Haskell County Fossils

ROCK Picture Rock

Home
NEW
VERTEBRATE Mastodon Jaw
VERTEBRATE Unidentified Small Bone
VERTEBRATE Tiny Bones in Shale Matrix
VERTEBRATE Equine Tooth (Pottowatamie Co, OK)
VERTEBRATE TRACE Pseudobradypus Keota Tracks
VERTEBRATE TRACE Tetrapod Tracks
VERTEBRATE TRACE Unidentified Specimens
INVERTEBRATE Eurypterid
INVERTEBRATE Unidentified (Possible)
INVERTEBRATE TRACE Unidentified Possible Worms and Burrows
INVERTEBRATE TRACE Ichnofauna
PLANT Fossilized Wood
PLANT Sphenopsida Calamites
PLANT Lycopsida Roots Stigmaria
PLANT Lycopsida Bark Sigillaria
PLANT Unidentified (Possible)
FOSSIL LINKS
MY BACKGROUND
CONTACT
UNIDENTIFIED Possible Mummified
UNIDENTIFIED Possible Mummified Continued
UNIDENTIFIED Various Specimens
ROCK Picture Rock
ROCK With Large Depression

Click here to go to PREVIOUS page...

Click here to go to NEXT page...

dsc0027picturerocksm.jpg Click to Enlarge

HASKELL COUNTY PICTURE ROCK
 
Picture rock is not a fossil, per se, although the sandstone which forms it can be fossiliferous.  This particular picture rock was found in Haskell County, and exhibits a range of beige, tan, and brown colors.  It was sawn into a flat faced slab, and may be used as a building or paving stone. 

stonepicturerock.jpg Click to Enlarge

KANAB WONDERSTONE, Kanab, Utah

This stone is not altered in any way, simply sawn into slabs.  Swirls and color variations are from Iron Oxides: tans and browns from Limonite, and reds from Hematite.  Scroll down the page for more information about this type of sandstone. 

stonecoaster.jpg Click to Enlarge

Drink coasters are sometimes made from "picture rock". 

PICTURE ROCK

 

This specimen above center is a piece of KANAB WONDERSTONE, also called Picture Sandstone or Picture Rock.  It has layers and swirls of reds, pinks, beige and browns, which create a beautiful landscape scene.  The reds and pinks are from Hematite, and the browns and tans are from Limonite and Iron Oxide.  The Sandstone is unaltered and completely natural - it has been sliced and smoothed only.  From near Kanab, Utah, USA

 

**Note: There are natural inclusions, streaks, and splotches of color which is characteristic to Sandstone.* *

 

SANDSTONE

Chemical Composition:  Mainly Quartz, along with Feldspar, Garnet, Magnetite, Tourmaline, Hornblende, Mica, Zircon, etc.  Cementing agents usually silica, carbonates, clay, and/or iron oxides. 

Hardness:   Variable depending on cementing materials.

Crystal Habit: Massive. Granular. 

Color:  Varies widely.  Light colors often from Calcite or Quartz.    Greens from Glauconite - Greensands.    Iron Oxides cause reds and browns:  tans & browns from Limonite, roses and reds from Hematite.

Misc:   Ripples and swirls common.  May be fossiliferous.  Used extensively in blocks as building material, as well as decorative carved portions of buildings.  Glauconitic sandstone, (greensands), used as a source of potash for fertilizer.

 

Click here to go to PREVIOUS page...

Click here to go to NEXT page...

sysadm