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Photograph of the Great Dismal Swamp in Virginia
The Great Dismal Swamp
The Great Dismal Swamp
The Great Dismal Swamp

Photograph of the Great Dismal Swamp in Virginia.

Photograph of the Great Dismal Swamp in Virginia
The Great Dismal Swamp
The Great Dismal Swamp
The Great Dismal Swamp

Photograph of the Great Dismal Swamp in Virginia.

Photograph of the Great Dismal Swamp in Virginia
The Great Dismal Swamp
The Great Dismal Swamp
The Great Dismal Swamp

Photograph of the Great Dismal Swamp in Virginia.

A solitary tree trunk stands amongst the devastation of the 2011 fire in Great Dismal Swamp, VA.
Great Dismal Swamp, 2018
Great Dismal Swamp, 2018
Great Dismal Swamp, 2018

Photograph of the Great Dismal Swamp in Virginia several years after the 2011 fire. USGS scientists recently collected peat and lake core samples from the swamp to help reconstruct natural environmental conditions over the past 12,000 years.

Photograph of the Great Dismal Swamp in Virginia several years after the 2011 fire. USGS scientists recently collected peat and lake core samples from the swamp to help reconstruct natural environmental conditions over the past 12,000 years.

A USGS researcher sits in the sand conducting fieldwork on Buttonwood Key, FL
Fieldwork on Florida Bay Islands
Fieldwork on Florida Bay Islands
Fieldwork on Florida Bay Islands

A USGS researcher conducts fieldwork on Buttonwood Key, an island in Florida Bay, to determine the impacts of Hurricane Irma. The storm left thick deposits of mud on the island, which are being measured, sampled and photographed.  Many of the islands in Florida Bay have open mudflats in the center, surrounded by mangroves on the perimeter. 

A USGS researcher conducts fieldwork on Buttonwood Key, an island in Florida Bay, to determine the impacts of Hurricane Irma. The storm left thick deposits of mud on the island, which are being measured, sampled and photographed.  Many of the islands in Florida Bay have open mudflats in the center, surrounded by mangroves on the perimeter. 

Image showing mangroves that have lost all their leaves and a berm that is significantly thinner following Hurricane Irma. 
Berm at Jim Foot Key, Florida (2018)
Berm at Jim Foot Key, Florida (2018)
Berm at Jim Foot Key, Florida (2018)

In Photo: The red circle indicates the same position as shown in the April 2014 photo.  The mangroves have lost all their leaves and the berm is significantly thinner following the storm. 

In Photo: The red circle indicates the same position as shown in the April 2014 photo.  The mangroves have lost all their leaves and the berm is significantly thinner following the storm. 

A boat sits along a dock on Paradox Lake. The autumn colored trees are reflected in the placid lake.
Autumn colors reflected on Paradox Lake in the Adirondack Mountains
Autumn colors reflected on Paradox Lake in the Adirondack Mountains
Autumn colors reflected on Paradox Lake in the Adirondack Mountains

The Northeast Bedrock Mapping Project consists of scientists conducting geologic mapping and scientific research of complexly deformed crystalline igneous and metamorphic rocks in the Northeastern United States. Current mapping activities are focused in New Hampshire, Vermont, Connecticut, and New York.

The Northeast Bedrock Mapping Project consists of scientists conducting geologic mapping and scientific research of complexly deformed crystalline igneous and metamorphic rocks in the Northeastern United States. Current mapping activities are focused in New Hampshire, Vermont, Connecticut, and New York.

USGS scientist Jessica Rodysill studies a sediment core to help understand past environmental conditions. This core was collected from Maryland.
Sediment Core in Maryland
Sediment Core in Maryland
Sediment Core in Maryland

USGS scientist Jessica Rodysill studies a sediment core to help understand past environmental conditions. This core was collected from Maryland. Credit: Elizabeth Goldbaum, USGS. 

USGS scientist Jessica Rodysill studies a sediment core to help understand past environmental conditions. This core was collected from Maryland. Credit: Elizabeth Goldbaum, USGS. 

A field of peatland surrounded by spruce and other understory plants in Alaska. Mountains can be seen in the background.
Thawing Peatlands, Alaska
Thawing Peatlands, Alaska
Thawing Peatlands, Alaska

Cores were collected from various areas of thawing permafrost-peatlands in Alaska. Permafrost thaw results in ground subsidence and inundation that kills black spruce and other understory plants living on the permafrost plateau. 

Cores were collected from various areas of thawing permafrost-peatlands in Alaska. Permafrost thaw results in ground subsidence and inundation that kills black spruce and other understory plants living on the permafrost plateau. 

A technician sits at a computer while running a sediment core through the Geotek.
FBGC Lab - Core Scanning
FBGC Lab - Core Scanning
FBGC Lab - Core Scanning

A technician sits at a computer while running a sediment core through the Geotek.

A technician sits at a computer while running a sediment core through the Geotek.

A team of scientists prepares to board their core collecting platform
Nomini Bay, VA
Nomini Bay, VA
Nomini Bay, VA

A team of scientists prepare to collect cores from the Nomini Bay, VA.

A team of scientists prepare to collect cores from the Nomini Bay, VA.

A lab technician swirls samples in a watch glass to assist in extracting pollen
Pollen Lab, FBGC
Pollen Lab, FBGC
Pollen Lab, FBGC

Tom Sheehan, a lab technician at the Florence Bascom Geoscience Center, swirls a sample in a watch glass to assist in separating pollen from heavier mineral material.

