Edited by Pavel Pospíšil and David Relich
English term
|
Czech term |
Explanation |
ablation |
ablace |
The process of decreasing
of ice volume of a glacier. Synonym wastage. |
abrasion |
abraze |
The grinding away of a
rock by friction and impact during transportation.
|
absolute age |
absolutní stáří |
Age given in years or some
other unit of time (mostly in million of years). |
abyssal fan |
abysální dejekční
kužel |
Great fan-shaped deposit
of sediment on the deep-sea floor at the base of many
submarine canyons. |
abyssal plain |
abysální rovina |
Very flat sediment-covered
region of the deep-sea floor, usually at the base of the
continental rise. |
accessory minerals |
akcesorické minerály |
Rock-forming minerals
which occur in a rock in a very small amount (several
percents of mineral content) and which have no effect to
classification of a rock. |
acid rocks |
kyselé vyvřelé horniny
|
Igneous rocks with high
amount of silica. They are macroscopically recognizable
by high percentage of quartz, K-feldspars and/or acidic
plagioclases. |
advancing glacier |
postupující ledovec
(rostoucí) |
Glacier with a positive
budget, so that accumulation results in the lower edges
being pushed outward and downward. |
aftershock |
|
Small earthquake that
follows a main shock. |
albite |
albit |
Kind of plagioclase
(acidic) within the feldspar group with formula
NaAlSi3O8. Its colour is light grey to grey. Other
properties see feldspars. |
aleurites |
aleurity |
Clastic sediments or
sedimentary rocks with size of particles between
0,002-0,063 mm. |
allothigenous minerals |
|
Minerals, which were
transported from other place into a newly formed
sediment. These minerals are highly resistent to
weathering processes. |
allotriomorphic minerals
|
alotriomorfně omezené
minerály |
Minerals of igneous rocks
which crystallize as latest in a process of magma
crystallization. It results in a shape of these minerals,
which are forced to crystallize in a space created by
formerly crystallized sorrounding minerals. |
alluvial deposits |
aluviální sedimenty
|
General term for clastic
sedimentary rocks with no cohesion, which have been
transported and deposited by a stream. |
alluvial fan |
aluviální kužel
(dejekční) |
Large fan-shaped pile of
sediment that usually forms where stream´s velocity
decreases as it emerges from a narrow canyon onto a flat
plain at the foot of a mountain range. |
alpine glaciation |
alpínské zalednění
|
Glaciation of a
mountainous area. |
amorphous substance |
amorfní látka |
Substance where atoms are
not ordered in crystal lattice. |
amphibole |
amfibol |
Ferromagnesian mafic
mineral which belongs to silicates. Properties: black in
colour, cleavaged, cleavage planes are stepped rather
than smooth, splintery appearance, columnar, hardness is
from 5 to 6, vitreous or silk luster. |
amphibolite |
amfibolit |
Mostly black, amphibole
(hornblende), plagioclase schist with characteristic
plane parallel structure (compare with hornoblendite).
|
amygdaloidal structure |
mandlovcovitá textura |
Type of structure of
igneous rocks, which is typical for its "almond
shaped" pores secondary filled with material. This
structure is formed after porous structure. |
andesite |
andezit |
Fine-grained igneous rock
of intermediate composition. Up to half of the rock is
plagioclase feldspar with the rest being ferromagnesian
minerals. It is often porphyritic. |
angular |
ostrohranný |
Sharp-edged; lacking
rounded edges or corners. |
anhydrite |
anhydrit |
Anhydrite is a relatively
common sedimentary mineral that forms massive rock
layers. Anhydrite does not form directly, but is the
result of the dewatering of the rock forming mineral
Gypsum (CaSO4-2H2O). Color is ordinarily white, gray or
colorless but also blue to violet. Luster is
vitreous.Crystal habits include the tabular, rectangular
box often elongated in one direction forming a prismatic
crystal. Most commonly massive and granular. Cleavage is
in three directions forming rectangles, but perfect in
one, very good in another and only marginally good in the
third direction. Hardness is 3.5. |
anorthite |
anortit |
Mineral which belongs to
plagioclase feldspar group with formula CaAl2Si2O8. Grey
to dark grey in colour, other properties see feldspars.
|
anticline |
antiklinála |
An arched fold in which
the rock layers usually dip away from the axis of the
fold. |
apatite |
apatit |
Hexagonal mineral with
formula Ca5(PO4,CO3)3(F,OH,Cl). Green, green-brown,
yellow in colour. Hardness is 5. Columnar shape. Poorly
cleavaged. |
aphanitic |
afanitický |
Pertaining to a texture of
rocks in which the crystalline constituents are too small
to be distinguished with the unaided eye. It includes
both microcrystalline and cryptocrystalline textures.
|
aplite |
aplit |
A dike rock consisting
almost entirely of light-coloured mineral constituents
and having a characteristic fine-grained granitic
texture. |
aquifer |
zvodeň |
A body of saturated rock
or sediment through which water can move readily. |
arcose |
arkóza |
A sandstone in which more
than 25% of the grains are feldspar. |
artesian well |
artéská studna |
A well in which water
rises above the aquifer. |
asthenosphere |
astenosféra |
A region of the earth´s
outer shell beneath the lithosphere. The asthenosphere is
of indeterminate thickness and behaves plastically.
|
authigenous minerals |
autigenní minerály |
Minerals which occur on
the place of their origin. |
bar |
|
A ridge of sediment,
usually sand or gravel, that has been deposited in the
middle or along the banks of a stream by a decrease in
stream velocity. |
basal sliding |
|
Movement in which the
entire glacier slides along as a single body on its base
over the underlying rock. |
basalt |
čedič |
A fine-grained, mafic,
igneous rock composed predominantly of ferromagnesian
minerals and with lesser amount of calcium-rich
plagioclase feldspar. Mostly black. |
base level |
úroveň hloubky eroze
|
A theoretical downward
limit for stream erosion of the earth´s surface. |
basic rocks |
bazické vyvřelé horniny
|
Igneous rocks with
relatively high percentage of mafic minerals and low
percentage of silica (amount of SiO2 is between 44 and 52
%). |
batholith |
batolit |
A large discordant pluton
with an outcropping area greater than 100 square
kilometers. |
bedding |
zvrstvení |
An arrangement of layers
or beds of rock. |
bedding plane |
vrstevní plocha |
A nearly flat surface
separating two beds of sedimentary rock. |
bedrock |
skalní podklad |
Solid rock that underlies
soil. |
bentonite |
bentonit |
Rock composed of clay
minerals, mainly montmorillonite, formed mostly by
decomposition in water or weathering on the Earth
surface. |
biochemical sedimentary
rocks |
biochemické sedimenty |
General term for organic
and chemical sedimentary rocks. |
biotite |
biotit |
Iron/magnesium bearing
mica. Black to dark brown in colour, other properties see
mica. |
blowout |
|
A depression on the land
surface caused by wind erosion. |
body waves |
|
Seismic waves that travel
through the earth´s interior. |
bonding |
vazby |
Attachment of an atom to
one or more adjacent atoms. |
borelog |
záznam vrtného profilu
|
Graphical report of a
well. |
boulder |
balvan |
A sediment particle with a
diameter greater than 256 mm. |
boulder loam |
souvková hlína |
Glacial sediment formed as
a result of glacier accumulation, either in front of a
glacier or on its base. It is mostly fine-grained
material with larger fragments. |
breccia |
brekcie |
A fragmental rock whose
components are angular and therefore, as distinguished
from conglomerates, are not waterworn. |
butte |
svědecká hora |
A narrow pinnacle of
resistant rock with a flat top and very steep sides.
|
calcite |
kalcit |
Mineral with the formula
CaCO3. Mostly white, yellow or grey in colour, cleavaged,
glassy luster on cleavage planes, hardness is 3, streak
is always white. Reacts strongly with dilute hydrochloric
acid. |
Cambrian |
kambrium |
The oldest period in
paleozoic, which took place 570-500 million of years ago.
|
canyon |
kaňon |
A long, deep valley with
steep slopes, which was formed as a result of water
stream erosion. |
carbonates |
karbonáty |
A group of minerals, which
have in their formulas CO3 anions. Properties of
individual members of this group are very similar to
calcite. |
Carboniferous |
karbon |
A period in paleozoic
(285-350 million of years ago), in which great amount of
coal was formed. |
cave |
jeskyně |
Naturally formed
underground chamber. |
caving sediments |
nezpevněné nesoudržné
sedimenty |
Sedimentary rocks without
cohesion. |
cement |
pojivo |
The solid material that
precipitates in the pore space of sediments, binding the
grains together into a hard rock. |
cementation |
zpevňování |
The process of chemical
precipitation of material in the spaces between sediment
grains, binding the grains together into a hard rock.
