This document provides information on 20 different minerals. For each mineral, it gives the mineral name, key physical properties such as hardness, crystal structure, cleavage, color, and identifying characteristics. Pictures or diagrams are also provided to illustrate some mineral characteristics. The minerals discussed include common rock-forming silicates as well as oxides, sulfides, carbonates, halides, and sulfates. Key identification tests involving hardness tests, streak tests, cleavage, crystal habit, and other properties are summarized for each mineral.
This rare photo shows a sunset at the North Pole with the moon appearing close to the earth, which was taken on March 13, 2011. It features both the sun and moon visible at the same time, with the sun below the moon, which is a scene that is unlikely to be witnessed in person and shows the beauty of nature at the North Pole.
The document discusses oxygen isotopes and how they can be used to study climate change during the Carboniferous Period. Oxygen isotopes are recorded in the calcite shells of microorganisms and preserved in limestone. Heavier oxygen isotopes are concentrated in the shells of microorganisms and limestone during glacial periods due to fractionation processes. Analyzing the ratio of oxygen isotopes over time in limestone reveals alternating warm and cold periods during the Carboniferous, dominated by the Carboniferous Ice Age when vast ice sheets covered the southern polar continents.
Fluorite is shown in the figure, displaying excellent four-directional octahedral cleavage as its crystal structure allows cleavage planes to form easily in four perpendicular directions, resulting in octahedral shapes when it breaks along these planes.
Alférez José Marìa Sobral, expedición del Antartic, expediciòn de Otto Norden...Martin Alberto Belaustegui
La Unión Europea ha acordado un paquete de sanciones contra Rusia por su invasión de Ucrania. Las sanciones incluyen restricciones a las importaciones de productos rusos de alta tecnología y a las exportaciones de bienes de lujo a Rusia. Además, se congelarán los activos de varios oligarcas rusos y se prohibirá el acceso de los bancos rusos a los mercados financieros de la UE.
The document discusses the benefits of exercise for mental health. Regular physical activity can help reduce anxiety and depression and improve mood and cognitive functioning. Exercise causes chemical changes in the brain that may help protect against mental illness and improve symptoms.
This document provides information on 20 different minerals. For each mineral, it gives the mineral name, key physical properties such as hardness, crystal structure, cleavage, color, and identifying characteristics. Pictures or diagrams are also provided to illustrate some mineral characteristics. The minerals discussed include common rock-forming silicates as well as oxides, sulfides, carbonates, halides, and sulfates. Key identification tests involving hardness tests, streak tests, cleavage, crystal habit, and other properties are summarized for each mineral.
This rare photo shows a sunset at the North Pole with the moon appearing close to the earth, which was taken on March 13, 2011. It features both the sun and moon visible at the same time, with the sun below the moon, which is a scene that is unlikely to be witnessed in person and shows the beauty of nature at the North Pole.
The document discusses oxygen isotopes and how they can be used to study climate change during the Carboniferous Period. Oxygen isotopes are recorded in the calcite shells of microorganisms and preserved in limestone. Heavier oxygen isotopes are concentrated in the shells of microorganisms and limestone during glacial periods due to fractionation processes. Analyzing the ratio of oxygen isotopes over time in limestone reveals alternating warm and cold periods during the Carboniferous, dominated by the Carboniferous Ice Age when vast ice sheets covered the southern polar continents.
Fluorite is shown in the figure, displaying excellent four-directional octahedral cleavage as its crystal structure allows cleavage planes to form easily in four perpendicular directions, resulting in octahedral shapes when it breaks along these planes.
Alférez José Marìa Sobral, expedición del Antartic, expediciòn de Otto Norden...Martin Alberto Belaustegui
La Unión Europea ha acordado un paquete de sanciones contra Rusia por su invasión de Ucrania. Las sanciones incluyen restricciones a las importaciones de productos rusos de alta tecnología y a las exportaciones de bienes de lujo a Rusia. Además, se congelarán los activos de varios oligarcas rusos y se prohibirá el acceso de los bancos rusos a los mercados financieros de la UE.
