en.wikipedia.org/wiki/Lizard_complexThe Lizard Complex, Cornwall is generally accepted to represent a preserved example of an exposed ophiolite complex in the United Kingdom. The rocks found in The Lizard area are analogous to those found in such famous areas as the Troodos Mountains, Cyprus and the Semail Ophiolite, Oman
www.nature.com/articles/282058a0The Lizard complex of south Cornwall consists of an assemblage of peridotites, gabbros, hornblende schists, metasediments, dolerites and metadolerites and acid-basic banded gneisses (the Kennack ...
www.booking.com/hotel/es/blue-loft-lizard-complex.en-gb.htmlLocated in Playa Blanca, 0.9 miles from Playa Dorada and 0.9 miles from Playa Blanca, Lizard Complex provides pool views and free WiFi. Each unit is equipped with a terrace, a fully equipped kitchen with a fridge, a seating area with a sofa, a TV and a private bathroom with shower.
www.booking.com/hotel/es/blue-loft-lizard-complex.htmlLocated in Playa Blanca, Lizard Complex provides pool views and free WiFi, a 16-minute walk from Playa Dorada and 0.9 miles from Playa Blanca. Featuring a patio or a balcony, all units include a seating area, a TV, an equipped kitchen, a dining area, and a private bathroom.
www.viamichelin.com/web/Hotel/Playa_Blanca-35580-_-4b8e2e94Located in Playa Blanca, 1.4 km from Playa Dorada and 1.5 km from Playa Blanca, Lizard Complex provides pool views and free WiFi. Each unit is equipped with a terrace, a fully equipped kitchen with a fridge, a seating area with a sofa, a TV and a private bathroom with shower.
pubs.geoscienceworld.org/.../Ophiolitic-mylonites-in-the-Lizard-complex-DuctileOphiolitic rocks in the Lizard complex, southwestern England, preserve fine examples of mylonitic schists within low-angle amphibolite-facies shear zones. Two prominent shear zones, with type localities at Carrick Luz and Porthoustock, both have a footwall in the mafic-ultramafic interface at the base of the oceanic crust.
www.researchgate.net/.../30049435_The_emplacement_of_peridotites_and_associat...of the Lizard Complex is interpreted to be a detached thrust sheet derived fr om the rifted margin ﬂoor of the pull-apart basin shown in Figure 9. Series schists and the Landewednack amphibolites
www.tripadvisor.com/Attraction_Review-g528889-d14803573-Reviews-Lizard_Po...This is a private tour with your personal driver guide. Transport is by luxury SUV. Your guide is experienced and local with a background as a police officer and has advanced driving qualifications.
www.geolsoc.org.uk/Policy-and-Media/Outreach/.../The-LizardThe rocks at the Lizard are part of an ophiolite – a piece of oceanic crust that has been uplifted onto continental crust. When the rocks of the Lizard were formed around 400 million years ago, the area was completely submerged by water.
jgs.lyellcollection.org/content/141/1/37Regional prograde pumpellyite actinolite facies metamorphism (Ml) has affected the Gramscatho Group sediments and volcanics structurally underlying the Lizard Complex. Metamorphism took place synchronously with the main penetrative deformation (Dl). There is no evidence of any increase in the regional gradient towards the Lizard Complex or of any local thermal overprinting.