 | An iceberg like this caused the sinking of the Titanic. |
 | CSS Hudson |
 | Cores being transported on the CSS Hudson. |
 | Micrograph detailing the sand-size fraction in core HU87033-009. |
 | Micrograph detailing the sand-size fraction from the same core at 670-672 cm depth, within H-2. |
 | X-ray of lithic-rich sediments. |
 | H-6 at ca. 60,000 years ago is currently the oldest commonly accepted Heinrich event. |
 | Winch lowering a piston core into the water. |
 | "Deep-tow fish" being lowered over the end of the ship. |
 | Scientists examining a seismic profile. |
 | 10m piston core being raised to the deck of the Hudson. |
 | The working-half of a 7 cm diameter core being sampled on the CSS Hudson. |
 | Core 87033-009 X-radiograph |
 | East Greenland |
 | East Greenland |
 | Figure showing the processes by which ice rafted detritus are deposited and transported. |
 | Color of the sediment at core site HU87033-009. |
 | Core 9 |
 | Hudson Bay and Hudson Strait |
 | Data from several sediment cores from Dowdeswell et al. [1995]. |
 | Core ODP-609, Data from Cortijo et al. [1997]. |
 | Variability in sediment properties within Heinrich and non-Heinrich sediments from same core. |
 | Correlations with Heinrich Events. Data from Grimm et al. [1993]. |
 | Areas/sites where possible teleconnection events have been described; update of Broecker [1994]. |
 | Heinrich events and other mysteries of the earth's climate system. |