|
Cenozoic |
kenozoikum |
Geological period from
Tertiary (65 million of years ago) to present. |
cirque |
kar |
A steep-sided,
amphitheater-like hollow carved into a mountain at the
head of a glacial valley. |
clastic sedimentary rocks
|
klastické sedimentární
horniny |
A sedimentary rocks
composed of fragments of preexisting rocks, formed by
weathering, transportation and deposition. |
clastic textures |
klastické struktury
|
An arrangement of rock
fragments of different size of particles. This term can
be used only for sedimentary rocks. |
clay |
jíl |
Sediment composed of
particles with diameter less than 0,002 mm. |
clay minerals |
jílové minerály |
A hydrous-aluminium
silicates that occurs as a platy grains of microscopic
size with a sheet silicate structure (e.g. kaolinite,
montmorillonite, illite, glauconite). |
clay shale |
jílová břidlice |
Pelitic sedimentary rock,
mostly laminated. |
claystone |
jílovec |
Partly lithificated
pelitic sediment. |
cleavage |
štěpnost |
The ability of a mineral
to break along preferred planes. It relates to inner
structure of a mineral. |
cleveage plane |
štěpná plocha |
Plane along which mineral
with cleavage breaks. |
cliff |
útes |
Steep, high rock on marine
coast, which arose by water erosion. |
coal |
uhlí |
A sedimentary rock formed
by the consolidation of plant material. It is rich in
carbon, usually black, and burns readily. |
coarse-grained rock |
hrubě zrnitá hornina |
Rock in which most of the
grains are from 3 to 10 mm in size. |
cobble |
valoun |
A sediment particle with a
diameter of 64 to 256 mm. |
coefficient of flatness
|
koeficient plochosti |
Ratio between the longest
and the shortest axis of rock fragment. |
columnar shape |
sloupcovitý tvar |
1. Shape formed by
jointing of some volcanic rocks - parallel, usually
vertical columns, mostly six-sided. 2. Habitus of some
minerals. |
compact structure |
kompaktní textura |
Type of structure of
rocks, where there are no pores in a rock. |
compaction |
kompakce |
A loss in overall volume
and pore space of a rock as a particles are packed closer
together by the weight of overlying material. |
concordant |
konkordantní |
Parallel to layering or
earlier developed planar structures. |
cone of depression |
depresní kužel |
A depression of the water
table formed around a well when water is pumped out; it
is shaped like an inverted cone. |
confined aquifer |
napjatá zvodeň |
An aquifer completely
filled with pressurized water and separated from the land
surface by a relatively impermeable confining bed, such
as shale. |
confining pressure |
všesměrný tlak |
Pressure applied equally
on all surfaces of a body; also called geostatic or
lithostatic pressure. |
conglomerate |
slepenec |
A coarse-grained
sedimentary rock (grains coarser than 2 mm) formed by the
cementation of rounded gravel. |
conchoidal fracture |
lasturnatý lom |
Type of fracture similar
to conch surface. |
contact metamorphism |
kontaktní metamorfóza |
Metamorphism under
conditions in which high temperature is the dominant
factor. |
contact schist |
kontaktní břidlice
|
Metamorphic rock formed
usually on a contact between magma and sedimentary
pelitic rock. |
contact-metamorphic rocks
|
kontaktně metamorfované
horniny |
Metamorphic rocks formed
as a result of contact between magma and some rock. This
type of metamorphism is mostly thermal. |
continental crust |
kontinentální zemská
kůra |
A part of the Earth´s
crust which forms continents. It´s thickness is from 25
km to 80 km, 38 km in average. The thickness of
continental crust and its structure varies according to
geological units. Young alpine mountain belts have
continental crust up to 80 km thick (Himalayas). |
continental drift |
kontinentální drift
|
A concept suggesting that
continents move over the earth´s surface. |
continental glaciation |
kontinentální
zalednění |
The covering of a large
region of a continent by a sheet of glacial ice. |
continental shelf |
kontinentální šelf
|
A submarine platform at
the edge of a continent, inclined very gently seaward
generally at an angle of less than 1!. It is bordered by
continental slope. |
continental slope |
kontinentální svah
|
A relatively steep slope
extending from a depth of 100 to 200 meters at the edge
of the continental shelf down to oceanic depths. |
convection |
konvekční proudění
|
A very slow circulation of
a substance driven by differences in temperature and
density within that substance. |
converging boundary |
konvergentní rozhraní |
Boundary between two
lithospheric plates that are moving toward each other.
|
coquina |
organodetritický vápenec
|
A limestone consisting of
large shells. |
coral reefs |
korálové útesy |
Organogenous rocks on
marine coast composed of coral skeletons. |
core |
zemské jádro |
The central zone of the
earth. It´s radius is 3478 km. |
correlation |
korelace |
Determining age
relationships between rock units or geologic events in
separate areas. |
craton |
kraton |
Portion of a continent
that has been structurally stable for a prolonged period
of time. |
creep |
plouživý pohyb |
Very slow, continuous
downslope movement of soil and rock. |
Cretaceous |
křída |
The last period of
Mesozoic before Tertiary (136-65 millions of year ago).
|
crevasses |
ledovcová trhlina |
Open fissures in a
glacier. |
cross bedding |
křížové zvrstvení
|
An arrangement of
relatively thin layers of rock inclined at an angle to
the more nearly horizontal bedding planes of the larger
rock unit. |
crust |
zemská kůra |
The outer layer of rock,
forming a thin skin over the earth´s surface. |
crust fault |
hlubinný zlom |
Very deep fault (from
tenths to hundreds of kilometers) in the Earth´s crust,
which separates two litospheric plates. |
crustal rebound |
|
The rise of the earth´s
crust after the removal of glacial ice. |
crystalline substance |
krystalická hmota |
Substance with specific
inner structure, which is called crystal lattice. |
crystalline texture |
krystalická struktura |
An arrangement of
interlocking crystals. |
Darcy´s law |
Darcyho zákon |
Formula, in which relation
between hydraulic gradient, hydraulic conductivity and
soak velocity is defined. |
debris |
suť |
Any unconsolidated
material at the earth´s surface. |
debris avalanche |
bahnotok |
A very rapidly moving,
turbulent mass of debris, air and water. This is the
fastest variety of debris flow. |
deflation |
deflace |
The removal of clay, silt
and sand particles from the land surface by wind. |
delta |
delta |
A body of sediment
deposited at the mouth of a river when the river velocity
decreases as it flows into a standing body of water.
|
denudation |
denudace |
General term for lowering
of the earth surface by processes such as erosion etc.
|
deposition |
usazováni |
The settling or coming to
rest of transported material. |
depth of focus |
hypocentrum zemětřesení
|
Distance between the focus
and the epicenter of an earthquake (perpendicular
distance between the focus and the Earth surface).
|
desert |
poušť |
A region with low
precipitation (usually defined as less than 25 cm per
year) |
Devonian |
devon |
Period of Paleozoic
(between 395-345 million of years ago). |
diabase |
diabas |
A rock of basaltic
composition, consisting essentially of labradorite and
pyroxene,and characterized by ophitic texture (discrete
crystals or grains of pyroxene fill the interstices
between lath-shaped feldspar crystals). |
diamond |
diamant |
Mineral which is composed
of carbon, the hardest mineral on the Earth
(hardness=10). It was formed in conditions of high
pressure and temperature. |
diatomite |
diatomit |
Organogenous sediment
composed mostly of very small silica shells (shells of
organisms called Diatomacea) |
dike |
pravá žíla |
A tabular, discordant
intrusive structure. |
diorite |
diorit |
Plutonic igneous rock of
intermediate composition. Up to half of the rock is
plagioclase feldspar and the rest is ferromagnesian
minerals. |
dip |
sklon |
The angle that a
structural surface, e.g. a bedding or fault plane, makes
with a horizontal. See dip angle, direction of dip.
|
dip angle |
úhel sklonu |
A vertical angle measured
downward from the horizontal plane to an inclined plane.
|
dip-slip fault |
|
A fault in which movement
is parallel to the dip of the fault surface. |
direction of dip |
směr sklonu |
The compass direction in
which the angle of dip is measured. |
disappearing stream |
ponor |
Surface stream, which
apparently disappears under ground and appears again on a
surface at different place. This type of stream is common
in area with limestones (karst). |
discordant |
diskordantní |
Not parallel to any
layering or parallel planes. |
diverging boundary |
divergentní rozhraní |
Boundary separating two
lithospheric plates moving away from each other. |
dolomite |
dolomit |
1. Type of mineral with
formula (Ca,Mg)(CO3)2. It´s properties are very similar
to calcite, but it reacts slowly with dilute hydrochloric
acid unless powdered. 2. A sedimentary rock composed
mostly of the mineral dolomite. |
Dolostone |
dolomit |
Synonym for dolomite. |
downcutting |
hloubková eroze |
A valley-deepening process
caused by erosion of a stream bed. |
drainage |
odvodnění |
Removal of water from some
area by system of channels, ditches or drainage wells.