The document discusses the benefits of exercise for mental health. Regular physical activity can help reduce anxiety and depression and improve mood and cognitive functioning. Exercise causes chemical changes in the brain that may help protect against mental illness and improve symptoms.
The document discusses the myth of the World Turtle and how it has been interpreted by scholars as referring to beliefs about a flat Earth. However, the author argues that many ancient myths were actually describing cosmological events and features of the Milky Way galaxy, not the Earth. The Turtle myth symbolized the bulge at the center of the Milky Way. When European scholars interpreted the myths literally as stories about Earth, they misunderstood the original symbolic and cosmological meaning. The author analyzes myths from various cultures and finds similarities between them that reflect cosmological truths about the formation of the galaxy and solar system.
The document discusses basic geographic vocabulary including meridians, parallels, the equator, tropics of cancer and capricorn, polar circles, latitude, longitude, and grid referencing systems like MMRB that are used to locate positions on Earth. Key lines include the meridian of Greenwich used as the prime meridian and reference for longitude measurements globally as well as the equator and tropics that divide the planet into climatic regions.
This document provides Spanish translations for common quantity words in English, including: many (muchos-as), too many (demasiados), a lot of (un montón de), some (algunos-as, un poco de), few (pocos-as), much (mucho-a), too much (demasiado-a), and little (poco-a). Examples are given to illustrate using each quantity word in a sentence both in English and Spanish.
The document proposes that from the perspective of an observer traveling at the speed of light, the Earth would appear flat rather than round. It argues that relativity suggests curvature is a function of time, and for a relativistic observer with no experienced passage of time, the Earth's curvature would be zero. The document also suggests that in 4 dimensions, the Earth could be conceptualized as a flat object that appears curved in 3 dimensions. Overall, the document puts forth a novel theory that relativistic effects could make the Earth appear flat rather than round to certain observers.
This document discusses sedimentary structures classified into physical and bio-genic structures. Physical structures are formed by physical processes without organisms and include primary structures like plane bedding, ripples and dunes formed by currents. Bio-genic structures result from bioturbation by organisms altering sediments. Sedimentary structures record depositional processes and can indicate paleocurrents, paleoslopes and paleogeography. They are important for interpreting geological history, sedimentary processes and finding petroleum resources.
The document discusses various types of sedimentary structures classified based on their formation process. Primary structures form during deposition without external forces, while secondary structures form after deposition due to forces. Examples of primary structures include ripple marks, cross-bedding and flaser bedding. Secondary structures include sole marks, tool marks and groove marks formed by erosion. Chemical structures also form via processes like dissolution and precipitation. Sedimentary structures provide clues about depositional environments and sediment transport directions.
This document provides guidance on mapping geological structures and features from maps. It includes explanations of key map elements like the map key, scale, and north arrow. It also defines and provides examples of important geological structures like folds, faults, intrusions, and unconformities. The document seeks to help readers interpret maps by describing these features, explaining how to identify and describe them, and posing questions about the geological history that can be answered from the map evidence.
Sedimentary structures provide important information about the depositional environment and post-depositional changes to sedimentary rocks. Key structures discussed include beds and bedding planes, laminations, graded bedding indicating changes in grain size over time, cross-bedding reflecting currents, load casts and flame structures from density differences, sole structures on bed bases indicating erosion, and trace fossils providing evidence of organism behavior and helping determine correct bed orientations. Together, an understanding of these sedimentary structures allows reconstruction of the depositional environment and testing of the law of superposition.
This document discusses various primary sedimentary structures that form as a result of mechanical processes during sediment deposition. It describes bedforms such as ripples and dunes that form under different flow regimes. It also discusses cross-bedding and other structures including graded bedding, soft-sediment deformation, and bedding-plane markings. Various sedimentary environments and the structures associated with them are outlined, such as turbidites and hummocky cross-stratification.
The document claims that the Earth is flat rather than spherical, and that magnetic fields on Earth form a spherical spiral structure generated by 64 tetrahedrons at the center. It also describes 13 magnetic shields of different frequencies or dimensions that provide layers of love, truth, and other qualities starting from the center of Earth outward.
