Compartir
Hydrogeology of the Mammoth Spring Groundwater Basin and Vicinity, Markagunt Plateau, Garfield, Iron, and Kane Counties, Utah (en Inglés)
Lawrence E. Spangler
(Autor)
·
Createspace Independent Publishing Platform
· Tapa Blanda
Hydrogeology of the Mammoth Spring Groundwater Basin and Vicinity, Markagunt Plateau, Garfield, Iron, and Kane Counties, Utah (en Inglés) - Spangler, Lawrence E.
$ 500.92
$ 910.77
Ahorras: $ 409.85
Elige la lista en la que quieres agregar tu producto o crea una nueva lista
✓ Producto agregado correctamente a la lista de deseos.
Ir a Mis Listas
Origen: Estados Unidos
(Costos de importación incluídos en el precio)
Se enviará desde nuestra bodega entre el
Lunes 05 de Agosto y el
Viernes 16 de Agosto.
Lo recibirás en cualquier lugar de México entre 1 y 3 días hábiles luego del envío.
Reseña del libro "Hydrogeology of the Mammoth Spring Groundwater Basin and Vicinity, Markagunt Plateau, Garfield, Iron, and Kane Counties, Utah (en Inglés)"
The Markagunt Plateau, in southwestern Utah, lies at an altitude of about 9,500 feet, largely within Dixie National For- est. The plateau is capped primarily by Tertiary- and Quater- nary-age volcanic rocks that overlie Paleocene- to Eocene-age limestone of the Claron Formation, which forms escarpments on the west and south sides of the plateau. In the southwestern part of the plateau, an extensive area of sinkholes has formed that resulted primarily from dissolution of the underlying limestone and subsequent subsidence and (or) collapse of the basalt, producing sinkholes as large as 1,000 feet across and 100 feet deep. Karst development in the Claron Formation likely has been enhanced by high infiltration rates through the basalt.