|
drawdown |
|
The lowering of the water
table near a pumped well. |
drilling |
vrtání |
Making of a vertical round
shaped hole under the surface for different purpose - for
example obtain a underground water or to obtain some
information about geologic conditions. |
drumlin |
drumlin |
A long, streamlined hill
made of till. |
dry stream bed |
vyschlé koryto řeky
|
Stream bed, which is
temporary without water. |
dull luster |
matný lesk |
|
earthflow |
sesuv |
Slow-to- rapid mass
wasting in which debris moves downslope as a very viscous
fluid (See landslide). |
earthquake |
zemětřesení |
A trembling or shaking of
the ground caused by the sudden release of energy stored
in the rocks beneath the surface. |
eclogite |
eklogit |
Basic metamorphic rock
consisting mainly from minerals garnet and pyroxene
(omphacite). Mostly dark grey to black in colour with
massive structure. |
effusive rocks |
výlevné horniny |
Igneous rocks which have
solidified on the earth surface. |
end moraine |
čelní moréna |
A ridge of till piled up
along the front edge of a glacier. |
environment of deposition
|
sedimentační prostředí
|
The location in which
deposition occurs, usually marked by charakteristic
physical, chemical or biological conditions. |
epicenter |
epicentrum zemětřesení
|
The point on the earth´s
surface directly above the focus of an earthquake.
|
epidote |
epidot |
It occurs sometimes in
form of finely crystalline masses in joints of a rock,
rarely forms elongate crystals. Color is
"pistachio" green to yellowish or brownish
green, also brown to black. Hardness is more than 5,
cleavaged. |
erlan |
erlan |
Contact metamorphic rock
consisting mainly of calcium silicates. |
erosion |
eroze |
The physical removal of
rock by an agent such as running water, glacial ice, or
wind. |
erratic |
eratický balvan |
An ice-transported boulder
that does not derive from bedrock near its present site.
|
esker |
esker |
A long, sinuous ridge of
sediment deposited by glacial meltwater. |
essential minerals |
hlavní (podstatné)
horninotvorné minerály |
Rock forming minerals,
which form essential part of a rock. They are important
for classification of a rock. |
evaporites |
evapority |
Sedimentary rocks that
form from crystals precipitating during evaporation of
water. |
even-grained texture |
stejnoměrně zrnitá
struktura |
Type of texture of igneous
rocks, where minerals in a rock are not very different in
size (opposite term to porphyritic structure). |
exfoliation |
exfoliace |
The stripping of
concentric rock scales to slabs from the outer surface of
a rock mass. |
extrusive rocks |
výlevné vyvřelé
horniny |
Any igneous rocks that
form at the earth´s surface, whether it soldifies
directly from a lava flow or is pyroclastic. |
fall |
skalní řícení |
The situation in mass
wasting that occurs when material free-falls or bounces
down a cliff. See rockfall. |
fault |
zlom |
A fracture in bedrock
along which movement has taken place. |
feldspars |
živce |
Group of most common
minerals of the earth´s crust. All feldspars contain
silicon, aluminium, and oxygen and may contain potassium,
calcium, and sodium. Pink, white to dark grey, rarely
green in colour. Hardness is around 6. Perfect cleavage,
vitreous luster when fresh, dull when weathered.
Attention: According to luster on cleavage planes are
feldspars very often confused with muscovite. |
felsic rocks |
světlé vyvřelé horniny
|
Silica rich igneous rocks
with silica content more then 65%. |
fine-grained rocks |
jemnozrnné horniny |
A rocks (except clastic
sediments) in which most of the mineral grains are
between 0,33-0,01 mm in size. |
fiord |
fjord |
A coastal inlet that is a
glacially carved valley, the base of which is submerged.
|
firn |
firn |
A compacted mass of
granular snow, transitional between snow and glacial ice.
|
fissured clays |
potrhané jíly |
Clays with a lot of small,
irregular fissures. |
flexure |
ohyb |
Bending of beds (without
rupture) as a result of long lasting and slow tectonic
pressure. |
flint |
pazourek |
A dense, fine-grained form
of silica which is very tough and breaks with a
conchoidal fracture and cutting edges. It occurs in
cretaceous cliffs. |
flood erosion |
|
Erosion caused by the high
velocity and large volume of water in a flood. |
flood plain |
inundační území
|
A broad strip of land
built up by sedimentation on either side of a stream
channel. |
flow |
tečení |
A type of movement that
implies that a descending mass is moving downslope as a
viscous fluid. |
fluidal structure |
proudovitá textura
|
Structure of igneous
rocks, where rock particles have preferred direction in
orientation. |
fluorite |
fluorit |
Mineral with formula CaF2.
It is a basic raw material for fluor and fourth member of
Moh´s scale. Purple, green, yellow in colour. Perfect
cleavage, vitreous luster. |
focus |
ohnisko zemětřesení
(hypocentrum) |
The point within the earth
from which seismic waves originate in an earthquake.
|
foids |
zástupci živců |
Group of minerals formed
instead of feldspars within the process of magma
crystallization, when amount of SiO2 in magma is reduced.
Main members of this group are: leucite, nepheline,
analcime, sodalite, nosean, hauyne. |
fold |
vrása |
Bend in layered bedrock of
sinusoidal shape. |
foliation |
foliace |
Parallel alignment of
structural features of a rock. |
foliation plane |
foliační plocha |
Plane with parallel
alignment to structural features of a rock. |
fossiliferous limestone
|
organogenní vápenec |
Limestone composed of
fossil shells or skeletons. |
fossils |
fosílie |
Traces or fragments of
skeletons of plants or animals preserved in rock. |
fracture |
zlom |
The way a substance breaks
where not controlled by cleavage. |
fracture plane |
lomná plocha |
Curved plane formed by
fracture, often conchoidal. |
fragments of rocks |
úlomky hornin |
Pieces of rock decoposed
by mechanical or chemical weathering. |
fresh rock |
nezvětralá hornina
|
Rock not affected by
weathering. |
frost action |
účinek mrazu |
Mechanical weathering of
rock by expanzion of freezing water. |
frost heaving |
|
The lifting of rock or
soil by the expansion of freezing water. |
frost wedging |
|
A type of frost action in
which the expansion of freezing water pries a rock apart.
|
gabbro |
gabro |
A mafic, coarse-grained
igneous rock composed predominantly of ferromagnesian
minerals and with lesser amounts of calcium-rich
plagioclase feldspar. |
gaining stream |
|
A stream that receives
water from the zone of saturation. |
garnet |
granát |
Reddish brown, yellowish
tan in clolour, vitreous to pitch luster. Hardness is 6.5
to 7.5. Without cleavage. Mineral which often occurs in
metamorphic rocks, sometimes in igneous rocks. |
geologic cross-section |
geologický řez |
A representation of a
portion of the earth in a vertical plane. |
geologic time scale |
geologická časová
škála |
Geologic term, which means
mirroring of Earth history expressed in a form of
geologic periods. |
geology |
geologie |
Scientific branch studying
origin and development of the Earth and other planets.
|
geophysics |
geofyzika |
The application of
physical laws and principles to a study of the earth.
|
geothermal energy |
geotermální energie
|
Thermal energy produced by
the Earth. Some sources of this energy can be harnessed
and used by a man. |
geothermal gradient |
geotermální gradient |
Rate of temperature
increase associated with increasing depth beneath the
surface of the earth (normally about 25°C/km). |
geyser |
gejzír |
A type of hot spring that
periodically erupts hot water and steam. |
geyserite |
gejzírit |
A deposit of silica that
forms around many geysers and hot springs. |
glacial age |
doba ledová |
Geologic period in
Quaternary, when glaciers were advancing. |
glacial budget |
|
Sum of advancing and
receding of glacier per one year (positive and negative).
|
glaciation |
zalednění |
General term for covering
of the Earth surface by a glacier. |
glacier |
ledovec |
A large, long-lasting mass
of ice, formed on land by the compaction and
recrystallization of snow, which moves because of its own
weight. |
glacier recession |
ústup ledovce |
Receding of a glacier.
|
glacier tonque |
splaz ledovce |
"Freezing stream
shaped" accumulation of ice on edge of a glacier.
