to the National Atlas Home page
About | Fact Sheets | Contact Us | Partners | Products | Site Map | FAQ | Help | Follow us on Twitter 
Part of Project LogoAgricultureBiologyBoundariesClimateEnvironmentGeologyGovernmentHistoryMappingPeopleTransportationWater
to the Interactive Map MakerMap LayersPrintable MapsWall MapsDynamic MapsArticlesMapping Professionals





 
Geology
Map Maker
Geologic Map
Shaded Relief
Map Layer
Generalized Geologic Map of the Conterminous United States
North America Shaded Relief
 

Article

  The North American Tapestry of Time and Terrain

Introduction
The Two maps
Zoom In
Features
Legend and Rock Ages
Rock Types
Political Boundaries
Credits

  Legend and Rock Ages
 

Cenozoic Rocks - 66 million years ago to the present

Map of cenozic era rocks.

 

The Cenozoic era is the most recent era in Earth history. It started about 65 million years ago and continues through the present day. The Cenozoic is divided into smaller segments called epochs which are, from oldest to youngest, the Paleocene, Eocene, Oligocene, Miocene, Pliocene, Pleistocene, and Holocene. These epochs have been combined to create larger periods. Some scientists create two periods in the Cenozoic called the Tertiary and the Quaternary. In this case, the Tertiary is made up of the epochs from the Paleocene through the Pliocene (and is divided into the Paleogene and Neogene), and the Quaternary includes the Pleistocene and Holocene epochs.

Much of what we see in terms of topography today has been formed in the Cenozoic for the simple reason that many older features have been changed or erased from the surface. This is different from rock ages, though. For example, we find truly ancient Precambrian rocks in the Rocky Mountains, but the character of the mountains themselves is relatively young, having developed mostly within the last 60 million years. Many of the features listed on this Web site have a Cenozoic component associated with them, whether it is in terms of rock age (the Coastal Plain, for example), topographic development (the Rockies, again), or activity (the San Andreas Fault and the Cascades).

Features related to the Cenozoic include the following:

Basin and Range
Central Valley
Coteau des Praires
Crater Lake
Crowleys Ridge
Driftless Area
Finger Lakes
Florida
Garlock Fault
Glacial Limit
Llano Estacado
Mississippi River Delta
Mississippi River Embayment
Mount Saint Helens
Northwest Angle
Pre-Pleistocene River System
Recessional Moraines
Rio Grande Rift
Sand Hills
Snake River Plain
Terminal Moraines
Trail Ridge
Trans-Mexico Volcanic Belt
Valles Caldera
Walker Lane
Yellowstone