The document discusses the benefits of exercise for mental health. Regular physical activity can help reduce anxiety and depression and improve mood and cognitive functioning. Exercise causes chemical changes in the brain that may help protect against mental illness and improve symptoms.
Code of Ethics for Professional Teachers of the PhilippinesJohn Bernal
This powerpoint presentation contains salient features of Code of Ethics for Professional Teachers of the Philippines citing Supreme Court Jurisprudence related to education.
The document summarizes Freud's psychosexual stages of development and other theories of human development. It discusses Freud's theory that personality develops through oral, anal, phallic, latent, and genital stages, where the libido or pleasure principle is focused on different erogenous zones. It also briefly mentions Erikson's psychosocial theory, learning theories, Piaget's cognitive development theory, Jung, and Maslow among the major theories of human development.
The document provides information on measuring dinosaur footprints and trackways to determine characteristics of dinosaurs such as speed and size. It discusses measuring footprint length and stride length to calculate hip height, total length, and whether the dinosaur was walking, trotting, or running. Examples are given for various dinosaurs such as Velociraptor, Ultrasaurus, and Gallimimus. Formulas are presented for calculating hip height, relative stride length, dimensionless speed, and actual speed based on footprint and stride length measurements.
This document discusses dinosaurs, including their diversity and characteristics. It notes that there were over 500 dinosaur genera and around 1,000 species. Herbivorous dinosaurs tended to have large bodies, neck and tail variations suited for different diets, and gastroliths or stomach stones. Carnivorous dinosaurs were often bipedal, had forward-facing eyes and sharp teeth and claws for hunting, and may have hunted in packs. Specific dinosaurs discussed include Spinosaurus, Stegosaurus, and Argentinosaurus, which was one of the largest at over 30 meters long.
This document discusses the construction and analysis of hydrographs. Hydrographs show changes in river discharge over time, especially during storm events. They are constructed by plotting river discharge levels against time to analyze flooding patterns. Key aspects of hydrographs include the rising limb as flood waters increase, the peak flow, recession limb as waters recede, and basin lag time between peak rainfall and peak river flow. Analyzing hydrographs can help predict flooding and inform flood prevention. Many factors influence hydrograph shape, such as area, slope, soil, land use, and precipitation patterns.
The document provides information about the hydrological cycle including key definitions and processes. It explains that precipitation is an input into the cycle, while evaporation and transpiration are outputs. It also describes several transfer processes by which water moves through the cycle, such as surface runoff, infiltration, percolation, groundwater flow, and river discharge.
This document lists several types of extinct marine organisms: bivalves, brachiopods, graptolites, and ammonites. Bivalves and brachiopods are shelled organisms, while graptolites and ammonites are shelled cephalopods that were important members of Paleozoic and Mesozoic seas.
This document describes various landforms created by glacial erosion and deposition. It defines cirques, corries, and cwms as hollows on mountainsides deepened and widened by corrie glaciers. Arêtes are knife-edged ridges between corries, while pyramidal peaks form when multiple corries erode a central horn-shaped area. Glacial troughs or U-shaped valleys have hanging valleys, truncated spurs, and misfit streams. Features of glacial deposition include till, moraines, drumlins, eskers, kames, kettles, and outwash plains.
Peter Knight photographed various glaciers around the world including niche glaciers in Wyoming that are sensitive to climate change, the ice cap on Cotopaxi volcano in Ecuador which extends further on the windward side due to higher snowfall, and valley, mountain, and ice sheet glaciers in locations such as Alaska, Greenland, and New Zealand. The photos show glacial landforms and features including moraines, crevasses, ice caves, supraglacial streams, ice cliffs, striations, and erratics.
The document discusses different types of glacial ice formations including glaciers, ice caps, ice sheets, and niche ice. It provides examples of each type through photographs of glaciers in locations like Wyoming, Ecuador, Alaska, and New Zealand. The text also examines glacial landforms created by erosion and deposition as glaciers advance and retreat, such as moraines, eskers, drumlins, and outwash plains.