|
glassy luster |
skelný lesk |
A luster that gives a
substance a glazed, porcelainlike appearance. See
vitreous luster. |
glauconite |
glaukonit |
Dark green coloured clay
mineral occuring in some sands and sandstones. Properties
see clay minerals. |
gneiss |
rula |
A metamorphic rock
composed prevailingly of quartz, feldspars and micas
arranged in plane parallel structure. |
graben |
příkopová propadlina
|
A down-dropped block
bounded by normal faults. |
graded bed |
|
A single bed with coarse
grains at the bottom of the bed and progressively finer
grains toward the top of the bed. |
graded bedding |
gradační zvrstvení
|
An arrangement of layers
of clastic sediments and sedimentary rocks. Each layer
has different size of particles and granularity of layers
tends topward from coarse to fine. |
granite |
granit |
A felsic, coarse-grained,
intrusive igneous rock composed mostly of quartz,
feldspars and often containing micas. It belongs to group
of granitoids. |
granite porphyr |
žulový porfyr |
Dike rock with composition
similar to granite. It differs only by a texture and
structure. |
granitoids |
granitoidy |
A group of "granite
like rocks", which differs from each other only by
type of feldspar. |
granoblastic texture |
granoblastická struktura |
Texture of metamorphic
rocks, which is characterized by "grain shaped"
minerals, e.g. marble. |
granodiorite |
granodiorit |
Igneous plutonic rock
belonging to group of granitoids. It has composition
similar to granite except the ratio between types of
feldspar (plagioclases>K-feldspars). |
granulite |
granulit |
High-grade metamorphic
rock, ligh-grey coloured. It is composed of quartz and
feldspars, mostly with presence of small garnet grains.
|
graphic texture |
písmenková struktura
|
Special texture created by
intergrowth of feldspars and quartz, which looks like
hieroglyfic letters. |
graphite |
grafit |
Mineral formed of carbon.
Gray to black in colour. Hardness is 1. It may have dull
luster, greasy feel, soils paper and fingers. |
gravel |
štěrk |
Sediment composed of
rounded particles coarser than 2 mm in diameter. |
greywacke |
droba |
A sandstone with more than
20% of unstable particles and feldspars within psammitic
fraction and more then 15% of finegrained matrix. |
ground moraine |
spodní (bazální)
moréna |
A blanket of till
deposited under a glacier or released as glacier ice
melted. |
groundmass |
základní hmota |
The material between the
phenocrysts in porphyritic igneous rock. It includes the
basis or base as well as the smaller crystals of the
rock. Essentially synonymous with matrix. |
groundwater |
podzemní voda |
The water that lies
beneath the ground surface, filling the cracks, crevices,
and pore space of rocks. |
gypsum |
sádrovec |
Mineral with formula
CaSO4. It is formed by evaporation. Clear, white, light
grey in colour. Hardness is 2. Vitreous to pearly luster,
brittle sheets. Perfect cleavage. |
habit |
habitus |
Term describing shape of a
crystal (e.g. tabular, columnar). |
halite |
sůl kamenná |
Mineral with formula NaCl.
It is formed by evaporation. Clear to grey in colour.
Hardness is 2.5. Perfect cleavage. Salty taste. |
hanging valley |
visuté údolí |
A smaller valley that
terminates abruptly high above a main valley. |
headward erosion |
zpětná eroze |
The lenghtening of a
valley in an uphill direction above its original source
by gullying, mass wasting, and sheet erosion. |
hematite |
hematit |
(1) Mineral with formula
Fe2O3. Mostly fine grained, reddish brown in colour.
Hardness is 1.5 to 5.5, dull luster. It occurs in form of
earthy masses. It is product of chemical weathering
(oxidation). (2) Rarely with formula Fe3O4, steel grey to
dull red in colour. Hardness is 6. May be micaceous (tiny
flakes) or massive. |
hemicrystalline rocks |
hemikrystalické horniny |
Volcanic rocks, which have
cooled very quickly. Part of rock mass is composed of
volcanic glass. |
hinge line |
osa vrásy |
Line about which a fold
appears to be hinged. Line of maximum curvature of a
folded surface. |
hinge plane |
rovina vrásy |
See axial plane. |
holocrystalline rocks |
holokrystalické horniny |
Igneous rocks with fully
crystalized rock mass. |
horizontal bedding |
horizontální zvrstvení |
Type of bedding, where
layers are oriented horizontally. |
hornblende |
obecný amfibol |
Common amphibole
frequently found in igneous and metamorphic rocks.
Properties see amphibole. |
hornfels |
kontaktní rohovec |
A fine-grained, unfoliated
metamorphic rock. |
horst |
hrásť |
An up-raised block bounded
by normal faults. |
hyaline texture |
hyalinní struktura
|
Texture of volcanic rocks
or their groundmass, which is formed by amorphous
substance. |
hydraulic conductivity |
koeficient filtrace |
Number characterizing
permeability of rocks. |
hydraulic gradient |
hydraulický gradient |
The ratio between vertical
difference of heights of two water tables and their
horizontal distance. |
hydrologic cycle |
hydrologický cyklus
|
The movement of water and
water vapor to the atmosphere, to the land, and to the
atmosphere again. |
hypidiomorphic minerals
|
hypidiomorfně omezené
minerály |
Partly confined mineral
grains formed during crystallization of magma. |
hypocenter |
hypocentrum zemětřesení
|
Synonym for the focus of
an earthquake. |
chalk |
křída |
A very fine-grained
bioclastic limestone, which often forms high white cliffs
on the coast. |
chalkopyrite |
chalkopyrit |
Metallic mineral with
formula CuFeS2. Golden yellow or greenish yellow in
colour. Hardness is 3.5 to 4. Massive. |
chemical sedimentary rocks
|
chemické sedimentární
horniny |
A sedimentary rocks
composed of material precipitated directly from solution.
|
chemical weathering |
chemické zvětrávání |
The decomposition of rock
resulting from exposure to water and atmospheric gases.
|
chert |
rohovec |
A hard, compact,
fine-grained sedimentary rock formed almost entirely of
silica. |
chlorite |
chlorit |
Mineral belonging to mica
group formed mostly during metamorphism. It can be also
formed by alteration processes. Green to blackish green
in colour. Dull to pearly luster. Hardness 2 to 2.5. May
have faint green-yellow streak. Crystal flakes are
flexible but not elastic. Finely crystalline aggregates
common. |
ice cap |
ledovcová čapka |
A glacier covering a
relatively small area of land but not restricted to a
valley. |
ice sheet |
kontinentální ledovec
|
A glacier covering a large
area (more than 50 000 square kilometers) of land.
|
iceberg |
ledovec |
Block of glacier-derived
ice floating in water. |
idiomorphic minerals |
idiomorfně omezené
minerály |
Completely confined
mineral grains formed during crystallization of magma.
|
igneous rocks |
vyvřelé horniny |
A rocks formed or
apparently formed from solidification of magma. |
illite |
illit |
Non-swelling type of clay
mineral. Properties see clay minerals. |
inner core |
vnitřní jádro |
The most inner part of the
Earth. |
intermediate igneous rocks
|
intermediární vyvřelé
horniny |
Igneous rocks with a
chemical content between felsic and mafic compositions.
|
intrusive bodies |
intruzívní tělesa
|
Bodies formed by magma
crystallization under the earth surface. |
intrusive rocks |
intruzivní horniny
|
Rocks that appears to have
crystallized from magma emplaced in surrounding rock.
|
isoclinal fold |
izoklinální vrása
|
A fold in which the limbs
are parallel to one another. |
isostasy |
izostáze |
The balance or equilibrium
between adjacent blocks of crust resting on a plastic
mantle. |
isostatic adjustment |
izostatické vyrovnání |
Concept of vertical
movement of sections of the earth´s crust to achieve
balance or equilibrium. |
izometric shape |
izometrický tvar |
Term describing ball-like
shape of mineral grains. |
joint |
prasklina, trhlina |
A fracture or crack in
bedrock along which essentially no displacement has
occured. |
Jurassic |
jura |
A period in Mesozoic
(145-195 million of years ago). |
K-feldspars |
draselné živce |
Subgroup of feldspars
containing potassium in the structure (KAlSi3O8).
