Very dark brown to fl hornblendes that contain titanium ordinarily are called basaltichornblende from the fact that they are usually a constituent of basalt and related rocks.
The pleochroism is always strong, and the angle of optical extinction on the plane of symmetry (x in the figure) varies from o° to 37°.
The dark.-coloured porphyritic crystals of basalts are known as basaltichornblende.
Hornblende occurs as an essential constituent of many kinds 1 Buffon, as was his manner, enlarges on the cruel injustice done to these birds by Nature in encumbering them with this deformity, which he declares must hinder.them from getting their food with ease.
www.1911encyclopedia.org /Hornblende (297 words)
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Hornblende's strong pleochroism and inclined extinction are its most distinctive characteristics.
Hornblende is common in many intrusive igneous rocks ranging from granite to gabbro; it is also present in medium grade metamorphosed mafic rocks.
Hornblende occurs in some volcanic rocks, but it is less abundant in extrusive rocks than in intrusive rocks.
(Hornblende) The mineralhornblende is a complex silicate which is an isomorphous mixture of three molecules; a calcium-iron-magnesium silicate, an aluminium-iron-magnesium silicate, and an iron-magnesium silicate.
Hornblende has a hardness of 5 - 6, a specific gravity of 2.9 - 3.4, and is colored green, greenish-brown, opaque, brown and fl.
V-1): hornblendegabbro and diorite distributed near Kawaura, Jinza-san, Ochiai, and the upper reaches of the Magi River; biotite-hornblende tonalite chiefly in the southern part of the batholith; biotite-hornblende granodiorlte and hornblende-biotite granodiorite in the main.
Hornblende occurs as a discrete crystal of up to 4 mm in length or as an aggregate of fibrous crystals accompanied by fibrous cummingtonite.
The mode of biotite is generally higher than that of hornblende in the northern part of the batholith, whereas that of hornblende is higher than that of biotite in the southern part.
The hornblende in these dark-colored secretions is partially idiomorphic and partially allotriomorphic, with the latter tendency decidedly the stronger; that is, crystal forms may be developed on part of a crystal while the rest has a very irregular outline.
The hornblende of these secretions does not contain inclusions of glass, but it is very apt to contain inclusions of the other phenocrysts so as sometimes to be filled with them, somewhat after the manner of inclusions in the hornblende of the crystalline schists.
This is more especially true of hornblende, which, with possibly one minor exception, is absolutely foreign to the andesites as well as to the basalts of Crater Lake, but which occurs with the same colors and other properties, although very sparingly, in nearly all the thin sections of dacites studied.
Hornblende is made up of 8 different elements which 7 are of the Earth's top 8 in abundance.
Hornblende is an Amphibole, which is a double chained inosilicate that has a silicon oxygen ratio of 4:11.
They say, "The composition of hornblende and the coexisting phases defines the thermal history of the erupting magma." For as diverse in compositional options as hornblende is, you can figure out what type of environment hornblende formed under by its composition.
Hornblende is scarce or absent in rocks that have undergone potassic alteration.
The hornblendes are edenite in composition (Figure 32A) whereas the actinolites are actinolite or actinolite hornblende (Figure 32B).
Hornblende was found in one drill core sample each of feldspar porphyry and phanerite from the Sydney Intrusion north of Folomian (DDH-331) and in several specimens from the Kalgoorlie and Ningi intrusion.
This unit, which is principally made up of biotite and hornblendegneisses, forms the bedrock in the southeast quarter of the area and from there northwestward is present as isolated remnants surrounded by batholithic rocks.
Most of the hornblende metagabbro is massive; locally, it is gneissose or schistose or sheared in zones a few inches wide.
Some common varieties are tremolite, actinolite, asbestus, edenite, hornblende (the last name being also used as a general term for the whole species).
Amphibole is a constituent of many crystalline rocks, as syenite, diorite, most varieties of trachyte, etc. See Hornblende.
Hornblendeschist (Geol.), a hornblenderock of schistose structure.
The mineral relationships and the occurrence of angular enclaves of diorite and meladiorite are characteristic of crystallization from a melt and are in agreement with a magmatic origin.
The presence of hornblende and biotite suggests that the former rock could have been a hornblendediorite.
Quartz sieve textures occur in the biotite and hornblende (Fig.
Hornblende commonly occurs as a euhedral to subhedral prismatic crystal with a maximum length of 2 mm.
Hornblende from the batholithic rocks is generally identified as magnesio-hornblende, ferro-hornblende, actinolitic hornblende, and ferroactinolitic hornblende with small amounts of actinolite and ferroactinolite, according to the nomenclature of Leake (1978) (Fig.
Hornblende in magnetiteseries rocks (0.420 to 0.896; mean 0.674) is lower in atomic Fe +Fe) ratios than hornblende in ilmenite-series rocks (0.541 to 0.926; mean 0.711).
Hornblende is more desirable than mica as a constituent of granite, having cleavage in two planes instead of one, as in mica, and polishing much more easily.
Hornblendegranite.-In addition to the hornblende contained in this granite as the characterizing accessory, fl mica is in nearly all cases likewise found.
Biotite is found as a microscopic constituent in many hornblendegranites, and the name "hornblendegranite" is, therefore, restricted to those in which no biotite is visible to the naked eye.
common hornblende includes the greenish-fl and fl kinds containing more iron.
Hornblende occurs as an essential constituent of many kinds See also:
Buffon, as was his manner, enlarges on the cruel injustice done to these birds by Nature in encumbering them with this deformity, which he declares must hinder them from getting their See also:
The provenance of erratics on the Stony Brook Campus based on Ar-Ar ages of mica and hornblende(Site not responding. Last check: )
Single grain Ar-Ar ages for biotite, muscovite and hornblende have been obtained on representative erratic boulders on the Stony Brook Campus to test the hypothesis that most of the boulders are from the basement of Long Island Sound (Pacholik and Hanson, 2001).
Muscovite, biotite and hornblende grains were co-irradiated with hornblende monitor standard Mmhb (age = 525 Ma, Samson and Alexander, 1987) in the Cd-lined, in core facility (CLICIT) at the Oregon State reactor.
The single grain Ar-Ar ages for mica and hornblende support the hypothesis that the boulders on the Stony Brook Campus were derived from the basement in Long Island Sound and that the basement is dominated by Avalonian terrane granites and gneisses.