A few months ago, the QUEST television program included a segment on various gelatinous marine animals, including jellies, found offshore of central and northern California and featured at the Monterey Bay Aquarium. The beginning of the video segment briefly showed one of the most important habitats for these animals — Monterey submarine canyon. Not unlike on land, features of the undersea landscape have a significant influence on the quantities and diversity of animals. Science involved in understanding the relationship of this “seascape” with submarine ecosystems requires quality maps and the technology to create those maps is improving all the time.

For this post, I simply wanted to show a few images of the canyon and beyond. As readers on my regular blog know, I just love showing images of our planet’s seafloor. We are currently in an age of exploration and discovery when it comes to mapping the seafloor — in many ways it’s like sending probes to another planet. Many of the images I show in this post are from the Monterey Bay Aquarium Research Institute (MBARI), which has not only done a lot of the mapping and science, but has also designed and built the technology to do it. See their page on marine geology, including Monterey canyon, here.

The first image (below) shows the deepest part of Monterey canyon, near the shoreline, cutting across the flat and relatively shallow continental shelf. The yellow arrow represent river sources of sediment that contribute to the longshore currents (red arrows) that funnel the sediment into the canyon and, ultimately, into the deep sea.


In fact, it is the movement of sediment through the canyon that is responsible for creating and sculpting the canyon. Not unlike the Colorado River incising into the Colorado Plateau to create the Grand Canyon, these underwater “rivers” of mud, silt, sand, and water rush down the canyon eroding the canyon little by little. Since I’m bringing up the Grand Canyon, I always like to point out the scale of Monterey submarine canyon with the map below, which compares the two canyon systems at the same scale (also from MBARI).

Grand Canyon (top) and Monterey submarine canyon (bottom); credit: MBARI

Finally, I’d like to point out that there is even more to discover and learn beyond the canyon itself. As the continental slope transitions to the much flatter open ocean floor (greater than 10,000 feet deep) the deep canyon transitions to a subtler feature. The Monterey submarine fan, shown in the map below, is a depositional feature — it’s where all the sediment that cut the canyon (and much more that simply traveled through it) ended up. This is the submarine equivalent of a delta in some ways.


Next time you are standing along the coast in Santa Cruz or Monterey and looking out into the ocean remember that there is an entire landscape on the seafloor as beautiful and complex as what we see on land.

– Image comparing Grand Canyon and Monterey Canyon courtesy of this MBARI publication (link opens a PDF)

– First and last images created in GeoMapApp, a free web-based software for creating topographic/bathymetric maps

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A Submarine Grand Canyon Offshore Central California 16 September,2010Brian Romans

Author

Brian Romans

Brian Romans is the author the popular geoscience blog Clastic Detritus where he writes about topics in the field of sedimentary and marine geology and shares photographs of geologic field work from around the world. He is fascinated by the dynamic processes that shape our planet and the science of reconstructing ancient landscapes preserved in the geologic record. Brian came to the Bay Area in 2003 and completed a Ph.D. in geology at Stanford University in 2008. He lives in Berkeley with his wife, a high school science teacher, and is currently working as a research scientist in the energy industry. Follow him on Twitter.

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