Location: Niwot Ridge
For the next few weeks, I am able to have the opportunity to stay in the outskirts of Nederland, Colorado for a 3-week class on lake and stream ecology. How fitting it would be, I thought, to connect experiences from this class to oceanic issues.
Within the first few hours of class we are welcomed by our professor, and continue into lecture for the first hour. Next stop: Niwot Ridge, elevation 3520 meters. An approximate 10 minute off-roading adventure, followed by a 25-30 minute steep, rocky hike, and we have arrived! While eating lunch and admiring the tree-less slopes of the mountains, we discuss groundwater and precipitation. Groundwater moves approximately a foot per day, but can move faster in more geological areas- such as high alpine environments. As it moves downhill toward the lake and stream systems, the water collects nutrients and minerals that it runs over. Therefore, by the time the groundwater gets to the oceanic waterways, it could have collected thousands of feet worth of particles, whether it is nutrients or pollutants. Even these high alpine areas have pollutants, through precipitation. For example, sodium chloride would not be abundant in mountain regions, although there are trace amounts of it found. Why would sodium chloride be present here? Well, precipitation in these areas comes from evaporation from the ocean, hence oceanic nutrients are cycled to the mountains, and vice versa. This enhances the importance of maintaining healthy oceanic and alpine ecosystems! Another nutrient that was found to be in these high elevations was ammonia. This was due to food plots, in which food for a desired animal is plotted on land in order for it to be easier to hunt. It is the same concept as planting crops in association with fertilizer runoff. There are many issues with runoff, mostly concluding that it will lead to eutrophication.
Location: Left Hand Reservoir