
The Causey Pike Fault or Causey Pike Thrust is a major WSW-ENE trending
fault within the
Lower Paleozoic
Lower may refer to:
* Lower (surname)
* Lower Township, New Jersey
*Lower Receiver (firearms)
* Lower Wick Gloucestershire, England
See also
*Nizhny
Nizhny (russian: Ни́жний; masculine), Nizhnyaya (; feminine), or Nizhneye (russian: Ни ...
rocks of the English
Lake District. It is named for
Causey Pike
Causey Pike is a fell in the English Lake District. It is situated in the Newlands Valley, 5 km south-west of the town of Keswick. Even though it has a modest height of 637 metres (2,090 ft) it is one of the most distinctive ...
, where the fault was first recognised.
Extent
The Causey Pike Fault has been recognised across the entire outcrop of the Lake District
inlier
An inlier is an area of older rocks surrounded by younger rocks. Inliers are typically formed by the erosion of overlying younger rocks to reveal a limited exposure of the older underlying rocks. Faulting or folding may also contribute to the obs ...
, extending about 35 km from near
Ennerdale Bridge
Ennerdale Bridge is a hamlet in the county of Cumbria, England. It is in the civil parish of Ennerdale and Kinniside. It had a total population taken at the 2011 census of 220.
Description
Ennerdale Bridge lies at the confluence of Croasdale ...
in the west, to near
Troutbeck in the east. A possible continuation of the fault to the east has been recognised in the
Cross Fell
Cross Fell is the highest mountain in the Pennines of Northern England and the highest point in England outside the Lake District. It is located in the North Pennines Area of Outstanding Natural Beauty. It lies within the county of Cumbria and ...
inlier, where it also juxtaposes two differing parts of the
Skiddaw Group
''For the Skiddaw group of hills, see Skiddaw Group''
The Skiddaw Group is a group of sedimentary rock formations named after the mountain Skiddaw in the English Lake District. The rocks are almost wholly Ordovician in age ( Tremadoc through ...
.
Recognition
It juxtaposes two successions dominated by
mudrock
Mudrocks are a class of fine-grained siliciclastic sedimentary rocks. The varying types of mudrocks include siltstone, claystone, mudstone, slate, and shale. Most of the particles of which the stone is composed are less than and are too sma ...
s that are of similar age.
To the north of the fault, the
Ordovician
The Ordovician ( ) is a geologic period and system, the second of six periods of the Paleozoic Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start of the Silurian Period Mya. ...
Skiddaw Group is represented by the Kirk Stile Formation, to the south by the Buttermere Formation, both of
Arenig
In geology, the Arenig (or Arenigian) is a time interval during the Ordovician period and also the suite of rocks which were deposited during this interval.
History
The term was first used by Adam Sedgwick in 1847 with reference to the "Areni ...
age. The younger sequence of volcanic rocks overlying the Skiddaw Group also differs, with the
Eycott Volcanic Group to the north and the
Borrowdale Volcanic Group
The Borrowdale Volcanic Group is a group of igneous rock formations named after the Borrowdale area of the Lake District, in England. They are Caradocian (late Ordovician) in age (roughly 450 million years old). It is thought that they represent ...
to the south. The fault is described as a
thrust
Thrust is a reaction force
In physics, a force is an influence that can change the motion of an object. A force can cause an object with mass to change its velocity (e.g. moving from a state of rest), i.e., to accelerate. Force can al ...
near Causey Pike, where
metasomatised rocks of the
Crummock Water
Crummock Water is a lake in the Lake District in Cumbria, North West England situated between Buttermere to the south and Loweswater to the north. Crummock Water is long, wide and deep. The River Cocker is considered to start at the north of ...
Aureole
An aureola or aureole (diminutive of Latin ''aurea'', "golden") is the radiance of luminous cloud which, in paintings of sacred personages, surrounds the whole figure.
In Romance languages, the noun Aureola is usually more related to the d ...
are emplaced over
sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks.
Most sandstone is composed of quartz or feldspar (both silicates ...
olistoliths of the Buttermere Formation, but the overall displacement on this structure is oblique, with a significant component of sinistral (left lateral)
strike-slip
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tecton ...
motion.
Age of movement
The differences in stratigraphy and interpreted
depositional environment
In geology, depositional environment or sedimentary environment describes the combination of physical, chemical, and biological processes associated with the deposition of a particular type of sediment and, therefore, the rock types that will b ...
across the fault may indicate that the fault was originally a normal fault, active during deposition of the Skiddaw Group. The oblique slip movement on the fault occurred during the
Acadian Orogeny, at least in part postdating the
contact metamorphism
Metamorphism is the transformation of existing rock (the protolith) to rock with a different mineral composition or texture. Metamorphism takes place at temperatures in excess of , and often also at elevated pressure or in the presence of chem ...
that caused the development of the Crummock Water Aureole (dated to about 401 Ma -
Emsian
The Emsian is one of three faunal stages in the Early Devonian Epoch. It lasted from 407.6 ± 2.6 million years ago to 393.3 ± 1.2 million years ago. It was preceded by the Pragian Stage and followed by the Eifelian Stage. It is named after ...
), which itself postdates the formation of the regional
cleavage
Cleavage may refer to:
Science
* Cleavage (crystal), in mineralogy and materials science, a process of splitting a crystal
* Cleavage (geology), the foliation perpendicular to stress as a result of ductile deformation
* Cleavage (embryo), in emb ...
seen within the Skiddaw Group.
References
{{Reflist
Geology of Cumbria