Properties see feldspars. |
kaolin |
kaolin |
Sediment composed mostly
of clay mineral kaolinite. It was formed as a residual
rock by processes of chemical weathering. |
kaolinite |
kaolinit |
Non-swelling member of
clay mineral group. Properties see clay minerals. |
karst |
kras |
An area formed mostly of
limestones with many sinkholes and a cave system beneath
the land surface, usually lacking a surface stream.
|
kinetic metamorphism |
dislokační metamorfóza |
Special type of
metamorphism caused by tectonic forces in a fold zone.
|
kyanite |
kyanit |
Mineral with formula
Al2SiO5 formed during metamorphism. Light blue to
greenish blue in colour, cleavaged. Hardness is 5
parallel to long direction of crystal and 7 across
crystal. It forms blade-shaped crystals and has vitreous
luster. |
labradorite |
labradorit |
Member of plagioclase
subgroup with special optical effects (it reflects
daylight as blue in some slices). Properties see
feldspars. |
lamination |
laminace |
The layering or bedding
less than 1 cm in thickness in a sediment or a
sedimentary rock. |
landslide |
sesuv |
The general term for a
slowly to very rapidly descending rock or debris (see
earthflow). |
lateral erosion |
boční eroze |
Erosion and undercutting
of stream banks caused by a stream swinging from side to
side across its valley floor. |
lateral moraine |
boční moréna |
A low ridgelike pile of
till along a side of a glacier. |
lava |
láva |
Magma on the earth's
surface. Fluid rock such as that which issues from a
volcano or a fissure in the earth's surface. |
lava flow |
lávový proud |
Long, narrow stream of
lava flowing downhill from a volcano. |
lava sheet |
lávový příkrov |
Wide-spreaded sheet of
lava covering large area around a volcano. |
lepidoblastic texture |
lepidoblastická struktura |
Type of metamorphic
texture formed mostly of scaled minerals. |
limb |
rameno vrásy |
Portion of a fold shared
by an anticline and a syncline. |
limestone |
vápenec |
A sedimentary rock
composed mostly of calcite. |
limonite |
limonit |
Limonite (Fe2O3.nH2O). is
a general name for several rust-like hydrous iron oxides.
It usually forms rust-like coatings on rocks.
Yellow-brown, orange-brown to dark brown in colour.
|
lithification |
zpevňování (diageneze)
|
The consolidation of
sediment into sedimentary rock. |
litosphere |
litosféra |
The rigid outer shell of
the earth, 70 to 125 or more kilometers thick. |
local metamorphic rocks
|
lokálni metamorfované
horniny |
Rocks produced by local
metamorphism. |
local metamorphism |
lokální metamorfóza |
Metamorphism involving
relatively high temperature or pressure which affects
small area. |
loess |
spraš |
A fine-grained deposit of
wind-blown dust containing CaCO3 often in the form of
"nodules". |
loessloam |
sprašová hlína |
Eolic sediment formed by
leaching of CaCO3 from loess. |
losing stream |
|
Stream that loses water to
the zone of saturation. |
lower mantle |
spodní plášť |
One of the inner shells of
the earth. |
luster |
lesk |
The quality and intensity
of light reflected from the surface of a mineral. |
macroscopically dense |
makroskopicky celistvý |
Type of rock texture
(according to absolute size of grains) with
macroscopically non-visible grains. |
mafic rocks |
tmavé vyvřelé horniny
|
Igneous rocks with low
amount of silica. They are composed mostly of Fe, Mg
rock-forming minerals. |
magma |
magma |
Molten rock, usually
mostly silica. It may contain dissolved gases as well as
some solid minerals. |
magma chamber |
magmatický krb |
Huge body of magma
situated beneath the surface where magma is accumulated.
|
magnitude |
magnitudo zemětřesení
|
A measure of the energy
released during an earthquake. |
mantle |
zemský plášť |
A thick shell of rock that
separates the earth's crust above from the core below.
|
marble |
mramor |
A fine- or coarse-grained
metamorphic rock composed of interlocking calcite (or
dolomite) crystals. |
marl |
slín |
Clay with high amount of
CaCO3 (25-75%). |
marl slate |
slínitá břidlice
|
Clayshale with high amount
of CaCO3 (25-75%). |
marlite |
slínovec |
Partly lithificated
pelitic sediment with significant amount of CaCO3
(25-75%). |
mass movement |
svahový pohyb |
Movement, caused by
gravity, in which bedrock, rock debris, or soil moves
downslopein bulk. |
mass wasting |
svahový pohyb |
Equivalent term to mass
movement. |
massive structure |
všesměrně zrnitá
textura |
Structure without
stratification, flow-banding, foliation, schistosity,
etc. |
matrix |
základní hmota |
Fine-grained material
found in the intergranular space between larger grains of
sedimentary rocks. |
meander |
meandr |
A pronounced sinuous curve
along a stream's course. |
meander cutoff |
|
A new, shorter channel
across the narrow neck of a meander. |
medial moraine |
střední moréna |
A single long ridge of
till on a glacier, formed by adjacent lateral moraines
joining and being carried downglacier. |
medium-grained rock |
středně zrnitá hornina |
Rock in which most of the
grains are from 1 to 2 mm in size. |
mechanical weathering |
mechanické zvětrávání |
The physical
disintegration of rock into smaller pieces. |
melaphyre |
melafyr |
Volcanic rock, formerly
porous Mesozoic basalt where pores were secondary filled
with other minerals. Its typical structure is
amygdaloidal. |
mesa |
tabulová hora |
A broad, flat-topped hill
bounded by cliffs and capped with a resistant rock layer.
|
mesh structure |
okatá textura |
Structure of some
metamorphic rocks composed of ellipsoidal mineral grains.
|
Mesozoic |
mesozoický |
Geological era that
followed the Paleozoic Era and preceded the Cenozoic Era
(from 225 to 65 mil. of years ago). |
metallic luster |
kovový lesk |
Luster giving a substance
the appearance of being made of metal. |
metamorphic rocks |
metamorfované horniny
|
Rocks produced by
metamorphism. |
metamorphism |
metamorfóza |
The transformation of
preexisting rock into structurally or mineralogically
distinct new rock as a result of high temperature, high
pressure, or both, but without the rock melting process.
|
metaquarcite |
metakvarcit |
Metamorphic rock composed
mostly of quartz with micas on foliation planes. |
metaquartzite |
metakvarcit |
A rock composed of
sand-sized grains of quartz that have been welded
together during metamorphism. |
micas |
slídy |
Group of minerals
belonging to sheet-silicates with variable size of grains
and colour. Significant properties are: hardness 2.5,
perfect cleavage, glassy to pearl luster and elasticity
of scales. |
mid-oceanic ridge |
stoedooceánský hobet
|
A giant mountain range
that lies under the ocean and extends around the world.
|
migmatite |
migmatit |
Mixed igneous and
metamorphic rockwith typical migmatitic structures.
|
mineral |
minerál |
A naturally occuring,
inorganic, homogenous, crystalline or amorphous mostly
solid that has a definite chemical composition. |
mineral content |
minerální složení
|
Term describing
composition of a rock. |
mineral hardness |
tvrdost minerálu |
The relative easy or
difficulty with which a smooth surface of a mineral can
be scratched; commonly measured by Mohs' scale. |
modified Mercali scale |
modifikovaná Mercaliho
škála |
Scale expressing
intensities of earthquakes (judged on amount of damage
done) in Roman numerals ranging from I to XII. |
Moh´s scale of hardness
|
Mohrova stupnice tvrdosti
|
Scale on which ten
minerals are designated as standards of hardness. |
Mohorovieie diskontinuity
|
Mohorovieieova
diskontinuita |
The boundary separating
the crust from the mantle beneath it (also called Moho).
|
monomict |
monomiktní |
Within the psefitic,
clastic sedimentary rocks, formed from one type of
fragments. |
montmorillonite |
montmorillonit |
Swelling type of clay
mineral. Properties see clay minerals. |
moraine |
moréna |
A body of till either
being carried on a glacier or left behind after a glacier
has receded. |
mud |
bahno |
Term loosely used for silt
and clay, usually wet. |
mudcracks |
bahenní praskliny |
Polygonal cracks formed in
very fine-grained sediment as it dries. |
mudflow |
bahnotok |
A flowing mixture of
debris and water, usually moving down a channel. |
mudpot |
bahenní sopka |
Specific type of hot
spring that contains thick, boiling mud. |
mudstone |
slínovec |
A fine-grained sedimentary
rock that lacks shale's laminations and fissility.
|
muscovite |
muskovit |
Transparent or white mica
that lacks iron and magnesium. Properties see micas.
|
nacreous luster |
perleťový lesk |
See pearly luster. |
natural glass |
vulkanické sklo |
Amorphous form of silica
formed by very fast cooling of lava. |
nematoblastic texture |
nematoblastická struktura |
Metamorphic texture formed
mostly of columnar or spicular minerals. |
Neogene |
neogenní |
Younger epoch of Tertiary
period (from 1.8 to 25 mil. of years ago). |
oblique-slip fault |
|
A fault with both
strike-slip and dip-slip components. |
obsidian |
obsidian |
Volcanic glass black in
colour with typical conchoidal fracture. |
oceanic crust |
oceánská kura |
The thin, basaltic crust
under oceans. |
oceanic trench |
hlubokomooský poíkop
|
A narrow, deep through
parallel to the edge of a continent or an island arc.
