Millions of Years, tons of pressure and
relentless erosion created a bizarre landscape. Forget the baked, hot
desert you see in the photos below. Instead, rewind 170 million years
to the Jurassic Period and the area shown below would be on SEA FRONT
PROPERTY! During this period, Goblin Valley was a muddy tidal flat along
an inland sea. The waves of the tidal flat deposited sand, silt and clay.
With pressure and time, the sediment became the Goblin-forming Entrada
formation you see today. |
|
Imagine the Jurassic Period
140 to 170 million years ago. This area was on the edge of a shallow inland
sea. Tidal deposits of sand, silt and clay sediments were left here. Over
millions of years, these distinct layers hardened to become the sandstone,
siltstone and shale layers of the Entrada Sandstone formation. The Entrada
can be seen here and in many areas across southern Utah, including Arches
National Park where the sandstone is harder. |
|
While this area was a tidal
flat, the area of Arches National Park was dry and covered in sand dunes.
The resulting rocks determined the effects of wind and water erosion.
The alternating layers of hard sandstone and soft siltstone created Goblins
here, and the hard sandstone left from ancient sand dunes created the
fins and arches in Arches National Park. |
|
None of the goblins have signs or names,
but the two RV Gypsies see a piggy goblin here. Do YOU?
Below: Lee Duquette rode a camel |
|
|
A row of goblins below
the Henry Mountains |
This goblin has small eyes and a big mouth |
|
|
|
Below: Lee Duquette saw a frog in the distance - so the
two RV Gypsies just had to take a closer look at the frog. |
|
|
Below; A mountain in the far distance is framed
between two goblins. |
Below; What does Lee Duquette
think he is going to find in there? |
|
|
|
Below: Looking into the distance, the two RV Gypsies
saw a patch of white, so they walked until they actually got to that patch
of white and they were amazed at how different it looked close up. |
|
|
Below: A rock falling onto Lee's head - LOL |
Below: A cow (steer) |
|
|
Below: A pumpkin and a monkey face |
Below: A saddle |
|
|
|
Below; Karen Duquette with a really
cute goblin |
Below: The two RV Gypsies with more
goblins |
|
|
|
|
Below: The goblin below got hit in the head
by a pair of shoes. |
Below: Two dragons and a castle |
|
|
Below: Three goblins |
Below: An ugly goblin with a big chin, big teeth,
and eyes on top of his head |
|
|
Below: Lee Duquette really enjoyed himself here. |
Below: BUTT CHEEKS |
|
|
Below: A few odd red stones - where did
they come from? |
|
|
Below: A raven making a lot of noise |
|
Below: Karen Duquette having fun with the
goblins |
|
|
|
|
|
|
|
|
|
|
The Valley of the Goblins is continually eroding. Even though very little
change will be seen in our lifetime, old goblins will fall, allowing for
a new generation of goblins to be created. Although erosion is a natural
process, it can be accelerated by human impact. After leaving Goblin Valley,
the two RV Gypsies heard on the news that a Boy Scout Leader and his troop
where here at Goblin Valley destroying the formations. How Terrible! There
were signs saying it is OK to touch and climb on these formations (which
is unusual in parks), but that does NOT mean to destroy them. |