The document discusses the myth of the World Turtle and how it has been interpreted by scholars as referring to beliefs about a flat Earth. However, the author argues that many ancient myths were actually describing cosmological events and features of the Milky Way galaxy, not the Earth. The Turtle myth symbolized the bulge at the center of the Milky Way. When European scholars interpreted the myths literally as stories about Earth, they misunderstood the original symbolic and cosmological meaning. The author analyzes myths from various cultures and finds similarities between them that reflect cosmological truths about the formation of the galaxy and solar system.
The document discusses basic geographic vocabulary including meridians, parallels, the equator, tropics of cancer and capricorn, polar circles, latitude, longitude, and grid referencing systems like MMRB that are used to locate positions on Earth. Key lines include the meridian of Greenwich used as the prime meridian and reference for longitude measurements globally as well as the equator and tropics that divide the planet into climatic regions.
This document provides Spanish translations for common quantity words in English, including: many (muchos-as), too many (demasiados), a lot of (un montón de), some (algunos-as, un poco de), few (pocos-as), much (mucho-a), too much (demasiado-a), and little (poco-a). Examples are given to illustrate using each quantity word in a sentence both in English and Spanish.
The document proposes that from the perspective of an observer traveling at the speed of light, the Earth would appear flat rather than round. It argues that relativity suggests curvature is a function of time, and for a relativistic observer with no experienced passage of time, the Earth's curvature would be zero. The document also suggests that in 4 dimensions, the Earth could be conceptualized as a flat object that appears curved in 3 dimensions. Overall, the document puts forth a novel theory that relativistic effects could make the Earth appear flat rather than round to certain observers.
This document discusses sedimentary structures classified into physical and bio-genic structures. Physical structures are formed by physical processes without organisms and include primary structures like plane bedding, ripples and dunes formed by currents. Bio-genic structures result from bioturbation by organisms altering sediments. Sedimentary structures record depositional processes and can indicate paleocurrents, paleoslopes and paleogeography. They are important for interpreting geological history, sedimentary processes and finding petroleum resources.
The document discusses various types of sedimentary structures classified based on their formation process. Primary structures form during deposition without external forces, while secondary structures form after deposition due to forces. Examples of primary structures include ripple marks, cross-bedding and flaser bedding. Secondary structures include sole marks, tool marks and groove marks formed by erosion. Chemical structures also form via processes like dissolution and precipitation. Sedimentary structures provide clues about depositional environments and sediment transport directions.
This document provides guidance on mapping geological structures and features from maps. It includes explanations of key map elements like the map key, scale, and north arrow. It also defines and provides examples of important geological structures like folds, faults, intrusions, and unconformities. The document seeks to help readers interpret maps by describing these features, explaining how to identify and describe them, and posing questions about the geological history that can be answered from the map evidence.
Sedimentary structures provide important information about the depositional environment and post-depositional changes to sedimentary rocks. Key structures discussed include beds and bedding planes, laminations, graded bedding indicating changes in grain size over time, cross-bedding reflecting currents, load casts and flame structures from density differences, sole structures on bed bases indicating erosion, and trace fossils providing evidence of organism behavior and helping determine correct bed orientations. Together, an understanding of these sedimentary structures allows reconstruction of the depositional environment and testing of the law of superposition.
This document discusses various primary sedimentary structures that form as a result of mechanical processes during sediment deposition. It describes bedforms such as ripples and dunes that form under different flow regimes. It also discusses cross-bedding and other structures including graded bedding, soft-sediment deformation, and bedding-plane markings. Various sedimentary environments and the structures associated with them are outlined, such as turbidites and hummocky cross-stratification.
The document claims that the Earth is flat rather than spherical, and that magnetic fields on Earth form a spherical spiral structure generated by 64 tetrahedrons at the center. It also describes 13 magnetic shields of different frequencies or dimensions that provide layers of love, truth, and other qualities starting from the center of Earth outward.
The document discusses the benefits of exercise for mental health. Regular physical activity can help reduce anxiety and depression and improve mood and cognitive functioning. Exercise causes chemical changes in the brain that may help protect against mental illness and improve symptoms.
Code of Ethics for Professional Teachers of the PhilippinesJohn Bernal
This powerpoint presentation contains salient features of Code of Ethics for Professional Teachers of the Philippines citing Supreme Court Jurisprudence related to education.