Tom Sheehan, a lab technician at the Florence Bascom Geoscience Center, swirls a sample in a watch glass to assist in separating pollen from heavier mineral material.

Picture of the burned area within the Great Dismal Swamp
Great Dismal Swamp Burn Area, March 2017
Great Dismal Swamp Burn Area, March 2017
Great Dismal Swamp Burn Area, March 2017

USGS scientists recently collected peat and lake core samples from the swamp to help reconstruct natural, environmental conditions over the past 12,000 years. 

USGS scientists recently collected peat and lake core samples from the swamp to help reconstruct natural, environmental conditions over the past 12,000 years. 

Living up to it's name, this picture shows the interior of the Great Dismal Swamp
Great Dismal Swamp, March 2017
Great Dismal Swamp, March 2017
Great Dismal Swamp, March 2017

Centuries of ditching, draining and harvesting resources have greatly altered the Great Dismal Swamp in Virginia.

Centuries of ditching, draining and harvesting resources have greatly altered the Great Dismal Swamp in Virginia.

USGS scientists inspect a sediment core from Bearsden Pond near the Fredericks Hall fault
Sediment Core from Bearsden Pond
Sediment Core from Bearsden Pond
Sediment Core from Bearsden Pond

USGS Research Geologist Jessica Rodysill and USGS-NAGT Student Intern Kristen Steele inspect a sediment core from Bearsden Pond near the Fredericks Hall fault, one of three subsidiary faults that broke in response to slip along the main Quail fault on 23 August 2011 during the M5.8 earthquake.  This research is a collaborative project between the USGS Land Use

USGS Research Geologist Jessica Rodysill and USGS-NAGT Student Intern Kristen Steele inspect a sediment core from Bearsden Pond near the Fredericks Hall fault, one of three subsidiary faults that broke in response to slip along the main Quail fault on 23 August 2011 during the M5.8 earthquake.  This research is a collaborative project between the USGS Land Use

Close-up photo pf botryoidal growth of manganese oxide minerals cryptomelane/hollandite
Botryoidal growth from a breccia, BARD Lab
Botryoidal growth from a breccia, BARD Lab
Botryoidal growth from a breccia, BARD Lab

Botryoidal growth of manganese oxide minerals cryptomelane/hollandite from a breccia in Virginia. Grey banding reflects variation in the Ba (bright) and K (dark) in the botryoidal mass. NCGMP: Appalachian Basin Project.

Botryoidal growth of manganese oxide minerals cryptomelane/hollandite from a breccia in Virginia. Grey banding reflects variation in the Ba (bright) and K (dark) in the botryoidal mass. NCGMP: Appalachian Basin Project.

Corals collected from the base of the Canetrap Formation. The corals are growing on disarticulated oyster and scallop shells.
ICW Section Outcrops, S.C., Summer 2016
ICW Section Outcrops, S.C., Summer 2016
ICW Section Outcrops, S.C., Summer 2016

In July of 2016, a team from the Climate and Land Use Research and Development Program took a trip to South Carolina to study outcrops of the “Canepatch” and “Socastee” formations along the Intra-Coastal Waterway, near Myrtle Beach. The age of these fossiliferous marine units has been controversial for several decades.

In July of 2016, a team from the Climate and Land Use Research and Development Program took a trip to South Carolina to study outcrops of the “Canepatch” and “Socastee” formations along the Intra-Coastal Waterway, near Myrtle Beach. The age of these fossiliferous marine units has been controversial for several decades.

A nearshore shell hash deposit from the Socastee Formation.
ICW Section Outcrops, S.C., Summer 2016
ICW Section Outcrops, S.C., Summer 2016
ICW Section Outcrops, S.C., Summer 2016

In July of 2016, a team from the Climate and Land Use Research and Development Program took a trip to South Carolina to study outcrops of the “Canepatch” and “Socastee” formations along the Intra-Coastal Waterway, near Myrtle Beach. The age of these fossiliferous marine units has been controversial for several decades.

In July of 2016, a team from the Climate and Land Use Research and Development Program took a trip to South Carolina to study outcrops of the “Canepatch” and “Socastee” formations along the Intra-Coastal Waterway, near Myrtle Beach. The age of these fossiliferous marine units has been controversial for several decades.

A unit at the base of the Canepatch Formation with many shells encased in dense estuarine clay.
ICW Section Outcrops, S.C., Summer 2016
ICW Section Outcrops, S.C., Summer 2016
ICW Section Outcrops, S.C., Summer 2016

In July of 2016, a team from the Climate and Land Use Research and Development Program took a trip to South Carolina to study outcrops of the “Canepatch” and “Socastee” formations along the Intra-Coastal Waterway, near Myrtle Beach. The age of these fossiliferous marine units has been controversial for several decades.

In July of 2016, a team from the Climate and Land Use Research and Development Program took a trip to South Carolina to study outcrops of the “Canepatch” and “Socastee” formations along the Intra-Coastal Waterway, near Myrtle Beach. The age of these fossiliferous marine units has been controversial for several decades.

Scientists sit on ground with eocene hyperthermal core samples
Eocene Hyperthermals - Core Samples
Eocene Hyperthermals - Core Samples
Eocene Hyperthermals - Core Samples

Scientists sit on the ground with core samples

A Russian corer set lays laid out on the floor
Pollen Lab Field Gear
Pollen Lab Field Gear
Pollen Lab Field Gear

This gear, known as a Russian corer, is commonly used to extract sediment cores from field sites. 

This gear, known as a Russian corer, is commonly used to extract sediment cores from field sites.