike 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 · igneous dike 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 dike. 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 dike. Apply the principle of cross-cutting relationships to order these three events: formation of the strata, movement of the fault, and intrusion of the dike.

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Unconformities

In the Grand Canyon, perfectly horizontal strata rest on top of tilted layers that have been cut off at an angle (the Great Unconformity): 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

The principle of correlation and index fossils

Two cliffs thousands of miles 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 miles no physical continuity section A section B

Summary

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