>
Pentagon To Send 200 Troops to Nigeria
Trump Says He May Send Second Aircraft Carrier to Middle East To Prepare for Potential Attack...
A Market Crash and Recession Are Bullish, Not Bearish
What Are They Still Hiding? New Epstein Questions Point to a Much Bigger Cover-Up
Drone-launching underwater drone hitches a ride on ship and sub hulls
Humanoid Robots Get "Brains" As Dual-Use Fears Mount
SpaceX Authorized to Increase High Speed Internet Download Speeds 5X Through 2026
Space AI is the Key to the Technological Singularity
Velocitor X-1 eVTOL could be beating the traffic in just a year
Starlink smasher? China claims world's best high-powered microwave weapon
Wood scraps turn 'useless' desert sand into concrete
Let's Do a Detailed Review of Zorin -- Is This Good for Ex-Windows Users?
The World's First Sodium-Ion Battery EV Is A Winter Range Monster
China's CATL 5C Battery Breakthrough will Make Most Combustion Engine Vehicles OBSOLETE

Above – A cross-section of underground ice is exposed at the steep slope that appears bright blue in this enhanced-color view from the HiRISE camera on NASA's Mars Reconnaissance Orbiter. The scene is about 550 yards wide. The scarp drops about 140 yards from the level ground in the upper third of the image. Image Credit: NASA/JPL-Caltech/UA/USGS
These eight scarps, with slopes as steep as 55 degrees, reveal new information about the internal layered structure of previously detected underground ice sheets in Mars' middle latitudes.
The ice was likely deposited as snow long ago. The deposits are exposed in cross section as relatively pure water ice, capped by a layer one to two yards (or meters) thick of ice-cemented rock and dust. They hold clues about Mars' climate history. They also may make frozen water more accessible than previously thought to future robotic or human exploration missions.