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İngilizce - Türkçe

laccolith anlamı
lakolit

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A laccolith is a sheet intrusion (or concordant pluton ) that has been injected between two layers of sedimentary rock . the laccolith a
Kaynak: Laccolith

Beshtau (Бештау, from Turkic besh 'five' and tau 'mountain') is an isolated five-domed igneous mountain (laccolith ) near Pyatigorsk
Kaynak: Beshtau

Plutons include batholith s, stocks , dikes , sills , laccolith s, lopolith s, and other igneous bodies. In practice, "pluton" usually
Kaynak: Pluton

The Shonkin Sag lends its name to the Shonkin Sag laccolith , a famous laccolith 200 | ft thick and 1 | mi wide near the western mouth of
Kaynak: Shonkin Sag

The geology of these mountains was first studied in 1875-1876 by Grove Karl Gilbert He coined the term "laccolite" (now laccolith ) to
Kaynak: Henry Mountains

Some of these intrusions form laccolith s emplaced at depths of a few kilometers. The predominant igneous rock is porphyritic hornblende
Kaynak: Abajo Mountains

The Pine Valley Mountains form the Pine Valley Laccolith, one of the largest laccolith s in the United States. Elevations in the
Kaynak: Pine Valley Mountain Wilderness

It is situated within the Gunnison National Forest and is of a geologic formation called a laccolith Laccolith formations are caused by
Kaynak: Tomichi Dome

intrusion or laccolith in the Black Hills near Hulett and Sundance in Crook County , northeastern Wyoming , above the Belle Fourche River .
Kaynak: Devils Tower

Typical intrusive formations are batholith s, stocks, laccolith s, sill s and dikes . The central cores of major mountain ranges consist of
Kaynak: Igneous rock

Many of the dikes clearly fed laccoliths in the area. Two concentric rings of laccolith s lie in the northwest section of the field 11 miles
Kaynak: Adel Mountains Volcanic Field

They are among the most extensive igneous features on Earth,date March 2013 in the form as dikes , dike swarm s, laccolith s, and sills .
Kaynak: Sheet intrusion

Viewed from above it suggests an impact crater , though it is actually the eroded remains of a laccolith . The approximate center of the
Kaynak: Solitario

The Pine Valley Mountains formed from the Pine Valle Laccolith, which is the largest laccolith in the United States and perhaps the
Kaynak: Pine Valley Mountains

uncommon, small volume ultrapotassic igneous rocks primarily occurring as dikes , lopolith s, laccolith s, stocks and small intrusion s.
Kaynak: Lamprophyre

The Shonkin Sag laccolith is a significant source of shonkinite. The Adel Mountains Volcanic Field in north-central Montana is a
Kaynak: Shonkinite

The mountain is laccolith . Today its territory is a Nature reserve (5.5 km 2). There is a pioneer children's camp Artek near Ayu-Dag
Kaynak: Ayu-Dag

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