The document summarizes Freud's psychosexual stages of development and other theories of human development. It discusses Freud's theory that personality develops through oral, anal, phallic, latent, and genital stages, where the libido or pleasure principle is focused on different erogenous zones. It also briefly mentions Erikson's psychosocial theory, learning theories, Piaget's cognitive development theory, Jung, and Maslow among the major theories of human development.
The document provides information on measuring dinosaur footprints and trackways to determine characteristics of dinosaurs such as speed and size. It discusses measuring footprint length and stride length to calculate hip height, total length, and whether the dinosaur was walking, trotting, or running. Examples are given for various dinosaurs such as Velociraptor, Ultrasaurus, and Gallimimus. Formulas are presented for calculating hip height, relative stride length, dimensionless speed, and actual speed based on footprint and stride length measurements.
This document discusses dinosaurs, including their diversity and characteristics. It notes that there were over 500 dinosaur genera and around 1,000 species. Herbivorous dinosaurs tended to have large bodies, neck and tail variations suited for different diets, and gastroliths or stomach stones. Carnivorous dinosaurs were often bipedal, had forward-facing eyes and sharp teeth and claws for hunting, and may have hunted in packs. Specific dinosaurs discussed include Spinosaurus, Stegosaurus, and Argentinosaurus, which was one of the largest at over 30 meters long.
This document discusses the construction and analysis of hydrographs. Hydrographs show changes in river discharge over time, especially during storm events. They are constructed by plotting river discharge levels against time to analyze flooding patterns. Key aspects of hydrographs include the rising limb as flood waters increase, the peak flow, recession limb as waters recede, and basin lag time between peak rainfall and peak river flow. Analyzing hydrographs can help predict flooding and inform flood prevention. Many factors influence hydrograph shape, such as area, slope, soil, land use, and precipitation patterns.
The document provides information about the hydrological cycle including key definitions and processes. It explains that precipitation is an input into the cycle, while evaporation and transpiration are outputs. It also describes several transfer processes by which water moves through the cycle, such as surface runoff, infiltration, percolation, groundwater flow, and river discharge.
This document lists several types of extinct marine organisms: bivalves, brachiopods, graptolites, and ammonites. Bivalves and brachiopods are shelled organisms, while graptolites and ammonites are shelled cephalopods that were important members of Paleozoic and Mesozoic seas.
This document describes various landforms created by glacial erosion and deposition. It defines cirques, corries, and cwms as hollows on mountainsides deepened and widened by corrie glaciers. Arêtes are knife-edged ridges between corries, while pyramidal peaks form when multiple corries erode a central horn-shaped area. Glacial troughs or U-shaped valleys have hanging valleys, truncated spurs, and misfit streams. Features of glacial deposition include till, moraines, drumlins, eskers, kames, kettles, and outwash plains.
Peter Knight photographed various glaciers around the world including niche glaciers in Wyoming that are sensitive to climate change, the ice cap on Cotopaxi volcano in Ecuador which extends further on the windward side due to higher snowfall, and valley, mountain, and ice sheet glaciers in locations such as Alaska, Greenland, and New Zealand. The photos show glacial landforms and features including moraines, crevasses, ice caves, supraglacial streams, ice cliffs, striations, and erratics.
The document discusses different types of glacial ice formations including glaciers, ice caps, ice sheets, and niche ice. It provides examples of each type through photographs of glaciers in locations like Wyoming, Ecuador, Alaska, and New Zealand. The text also examines glacial landforms created by erosion and deposition as glaciers advance and retreat, such as moraines, eskers, drumlins, and outwash plains.
Organic chemical sedimentary_rockssmallangelabentley
This document provides information on different types of sedimentary rocks formed through organic, chemical, and evaporative processes. Organic rocks like chalk are composed of microscopic shells and form limestones. Chemical rocks like oolitic limestone form through precipitation and contain spherical grains. Evaporite rocks like halite form through evaporation in arid climates and include common minerals like gypsum and rock salt. Each rock type is described in terms of its composition, texture, and environmental conditions of formation.
