"Wisdom begins in wonder" – Socrates
Category: Earth/Climate science
VOC Release From Groundwater Rise
06/17/26
“How can groundwater rise release volatile organic compounds into buildings?”
Volatile organic compounds can contaminate groundwater through industrial pollution. When groundwater rises, the volatile organic compounds can vaporize and disperse into air pockets between soil pores. These can eventually migrate into indoor spaces through foundation cracks and building ventilation. This is how VOC Release From Groundwater Rise works.
Why Groundwater Rise Will Flood Pipes
06/16/26
“Why will groundwater rise flood pipes?”
Climate change is causing groundwater to rise in many places. The elevated water table will hit underground infrastructure such as pipes. Groundwater will flood into the pipes through cracks and joints. The extra water in the pipes will reduce their capacity to convey stormwater and wastewater, leading to more infrastructure and public health damage. This is Why Groundwater Rise Will Flood Pipes.
How Pumps Can Lower Water Tables
06/15/26
“How can pumps lower water tables?”
People may need to lower water tables for construction, flood safety, or contamination remediation. One way to accomplish this is to use a pump to suck out the water from the aquifer like a straw. The water table will naturally get smaller when water is removed. This is How Pumps Can Lower Water Tables.
Image credit: https://images.squarespace-cdn.com/
Turbidity Currents
06/14/26
“How can sediment avalanches happen underwater?”
It’s easy to think of sediment in water bodies as unchanging. However, sometimes, sediment can accumulate near a steep slope, and an event can cause this sediment to tumble downhill. The water that becomes mixed with this sediment will end up denser than the surrounding water, and gravity will pull the mixture downhill, resulting in a strong, long-traveling current called a Turbidity Current. Turbidity currents can carve out abyssal channels if done repeatedly enough.
Image credit: https://encrypted-tbn0.gstatic.com/
Continental Slope
06/12/26
“How does the ocean transition from shallow to deep waters?”
The ocean’s continental shelf defines its shallow layers. But when does it transition to deep water? Well, once the continental shelf reaches its border, it will go through a Continental Slope that descends at an average of 4 degrees until it hits the abyssal plain. Continental slope gradients are closest off stable coastlines that lack major rivers and are highest near young mountain ranges with narrow continental shelves.
Image credit: https://www.reddit.com/
The Continental Shelf
06/10/26
“What’s the part of the Earth’s surface that’s just beyond the ocean shoreline?”
It’s easy to think that the Earth’s land ends at the ocean shoreline. But in fact, it extends into The Continental Shelf. The continental shelf is the Earth’s physical surface that’s just beyond the shoreline. This landform is typically submerged below 100 – 200 meters of water. The continental shelf typically ends at a point of increasing slope downwards. Most ocean-based extractionist industries such as offshore drilling take place in the continental shelf.
The Abyssal Plain
06/09/26
“What is the giant underwater plain on the ocean floor?”
The oceans lie above the Earth’s crust. Between 3,000 – 6,000 km below the ocean surface, so deep that sunlight can’t reach it, lies a giant flat part of the ocean floor known as The Abyssal Plain. The abyssal plain’s ultra smooth flatness is forge by from millions of years of particulate settlement depositing over surface irregularities. This flatness makes the abyssal plain suitable for undersea cable routing. Other interesting facts about the abyssal plain include pressures can reach up to 600 times atmospheric pressure and water temperature ranges between a stable 2 – 3 degrees celsius.
Image credit: https://www.thedailyatom.com/
Abyssal Channels
06/08/26
“How are there channels on the sea floor?”
Channels are found in all places in the world. Channels on the sea floor, known as Abyssal Channels, are formed when sediment-dense water rushes down a continental shelf and erodes a path on the sea floor. Sediment can move rapidly through these channels, creating barriers for engineers working to route underwater pipelines and cables through them.
Image credit https://img.magnific.com/
Why Historically Redlined Neighborhoods Are Especially Vulnerable to Pollution From Groundwater Flooding
06/07/26
“Why are historically redlined neighborhoods especially vulnerable to pollution from groundwater flooding?”
Redlining in the US forcibly segregated Black and Brown communities in urban areas into neighborhoods with the lowest amount of public investment. Racist municipal officials often would zone toxic industries in these neighborhoods. These industries would accumulate contaminants underground over their course of operation. Groundwater flooding releases these contaminants from the earth to the surface, harming the communities that live nearby. This is Why Historically Redlined Neighborhoods Are Especially Vulnerable to Pollution From Groundwater Flooding. Examples include West Oakland in California and Southeast Queens in New York.
Image credit: https://savesfbay.org/
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