GeoLog

Regular Features

Imaggeo On Monday: Carbon-sink

Imaggeo On Monday: Carbon-sink

Biochar is a carbon rich product of biomass pyrolysis, a process where biological material is exposed to high temperatures, in the absence of oxygen, to cause the decomposition of that material into various chemical and physical components. By going through this process, biochar can be a valuable soil additive and a carbon sink with a …[Read More]

Imaggeo On Monday: Sunset in the Arabian basin

Imaggeo On Monday: Sunset in the Arabian basin

We know the topography of the moon better than the Earth’s seafloor, so we need to keep studying the ocean, and, for me, going to sea is the best way.   Only twenty percent of the seafloor is already mapped (see the Seabed 2030 Project), leaving eighty percent of our ocean unmapped, unobserved, and unexplored. …[Read More]

Imaggeo On Monday: Watercolors- Nature’s talent

Imaggeo On Monday: Watercolors- Nature’s talent

The photo was taken from the International Space Station (ISS), approx. 400 km above the Earth, in the educational project administered by NASA: Sally Ride EarthKAM, Mission 59, November 2017. The image was requested by a team of students from my college, coordinated by me. Even though we weren’t there, on ISS, to trigger the …[Read More]

Imaggeo On Monday: Geoscientific selfie at the Dead Sea

Imaggeo On Monday: Geoscientific selfie at the Dead Sea

This is an aerial image taken from a balloon at around 150m height, at the eastern shoreline of the Dead Sea. Such “selfies” are scientifically valuable, providing important data that help researchers to analyze the morphology of the retreating lake and investigate associated hazards like sinkholes, subsidence and landslides. The older shorelines, visible as lines …[Read More]

Imaggeo On Monday: Patterns in the landform

Imaggeo On Monday: Patterns in the landform

The badlands at the Zabriskie Point (Death Valley, California, USA) rest upon a mudstone foundation. In the prehistoric lakes of Death Valley, fine grained sediments were deposited to form soft rocks. The clay minerals in the mudstone are shaped like tiny plates, which helps create the layers. The combination of the almost impermeable mudstone and …[Read More]