|
olivine |
olivín |
A ferromagnesian mineral
with the formula (Fe, Mg)2SiO4. Yellowish green to green
in colour, conchoidal fracture but not obvious cleavage,
with vitreous luster. Hardness is 6.5 to 7. Most olivine
occurs in a form of accumulations of small crystals in
dark-coloured igneous rocks (e.g. basalt). |
oolitic limestone |
oolitický vápenec
|
A limestone formed from a
small spheres of calcite precipitated from seawater.
|
open fold |
otevoená vrása |
A fold with gently dipping
limbs (angle between limbs 70-120). |
orbicular structure |
kulovitá textura |
Special type of structure
of plutonic rocks where feldspars are in concentric
arrangement. |
Ordovician |
ordovický |
Period in lower Paleozoic
(from 435 to 500 mil. of years ago). |
ore |
ruda |
Naturally occuring
material that can be profitably mined. |
organic sedimentary rocks
|
organogenní
sedimentární horniny |
Rocks composed mostly of
the remains of plants and animals. |
organic sediments |
organogenní sediment
|
Sediments composed mostly
of the remains of plants and animals. |
orogeny |
orogen |
An episode of intense
deformation of the rocks in a region, generally
accompanied by metamorphism and plutonic activity.
|
orthoclase |
ortoklas |
A potassium feldspar with
the formula KAlSi3O8. Properties see feldspars. |
orthogneiss |
ortorula |
Type of gneiss formed from
igneous rocks. |
outcrop |
výchoz |
A surface exposure of bare
rock, not covered by soil or vegetation. |
outer core |
vnijší jádro |
A thick shell of rock
between inner core and lower mantle. |
overturned fold |
poekocená vrása |
A fold in which both limbs
dip approximatelly in the same direction. |
oxbow lake |
slepé rameno |
A crescent-shaped lake
occupying the abandoned channel of a stream meander that
is isolated from the present channel by a meander cutoff
and sedimentation. |
P-waves |
p-vlny |
Compressional waves
(seismic waves) in which rock vibrates parallel to the
direction of wave propagation. |
Paleogene |
paleogen |
Older epoch of Tertiary
period (from 23.7 to 66.4 mil. of years ago). |
Paleozoic |
paleozoikum |
Geological era that
followed the Precambrian and during which began with the
appearance of complex life, as indicated by fossils (from
245 to 570 mil. of years ago). |
paragneiss |
pararula |
Type of gneiss formed from
sedimentary rocks. |
parent rock |
mateená hornina |
Original rock before being
metamorphosed. |
pearly luster |
perleťový lesk |
A luster that gives a
substance pearly appearance. |
pebble |
oblázek |
A sediment particle with a
diameter of 2 to 64 mm. |
pegmatite |
pegmatit |
Extremely coarse-grained
igneous rock formed mainly of feldspars and quartz
together with micas and other minerals. It has zonal
structure. In czech classification it belongs to dike
rocks, in english classification to plutonic rocks.
|
pelagic sediment |
pelagické sediment
|
Sediment made up of
fine-grained clay and skeletons of microscopic organisms
that settle slowly down through the ocean water to the
sea bottom. |
pelites |
pelity |
Within the clastic
subgroup of sediments and sedimentary rocks the most
fine-grained category (<0.002 mm). |
pencil structure |
stébelnatá textura
|
Rare type of structure of
metamorphic rocks characterized by mineral grains which
are extremly elongated along one axis and arranged in
linear parallel structure. |
perlite |
perlit |
Type of volcanic glass. It
seems to be composed of many small particles
"pearls". |
permeability |
permeabilita |
The capacity of a rock to
transmit a fluids (liquids or gases). |
Permian |
perm |
The youngest period of
Paleozoic (from 245 to 286 mil. of years ago). |
phaneritic |
faneritický |
A textural term applied to
igneous rocks in which all the crystals of the essential
minerals can be distinguished with the unaided eye. The
adjective form phaneritic is currently used more
frequently than the noun. |
phenocryst |
porfyrická vyrostlice
|
Any of the large crystals
in porphyritic igneous rock. |
phonolite |
znilec (fonolit) |
Type of rock composed of
feldspars, foids, pyroxenes and amphiboles. |
phthanite |
buli?nik |
Biochemical sedimentary
rock, mostly black in colour, composed of silica. |
phyllite |
fylit |
A metamorphic rock in
which clay minerals have recrystallized into microscopic
micas, giving the rock a silky sheen. |
pitch luster |
smolný lesk |
A luster that gives a
substance pitch appearance. |
pitchstone |
smolek |
Type of volcanic glass
with typical pitch luster. |
plagioclases |
sodnovápenaté ?ivce
|
Subgroup of feldspars
containing sodium and/or calcium in addition to
aluminium, silicon, and oxygen. Properties see feldspars.
|
plate tectonics |
desková tektonika |
A theory that the earth's
surface is divided into a few large, thick plates that
are slowly moving and changing in size. Intense geologic
activity occurs at the plate boundaries. |
plateau |
náhorní rovina |
Broad, flat-topped area
elevated above the surrounding land and bounded, at least
in part, by cliffs. |
plunging fold |
vrása |
A fold in which the hinge
line (or axis) is not horizontal. |
pluton |
pluton |
An igneous body that
crystallized deep underground. |
plutonic rocks |
hlubinné horniny |
Igneous rocks formed at
great depth. |
polar wandering |
migrace pólu |
An apparent movement of
the earth's poles. |
polymict |
polymiktni(valouny více
druhu) |
Within psefitic sediments
or sedimentary rocks, term describing composition of many
types of fragments. |
porcelanite |
porcelanit |
Metamorphic rock with
typical conchoidal fracture and sharp edges which was
formed by contact metamorphism of pelitic sediments.
|
pore space |
intergranulární prostor
|
The total amount of space
taken up by openings between sediment grains. |
porosity |
pórosita |
The percentage of a rock's
volume that is taken up by openings. |
porous structure |
pórovitá textura |
Structure of a rock where
part of rock volume is taken up by openings. |
porphyritic texture |
porfyrická struktura |
Texture of those igneous
rocks in which larger crystals (phenocrysts) are set in a
finer groundmass which may be crystalline or glassy, or
both. |
porphyroblastic texture
|
porfyroblastická
struktura |
Texture of metamorphic
rocks very similar to porphyritic texture of igneous
rocks (groundmass cannot be glassy). |
potassium feldspar |
draselný ?ivec |
A feldspar with the
formula KAlSi3O8. |
Precambrian time |
prekambrium |
The vast amount of time
that preceded the Paleozoic Era (before 570 mil. of
years). |
psammites |
psamity |
Clastic sediments or
sedimentary rocks with sizes of particles between 0.06
and 2 mm. |
psefites |
psefity |
Clastic sediments or
sedimentary rocks with size of particles over 2 mm.
|
pyrite |
pyrit |
Mineral with formula FeS2
with "gold" appearance. It is sometimes present
as accessory mineral in igneous rocks. |
pyroclastic rocks |
pyroklastika |
Rocks formed by
lithification of pyroclasts. |
pyroclasts |
pyroklastika |
Fragments of rocks formed
by volcanic explosion. |
pyroxene |
pyroxen |
Ferromagnesian mafic
mineral which belongs to silicates. Black to dark-green
in colour, vitreous to dull luster. Hardness is from 5 to
6. It has two imperfect cleavages meet at nearly 90
degrees (it is not often macroscopically visible). Shape
is usually short columnar. |
quarry |
lom |
An open or surface
working, usually for the extraction of building stone, as
slate, limestone, etc. In its widest sense the term mines
includes quarries, and has been sometimes so construed by
the courts; but when the distinction is drawn, mine
denotes underground workings and quarry denotes
superficial workings. |
quartz |
koemen |
Mineral with the formula
SiO2. In the nature it occurs in many different colours,
but as a rock forming mineral it is usually light grey or
grey in colour. Hardness is 7, usually forms
allotriomorphic grains.They are macroscopically
recognizable from feldspars by fracture planes with
vitreous luster (no cleavage planes). |
quartz diorite |
koemenný diorit |
Plutonic rock belonging to
granitoid group, where plagioclases prevail over
K-feldspars. |
quartzite |
koemenec |
A quartz rock derived from
sandstone, composed dominantly of quartz, and
characterized by such thorough induration, either through
cementation with silica or through recrystallization,
that it is essentially homogeneous and breaks with
vitreous surfaces that transect original grains and
matrix or interstitial material with approximatelly equal
ease. |
Quaternary |
kvartér |
The youngest geological
period; includes the present time (from 1.8 mil. of years
ago to present). |
receding glacier |
ustupující ledovec
(zmenšující se) |
A glacier with a negative
budget, which causes the glacier to grow smaller as its
edges melt back. |
Recent |
recentní (soueasný)
|
Formed in the present
time. |
recumbent fold |
le?atá vrása |
A fold overturned to such
an extent that the limbs are essentially horizontal.
