Images

Figure 1. Location of the nine River Input Monitoring (RIM) stations in the Chesapeake Bay watershed.

This is a field photo of geologists from the Indiana Geological and Water Survey and Ohio Geological Survey conducting core drilling of glacial sediments. The information gained from this project aided in the development of a bedrock topography map of a buried ancient river bed. 

This is a 20 foot section of a drill core collected by the Indiana Geological and Water Survey (IGWS). IGWS geologists dub these cores "golden spikes" when they are drilled deep enough to reach the underlying bedrock.

TNMCorps Mapping Challenge: Cemeteries in Western TN with a FINISHED stamp

The Betsiboka River in Northern Madagascar is seen in this Landsat 9 natural color image from December 7, 2021. Extensive logging has left the land vulnerable, and iron rich soils are washed into the river, coloring it a reddish orange as it flows to the Betsiboka estuary delta.

Product ID LC09_L1TP_160071_20211207_20220120_02_T1

NASA and the USGS briefed the Landsat Science Team about Landsat 9 at their Fall Meeting held virtually on November 24, 2021.

 

Read the details here: https://www.usgs.gov/landsat-missions/news/landsat-science-team-virtual…

Deforestation can happen naturally, through infestation of native beetles and extreme weather. However, people can intentionally clear forests for timber and other industries. Difference between the two can be difficult to diagnose.

On Tuesday December 7, 2021, updates were made to all USGS webpages, including the Landsat Missions Web Site (LMWS). 

Learn more here: https://www.usgs.gov/landsat-missions/news/landsat-mission-web-site-cha…

On November 23, 2021, the Landsat Archive added its ten millionth image. The Landsat 7 scene was acquired over the Dead Sea and is shown as a false color image using the short-wave infrared, near infrared and red bands (bands 5,4,3).

These images of an area in south central Queensland, Australia were acquired by the instruments onboard both Landsat 8 and Landsat 9 on November 15, 2021, as Landsat 9 flew beneath Landsat 8 as the satellite continued its climb to nominal orbital altitude.

This graphic displays a few of the common band Red-Green-Blue (RGB) combinations of Landsat data. For more information about using Landsat bands in your research, visit the following pages: 

Thick vegetation at a Guymon, Oklahoma, site required parking a quarter-mile away. The pickup is visible at the top center of the photo, which was taken on November 11, 2021, the first characterization day there. (Photo by Jeff Irwin, USGS)

Landsat image of Window Rock, Arizona, acquired on November 3, 2021.

For more information about Landsat, please visit www.usgs.gov/Landsat

To download the data, visit earthexplorer.usgs.gov

Landsat 5 images of Zhuozhou, China, on September 7, 1999, showing top-of-atmosphere (TOA) reflectance; Level-2 surface reflectance (SR); and Level-2 surface temperature (ST), in Kelvin (K). View fact sheet at Landsat Collection 2 Level-2 Science Products (usgs.gov).

Sediments swirl in Lake Erie and Lake St. Clair in this Landsat 9 image of both Detroit, Michigan, and Windsor, Ontario, from Oct. 31, 2021. The Great Lakes serve as sources of freshwater, recreational activity, transport, and habitat for the upper-midwestern US, and water quality remains a high priority. 

The city of Kathmandu, Nepal, seen at the bottom left of this Landsat 9 image, lies in a valley south of the Himalayan Mountainsbetween Nepal and China. Glaciers, and the lakes formed by glacial meltwater, are visible in the top middle of this image.

In the Western U.S., in places like the Navajo Nation as seen in this Landsat 9 image, Landsat and other satellite data help people monitor drought conditions and manage irrigation water. With only 85 rain gauges to cover more than 27,000 square miles, satellite data and climate models are filling the gaps to help the Navajo Nation monitor drought severity.

Image showing a section of Lava River Cave, located in Northern Arizona. 

This map details the subsurface contact between the consolidated Paleozoic bedrock surface and the overlying unconsolidated Quaternary-aged sediments. This image is used with the permission of the Ohio Department of Natural Resources, Division of Geological Survey and the Indiana Geological and Water Survey.