Image of cross-bedded rocks

Example of cross-bedding in Nova Scotia • Michael C. Rygel (CC BY SA 3.0)

Reading the rocks

In his book Con­ver­sa­tions with the Earth, Ger­man geol­o­gist Hans Cloos described the moment when he “became a geol­o­gist for­ev­er.” It did not hap­pen at uni­ver­si­ty. It did not hap­pen with the pass­ing of an exam or the award­ing of a degree. It hap­pened one morn­ing in Naples, Italy, when Cloos opened the win­dow of his hotel room and saw the smok­ing cone of Vesu­vius loom­ing above the still-sleep­ing city. At that moment he had the real­iza­tion that moti­vat­ed a life­time of cre­ative work in geol­o­gy: The Earth is alive.

Image of the Earth from space

The Hawaiian Islands • eol.jsc.nasa.gov (Public Domain)

CAT scanning Earth

In geol­o­gy, before the 1960s, we were taught the Earth was “as sol­id as a rock.” And we were told the sur­face of the Earth had always looked more or less the way it looks today, the same con­ti­nents, the same ocean basins. Oh yes, there had been changes on the sur­face, crin­klings and fold­ings that lift­ed moun­tains or cracked the crust, ver­ti­cal move­ments most­ly, like the wrin­kles on the skin of an orange.

Image of the sealed Kola borehole

The sealed and abandoned Kola Superdeep Borehole in 2012 • Photo by Rakot13 (CC BY SA 3.0)

Image of glacial striations

Glacial scratches • Photo by Amezcackle (Public Domain)

Ice works the land

Set a geol­o­gist down any­where in New Eng­land and some­where near­by he will show you the work of ice. Eigh­teen thou­sand years ago all of New Eng­land lay beneath a half-mile-thick sheet of ice, part of a con­ti­nent-span­ning glac­i­er that reached from the deeply indent­ed coast of the Pacif­ic North­west to the gen­tly slop­ing con­ti­nen­tal shelf of New England.

Artist's impression of a protoplanetary disc

Artist's impression of a protoplanetary disc • ESO/L. Calçada (CC BY 4.0)

The sands of time

The ingre­di­ents of life on Earth were col­lect­ed by grav­i­ty. The hearth that held the tin­der and received the spark of life was a small heavy-ele­ment plan­et near a yel­low star. Chem­istry was the steel and time the flint that struck the spark. For the spark to catch and the flame to grow required not bib­li­cal days, but hun­dreds of mil­lions of years. The solar sys­tem has been around for four and a half bil­lion years. That’s time enough for miracles.

Photo of rocks carried by glacier

Photo by Matt Gross on Unsplash

The rock asks that its story be read

Every rock, every peb­ble, every grain of sand has a sto­ry to tell of the evo­lu­tion of the earth. Every blade of grass is a poem of the past. Our own bod­ies are muse­ums of our his­to­ry, our cells are the scrap­books of our micro­bial ances­tors, we breathe the exha­la­tions of bac­te­ria that swam in ancient seas. The sto­ry of the earth is wait­ing to be read.