|
regional metamorphic rocks
|
regionálni metamorfované
horniny |
Type of metamorphic rocks
formed by the proces of regional metamorphism. |
regional metamorphism |
regionální metamorfóza |
Metamorphism involving
relatively high temperature and pressure which affects
large areas. |
recharge |
|
The addition of new water
to an aquifer or to the zone of saturation. |
residual rocks |
reziduální horniny
|
Remaining part of parent
rock after weathering which was not transported. It is
often fragmented and caving. |
resinous luster |
smolný lesk |
See pitch luster. |
reverse fault |
poesmyk |
A fault in which the
hanging-wall block moved up relative to the footwall
block. |
rhyolite |
ryolit |
A fine-grained, felsic,
volcanic igneous rock made up mostly of feldspar and
quartz. Often with porous and fluidal structure. |
rift valley |
riftové údolí |
A tensional valley bounded
by normal faults. Rift valleys are found at diverging
plate boundaries on continents and along the crest of the
mid-oceanic ridge. |
rigid zone |
|
Upper part of a glacier in
which there is no plastic flow. |
Richter scale |
Richterova stupnice
|
A numerical scale of
earthquake magnitudes. |
ripple marks |
eeoiny |
Small ridges formed on
sediment surfaces exposed to moving wind or water. The
ridges form perpendicularly to the motion. |
rock |
hornina |
Rock is inhomogeneous
mineral association which forms the earth's crust in a
form of many separated units. Every rock is characterized
by structure, texture and mineral coposition reflecting
its origin. |
rock avalanche |
|
A very rapidly moving,
turbulent mass of broken-up bedrock. |
rock forming minerals |
horninotvorne mineraly |
Group of minerals that
form greatest part of rock volume. |
rock strength |
pevnost horniny |
Ability of rock to resist
to surrounding pressure. |
rockfall |
skalní oícení |
Rock falling freely or
bouncing down a cliff. |
rounding |
zaoblení |
The grinding away of sharp
edges and corners of rock fragments during
transportation. |
rupture |
koehká deformace |
Brittle deformation of
rock. |
S-waves |
S-vlny |
A seismic waves propagated
by a shearing motion, which causes rock to vibrate
perpendicular to the direction of wave propagation.
|
sand |
písek |
Sediment composed of
particles with a diameter between 2 mm and 0.06 mm.
|
sand dune |
píseené duny |
A mound of loose sand
grains heaped up by the wind. |
sandstone |
piskovec |
A medium-grained
sedimentary rock (grains between 2 mm and 0.06 mm) formed
by the cementation of sand grains (mainly quartz).
|
saturated zone |
nasycená zóna |
A subsurface zone in which
all rock openings are filled with water. |
scaled shape |
šupinkovity |
Sheet-like mineral shape
(e.g. micas). |
sea-floor spreading |
|
The concept that the ocean
floor is moving away from the mid-oceanic ridge and
across the deep ocean basin, to disappear beneath
continents and island arcs. |
sediment |
nezpevniná usazená
hornina |
Loose, solid particles
that can originate by (1) weathering and erosion of
preexisting rocks, (2) chemical precipitation from
solution, usually in water, and (3) secretion by
organisms. |
sedimentary environment
|
sedimentaení prostoedí
|
Area with specific
conditions for deposition which are approximatelly the
same on every place within the area. |
sedimentary rocks |
zepvniné usazené horniny
|
Rock that has formed from
(1) lithification of any type of sediment, (2)
precipitation from solution |
sedimentation |
sedimentace |
See deposition. |
seismic waves |
seismické vlny |
A wave of energy produced
by an earthquake. |
seismogram |
seismogram |
Paper record of earth
vibration. |
seismograph |
seismograf |
A seismometer with a
recording device that produces a permanent record of
earth motion. |
sericite |
sericit |
Very fine-grained variety
of muscovite. Mineral grains are usually not visible. The
presence of sericite in a rock can be easily identified
by typical silk luster. It is mineral typical for
metamorphic rocks. Properties see micas. |
serpentine |
serpentin |
Mineral typical for
metamorphic rocks. Very dark green to black in colour,
hardness varies from 3 to 5. Luster is dull to greasy,
slight greasy feel. It forms very fine-grained
(macroscopically massive) accumulations. |
serpentinite |
serpentinit |
Type of metamorphic rock
composed mostly of mineral serpentine. It is usually dark
green to green-black in colour, massive and
macroscopically dense. Joints of this rock are usually
filled with chrysotile (asbestos). |
shale |
boidlice |
A fine-grained sedimentary
rock (grains finer than 0.06 mm in diameter) formed by
the cementation of silt and clay (mud). Shale has thin
layers (laminations) and an ability to split (fissility)
into small chips. |
shear force |
|
The component of
gravitational force that is parallel to an inclined
surface. |
shear strength |
smyková pevnost |
The resistance to movement
or deformation of material. |
shear stress |
smykové napití |
Stress due to forces that
tend to cause movement or strain parallel to the
direction of the forces. |
sheet joints |
|
Cracks that develop
parallel to the outer surface of a large mass of
expanding rock, as pressure is released during unloading.
|
shelf |
šelf |
Zone of sea bottom along
all continents with varying width and dip 0.1%. It is
bordered from one side by continental slope and from
other side by continent. |
shock metamorphism |
šoková metamorfóza |
The fastest type of
metamorphism affecting surrounding rocks usually in
tenths of second. |
shrinking |
smrš?ování |
Decreasing of mineral and
rock volumes caused by lowering of moisture. |
schist |
krystalická boidlice
|
A metamorphic rock
characterized by coarse-grained minerals oriented
approximatelly parallel. |
silica |
oxid koemieitý |
A term used for oxygen
plus silicon. |
silicate |
silikáty |
A substance that contains
silica as part of its chemical formula. |
sill |
ložní žíla |
A tabular intrusive
structure concordant with the country rock. |
sillimanite |
silimanit |
Mineral typical for
metamorphic rocks. White, pale green or brown in colour,
hardness varies from 6 to 7. It forms long, slender
crystals, commonly as groups of parallel crystals.
|
silt |
prach |
Sediment composed of
particles with a diameter of 0.002 mm to 0.06 mm. |
siltstone |
prachovec |
A sedimentary rock
consisting mostly of silt grains. |
Silurian |
silur |
Geological period of
Paleozoic between 408 ad 438 mil. of years ago. |
sinkhole |
závrt |
A closed depresion found
on land surfaces underlain by limestone. |
sinter |
sintr |
A deposit of silica that
forms around some hot springs and geysers. |
slate |
boidlice |
A fine-grained rock that
splits easily along flat, parallel planes. |
slide |
sesuv |
In mass wasting, movement
of a descending mass along a plane approximatelly
parallel to the slope of the surface (see landslide).
|
slip |
sesuv |
In mass wasting, movement
of a descending mass along one or more well-defined
surfaces (see landslide). |
slope angle |
úhel sklonu svahu |
Dip angle of a slope. |
slump |
sesuv |
In mass wasting, movement
along a curved surface in which the upper part moves
vertically downward while the lower part moves outward
(see landslide). |
snow line |
snižná eára |
An irregular line making
the highest level to which the winter snow cover on a
glacier is lost during a melt season. |
soil |
(1) puda, (2) zemina
|
(1) A layer of weathered,
unconsolidated material on the top of bedrock; often also
defined as containing organic matter and being capable of
supporting plant growth. (2) Geotechnical term for
sediments, caving residual and volcanoclastic rocks.
|
soil moisture |
vlhkost zeminy |
Term expressing amount of
water in soil by ratio between weight of water in a soil
sample and weight of dry soil sample. |
solifluction |
soliflukce |
Flow of water-saturated
debris over impermeable material. |
sorting |
toídiní |
Process of selection and
separation of sediment grains according to their grain
size (or grain shape or specific gravity). |
specific gravity |
specifická hmotnost
|
The ratio of the mass of
an equal volume of water, determined at a specified
temperature. |
spring |
pramen |
A place where water flows
naturally out of rock onto the land surface. |
stalactite |
stalaktit |
Iciclelike pendant of
dripstone formed on cave ceilings. |
stalagmite |
stalagmit |
Cone-shaped mass of
dripstone formed on cave floors, generally directly below
a stalactite. |
state of crystallization
|
stupen krystalizace |
|
staurolite |
staurolit |
Typical mineral of
metamorphic rocks famous for its twinned crystals that
form into the shape of a cross (or into the shape of the
letter "X"). Shape of a crystals is columnar.
