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Science Moab: When the rivers ran backwards


Science Moab talks with Andre Potochnik about how adjustments in river drainages mirror higher panorama motion

Hundreds of thousands of years in the past, streams and rivers that had run into the guts of the rustic throughout what’s now the Colorado Plateau reversed as new mountain levels rose up, sending water in the wrong way and into the Pacific Ocean. 

Through finding out deposits of river gravels, Andre Potochnik has been in a position to search out proof of primary adjustments within the drainages at the southern a part of the Colorado Plateau. Science Moab talked with Andre about his paintings in Arizona at the Apache Reservation and the way he has get a hold of the timing of important drainage reversals for rivers and the way this knowledge affects interpretations of the Colorado River and the Grand Canyon.

Science Moab: What did the panorama seem like over the past 60 million years, and what resulted in without equal reversal of drainage patterns at the Colorado Plateau?

Potochnik: Starting round 80 million years in the past, streams flowed northeast from a big mountain vary that existed south of the Colorado Plateau. Those rivers most likely ended up flowing all of the method to the Mississippi River embayment. Round 30 million years in the past, plate tectonics modified between the Pacific plate and the North American plate in one of these method that the compressional stresses at the continent had been launched, and the continental crust then started to unfold out to the east and west. This led to the traditional mountain gadget south of the plateau that we name the Mogollon Highland to cave in, making all of the southern fringe of the plateau gently flex backpedal towards the southwest. This led to without equal reversal of the drainages.

Science Moab: May you provide an explanation for how finding out deposits of historical river gravels and terraces has helped you already know the relative glide of historical rivers?

Potochnik: Paleo-current signs, which point out the route of glide, can also be ascertained by way of a couple of other strategies. The primary one I exploit is known as “movement imbrication,” which is the layering of gravels of various sizes. Those gravels constitute motion alongside the channel backside, and the motion of those gravels involves a forestall when the river flood that’s wearing them subsides. Since most of the boulders have a tendency to have some flat size to them, they’ll have a tendency to layer such that they’re tilted upward within the route of glide, which is the the attitude at which they’re least more likely to get transported additional. Through measuring loads and loads of measurements over an excessively huge area, I used to be in a position to piece in combination the glide instructions for a given locality.

Science Moab: How are you able to practice your paintings to the Colorado River drainage?

Potochnik: If historical canyons had been carved in jap Arizona, then why don’t you in western Arizona as smartly? We even have the proof for historical rim gravels in that house. I become very curious to peer if I may practice what I’ve discovered within the Salt River Canyon [to the Grand Canyon area], since the two areas are very equivalent geographically, and paleo-geographically. The Mogollon Highland prolonged all of the method throughout Arizona to the Grand Canyon area; obviously the Colorado River is passing thru an historical mountain gadget that collapsed in that area as smartly. 

Some of the mysteries of the Grand Canyon is: when did the canyon get lower? There used to be rather a dialogue about this again in 2008, when Rebecca Vegetation studied the uplift of the traditional mountain gadget close to the mouth of the Grand Canyon, and got here up with some numbers for the uplift of the Mogollon Highland in that area of 70-74 million years in the past. The implication used to be that there should were a large uplift at the moment and there should were a large canyon lower into the southern fringe of the Colorado Plateau in western Arizona, suggesting that the Grand Canyon can have begun to be lower by way of historical northeast flowing rivers onto the Plateau from the Mogollon Highland at the moment. 

When the Colorado River discovered its route off of the southern fringe of the Colorado Plateau to the southwest, it merely flowed during the predecessor canyon that had already been carved, very similar to what the trendy Salt River has executed. The Grand Canyon could be so much older than six million years.

​​Science Moab is a nonprofit devoted to attractive group participants and guests with the science going down in Southeast Utah and the Colorado Plateau. To be told extra and pay attention to the remainder of this interview, consult with www.sciencemoab.org/radio



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