Sedimentary structures provide important information about depositional environments and allow the orientation of sedimentary beds to be determined. Key structures discussed include beds and bedding planes, laminations, graded bedding indicating changes in grain size over time, cross-bedding showing current direction, sole structures like flute casts formed by erosion on sediment surfaces, and trace fossils providing evidence of organism behavior and helping determine the correct vertical orientation of strata. Together, an understanding of these sedimentary structures is essential for interpreting the depositional history preserved in sedimentary rocks.
Metamorphism is the change in form of pre-existing rocks due to heat, pressure, or both. Contact metamorphism involves changes from heat alone near igneous intrusions, forming rocks like marble, quartzite, and hornfels. Regional metamorphism over large areas is caused by heat and pressure, producing foliated rocks like slate, schist, and gneiss from sediments. Dynamic metamorphism involves crushing along fault planes to form breccias and mylonites. Grade of metamorphism depends on conditions and mineral growth.
This document provides an introduction to metamorphism, including definitions, causes, limits, types, effects, and characteristics. Metamorphism is the change in form of pre-existing rocks due to increases in temperature, pressure, or both. The main types of metamorphism are contact/thermal, dynamic, and regional. Metamorphism results in recrystallization and realignment of minerals without melting, changing the rock's appearance, properties, and grade of alteration. Argillaceous sediments are most susceptible to metamorphic changes.
Lava cools and solidifies in different ways depending on factors like thickness, rate of cooling, and whether it erupts on land or underwater. This results in a variety of igneous rock textures like pillow lava formed under water, glassy texture from instant cooling, rope-like pahoehoe or jagged aa textures on land, and vesicles or mineral deposits within the rock. Thick lava flows exhibit columnar jointing as they slowly cool from the outside in, forming hexagonal or pentagonal columns.
Igneous rocks form from the cooling and solidification of magma or lava. There are two main types - extrusive rocks which cool at the surface and intrusive rocks which cool underground. Crystal size depends on the cooling rate, with rapid surface cooling producing microscopic crystals and slow underground cooling producing larger crystals. Texture and mineral composition further classify igneous rocks into categories like rhyolite, granite, gabbro and basalt. Pyroclastic rocks form from explosive eruptions and include tuffs, agglomerates and volcanic bombs.
Graphic logs are a method used by geologists to record sedimentary rock layers and structures to scale using symbols. The vertical scale shows bed thickness proportionally, while the horizontal scale maps particle sizes. A variety of symbols indicate features like graded bedding, cross-bedding, ripples, and erosion surfaces. Example graphic logs depict typical sequences in glacial, river, desert, and delta depositional environments. Questions on exams may involve interpreting sedimentary histories from graphic logs.
Graphic logs are a method used by geologists to record sedimentary rock layers and structures to scale using symbols. The vertical scale shows bed thickness proportionally, while the horizontal scale maps particle sizes. A variety of symbols indicate features like graded bedding, cross-bedding, ripples, and erosion surfaces. Example graphic logs depict typical sequences in glacial, river, desert, and delta depositional environments. Questions on exams may involve interpreting sedimentary histories from graphic logs.
This document provides information on clastic/detrital sedimentary rocks, including their characteristics, classification, particle sizes, rock groups, terminology, and examples. It describes the key properties of sedimentary rocks formed from eroded fragments such as conglomerate, breccia, sandstone, siltstone, mudstone, shale, and discusses the environments in which they form.
This document discusses classifying igneous rocks based on their texture, grain size, color, density, and chemical composition. Igneous rocks can be classified as volcanic, hypabyssal, or plutonic based on grain size, and further classified as ultramafic, mafic, intermediate, or acid based on their chemistry and mineral content, with darker, denser rocks generally being richer in ferromagnesian minerals and lighter rocks richer in quartz and feldspar.
The document discusses whether dinosaurs were warm-blooded or cold-blooded. While there is no conclusive evidence, dinosaurs likely evolved endothermy or warm-bloodedness at some point in their history, as modern birds are their descendants. Evidence presented includes bone structure and histology, dinosaur behavior like fast running, predator to prey ratios, and the existence of Arctic dinosaurs, but the available evidence remains speculative overall.