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GEOTOUR GUIDE - City of Kamloops

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hoW did all These GeoloGiCal maTerials form?<br />

a quick tOur thrOugh geOlOgic time.<br />

How old is <strong>Kamloops</strong>? Well, European settlement <strong>of</strong> the <strong>Kamloops</strong> area goes back to the mid 1800s. However, First Nations<br />

settlement in the region is much older and likely goes back several thousand years. But the land itself is much, much, much older.<br />

What follows is a brief summary <strong>of</strong> the geological history that geologists have pieced together for the <strong>Kamloops</strong> region.<br />

a BooK WiTh mosT paGes missinG<br />

Imagine the analogy <strong>of</strong> viewing the Earth as a story book, or more accurately, a library <strong>of</strong> books. In its many pages are recorded,<br />

in rock and fossil, the Earth’s history. Each volcanic eruption, each flood deposit, each slow burial <strong>of</strong> mud and animal and plant<br />

remains on the seafloor is another page. Each region on Earth is a separate book, recording the history <strong>of</strong> that place. However,<br />

when geologists try to read the story we find that most <strong>of</strong> the pages are missing. Only a few pages remain. Why? Erosion is the<br />

answer. Erosion is continually removing geological materials and the records they contain. Few geological materials escape<br />

erosion. Today, most <strong>of</strong> British Columbia is eroding, bit by bit, by river scour, glacier grind, rock fall, and land slide. We lose<br />

“pages” every year. Geologists work with the remaining scraps <strong>of</strong> the story to piece together the geological history <strong>of</strong> a place<br />

such as <strong>Kamloops</strong>.<br />

Figure 5. The geological history <strong>of</strong> the <strong>Kamloops</strong> region is presented as a clock. Each ancient geological<br />

event is recorded in a geological material and the fossils that it contains. Much ancient history has been<br />

destroyed by erosion <strong>of</strong> the geological materials over geological time, leaving many gaps in the history.<br />

4

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