jump Index ScientificPsychic.com
Scientific Psychic Expand your mind

Circular Carolina Bays

The Delmarva Peninsula on the East Coast of the United States is divided between Maryland, Delaware and Virginia. The northern part of the peninsula has many small Carolina Bays, but larger bays are also encountered. The bays in Delmarva tend to be more circular than elliptical, and the pattern of the bays looks like a shotgun blast.

The Delmarva Peninsula
The Delmarva Peninsula

Circular Carolina Bays in northern Delmarva
Circular Carolina Bays in northern Delmarva near Barclay, MD

The southern part of the Delmarva peninsula belongs to Virginia. The Carolina Bays along this narrow strip of land are circular. This image near Mappsville, Virginia shows large bays with diameters of approximately 1.3 kilometers. Delmarva does not have deep sandy soil because thirty-five million years ago, a meteorite struck the Chesapeake Bay and created a tsunami that washed away the loose surface sand of the Delmarva peninsula. The shallow depth of unconsolidated material in Delmarva made it impossible to create inclined conical cavities, and this resulted in circular bays.

Circular Bays in the Virginia part of Delmarva
Circular Bays in Delmarva near Mappsville, VA

The following photographs show an experiment to test the impact of an ice projectile on shallow depth of viscous material. The target consisted of equal parts of sand and pottery clay with enough water to have the consistency of bricklayer's mortar. The depth of the material was controlled by burying a pie tin with the viscous mixture.

An oblique impact on a target that constrains the depth of the medium results in a circular structure. When the depth of the medium is not constrained, and impact creates an inclined conical cavity that becomes an elliptical bay by viscous relaxation.


(Click on the images to enlarge them)




Pie tin is filled
with sand/clay mixture





Green sand enhances
visualization


Penetration is constrained
by depth of pie tin


A circular crater is formed





Oblique impact is
stopped by barrier


Start of viscous relaxation


Crater wall collapses
as ice melts


Circular structure
after viscous relaxation



Without depth constraint
an ellipse is formed





© Copyright  - Antonio Zamora