Color is reddish-brown, brown, or black. Hardness is
7-7.5. Luster is vitreous to resinous to dull. Cleavage
poor, in one direction. Fracture is uneven to conchoidal.
|
stock |
peo |
A small discordant pluton
with an outcropping area of less than 100 square
kilometers. |
strain |
deformace |
Change in size (volume) or
shape of a body (or rock unit) in response to stress.
|
streak |
vryp |
Color of pulverized
substance; a useful property for mineral identification.
|
stream gradient |
|
Downhill slope of a
stream's bed or the water surface, if the stream is very
large. |
stream piracy |
|
The natural diversion of
the headwaters of one stream into the channel of another.
|
stream terraces |
oíení terasy |
Steplike landformes found
above a stream and their flood plains. |
stress |
tlak |
A force acting on a body,
or rock unit, that tends to change the size or shape of
that body, or rock unit. Force per unit area within a
body. |
striations |
podélné rýhování
|
(1) On minerals, extremly
straight, parallel lines; (2) Glacial-straight scratches
in rock caused by abrasion by a moving glacier. |
strike |
smir plochy |
The compass direction of a
line formed by the intersection of an inclined plane
(such as a bedding plane) with a horizontal plane.
|
strike-slip fault |
horizontální posun
|
A fault in which movement
is parallel to the strike of the fault surface. |
structural geology |
strukturní geologie |
The branch of geology
concerned with the internal structure of bedrock and the
shapes, arrangement, and interrelationships of rock
units. |
structure |
textura |
Macroscopically
distinguishable arrangement of mineral grains in a rock.
|
subduction zone |
subdukení zóna |
Mostly macroscopically
distinguishable arrangement of mineral grains in a rock.
|
submarine canyon |
podmořský kaňon |
V-shaped valley that run
across the continental shelf and down the continental
slope. |
superposition |
superpozice |
A principle or law stating
that within a sequence of undisturbed sedimentary rocks,
the oldest layers are on the bottom, the youngest on the
top. |
surface waves |
povrchové vlny |
A seismic waves that
travel on the earth's surface. |
swelling |
bobtnání |
Increasing of mineral and
rock volumes caused bz raising of moisture. |
syenite |
syenit |
A plutonic igneous rock
consisting principally of alkali feldspar, usually with
one or more mafic minerals such as hornblende or biotite.
A small amount of plagioclase may be present. Also of
quartz if less than 5%. Quartz-free granite. Name from
Syene (Aswan), where it was later renamed "Aswan red
granite". |
syncline |
synklinála |
A fold in which the
layered rock usually dips toward an axis. |
tabular shape |
tabulkovitý tvar |
Table-like shape of
minerals in a rock (e.g. feldspars). Two of three
crystallographic axes are elongated, one is short.A fold
in which the layered rock usually dips toward an axis.
|
talc |
mastek |
The softest mineral formed
by metamorphic processes. It is the first member of Moh's
scale. |
tectonic forces |
tektonické síly |
Forces generated from
within the earth that result in uplift, movement, or
deformation of part of the earth's crust. |
tension fault |
tahový zlom |
Fault in the earth's crust
created by tensional forces. |
tensional stress |
tahové napití |
A force that tends to
elongate or pull apart a body. |
terminus |
eelo ledovce |
The lower edge of a
glacier. |
terrigenous sediment |
suchozemský sediment |
Land-derived sediment that
has found its way to the sea floor. |
Tertiary |
toetihory |
Older period of Cenozoic
(from 1.6 to 66.4 mil. of years ago). |
texture |
struktura |
Macroscopically and
microscopically distinguishable characteristics (size of
particles, shape of particles, state of crystallization)
of a rock. |
thrust fault |
nasunutí |
A reverse fault in which
the dip of the fault plane is at a low angle to
horizontal. |
till |
till |
Unsorted and unlayered
rock debris carried by a glacier. |
tillite |
tilit |
Lithified till. |
tourmaline |
turmalín |
Black, pink, blue, green
or brown mineral with vitreous luster. Hardness is from 7
to 7.5. It forms slender crystals with triangular
cross-sections and striated sides. |
trachyte |
trachyt |
Felsic volcanic rock
composed mostly of K-feldspars, acidic plagioclases,
biotite and hornblende. |
transform boundary |
transformní rozhraní |
Boundary between two
plates that are sliding past each other. |
translucent |
prusvitný |
Term for a substance which
transmits light, but if you place this substance over an
image on paper you will not see it. |
transparent |
pruhledný |
Term for a substance which
transmits light and if place this substance over an image
on paper you will see it. |
transportation |
poenos (transport) |
The movement of eroded
particles by agents such as rivers, waves, glaciers, or
wind. |
travertine |
travertin |
A porous deposit of
calcite that often precipitates around springs that
contain high amount of CaCO3. |
Triassic |
trias |
The oldest period in
Mesozoic (from 208 to 245 mil. of years ago). |
tsunami |
tsunami |
Huge ocean wave produced
by diplacement of the sea floor; also called seismic sea
wave. |
tuff |
tuf |
A rock formed from
fine-grained pyroclastic particles (ash and dust).
|
turbidity current |
turbiditní proud |
A flowing mass of
sediment-laden water that is heavier than clear water and
therefore flows downslope along the bottom of the sea or
a lake. |
U-shaped valley |
údolí tvaru U |
Characteristic
cross-profile of a valley carved by glacial erosion.
|
ultrabasic rocks |
ultrabazické horniny
|
Type of igneous rocks with
small amount of silica (<44%) composed mostly of basic
plagioclases, pyroxenes and amhiboles. |
ultramafic rocks |
ultramafické horniny
|
Rocks composed entirely or
almost of ferromagnesian minerals (Colour index >90).
|
unconfined aquifer |
volná zvodeo |
A partially filled aquifer
exposed to the land surface and marked by a rising and
falling water table. |
unsaturated zone |
nenasycená zóna |
A subsurface zone in which
rock openings are filled partly with air and partly with
water; above the saturated zone. |
upper mantle |
svrchní pláš? |
One of the inner shells of
the earth. |
valley glacier |
|
A glacier confined to a
valley. The ice flows from a higher to a lower elevation.
|
varve |
varva |
Two thin layers of
sediment, one dark and other light in color, representing
one year's deposition in a lake. |
ventifact |
hranec |
Boulder, cobble, or pebble
with flat surfaces caused by the abrasion of wind-blown
sand. |
viscosity |
viskozita |
Resistance to flow. |
vitreous luster |
skelný lesk |
See glassy luster. |
volcanic ash |
vulkanický popel |
Fine grained material
(<2 mm) composed of rock fragments formed by volcanic
explosion. |
volcanic neck |
|
An intrusive structure
that apparently represents magma that solidified within
the throat of a volcano. It forms isolated hill in
surrounding denudated landscape. |
volcanism |
vulkanismus |
Volcanic activity,
including the eruption of lava and rock fragments and gas
explosions. |
volcano |
sopka |
A hill or mountain
constructed by the extrusion of lava or rock fragments
from a vent. |
volcanoclastic rocks |
vulkanoklastické horniny |
Rock formed by
lithification of rock fragments erupted from a volcano.
Mineral composition is very similar to igneous rocks,
structures and textures are similar to clastic
sedimentary rocks. |
water table |
hladina podzemní vody
|
The upper surface of the
zone of saturation. |
weak zone |
oslabená zóna |
Zone in rock massif where
rock properties are significantly worse then in
surrounding rock. |
weathering |
zvitrávání |
The group of processes
that change rock at near the earth's surface. |
well |
studna, sonda, vrt |
A hole, generally
cylindrical and usually walled or lined with pipe, that
is dug or drilled into the ground to penetrate an aquifer
below the zone of saturation. |
wind ripples |
|
Small, low ridges of sand
produced by the saltation of windblown sand. |
xenolith |
xenolit |
Fragment of rock distinct
from the igneous rock in which it is enclosed. |
zone of accumulation |
zóna akumulace |
That portion of a glacier
with a perennial snow cover. |
zone of aeration |
provzdušnilá zóna
|
See unsaturated zone. |
zone of leaching |
zóna vyluhování |
Top layer of soil
characterized by downward movement of water which leaches
some mineral components. |
zone of plastic flow |
zóna plastického teeení |
Lower zone of a glacier
where plasticity limit of ice is exceeded. |
zone of wastage |
zóna tání |
That portion of a glacier
in which ice is lost or wasted. |