HISTORIA DE LA ESTADÍSTICA EN LA ANTIGUEDAD
Fechas importantes y descripción de estas fechas con los hechos y desarrollo que se presento en cada una de ellas.
El paradigma interpretativo o hermenéutico de la investigación se construye como una respuesta a las insuficiencias heurísticas de la investigación positivista o cientificista en la comprensión de la complejidad de los problemas sociales.
PROPUESTA DE LINEAMIENTOS PARA LA FORMACIÓN POR COMPETENCIAS EN EDUCACIÓN SUPERIOR
Desde el año 2008 el Ministerio de Educación Nacional ha emprendido acciones tendientes a la formulación de competencias genéricas, o transversales a todos los núcleos de formación en educación superior, que posibiliten un monitoreo de la calidad de la educación superior en el país y que puedan constituirse en el elemento articulador de todos los niveles educativos: inicial, básica, media y superior.
FUNDAMENTOS
1. Competencias abstractas del pensamiento: Razonamiento crítico, entendimiento interpersonal, pensamiento creativo, razonamiento analítico y solución de problemas
2. Conocimientos y competencias prácticas necesarias para el despliegue de las competencias abstractas: Conocimiento del entorno, comunicación, trabajo en equipo, alfabetización cuantitativa, manejo de información, comunicación en inglés y TICs.
3. Dinamizadores para el desarrollo de las competencias genéricas: Saber aprender y recontextualizar.
This presentation will help students to know about the basic concept and understanding about the rivers that What is river? What is the flow of river? What are the types of river or its drainage pattern? Rivers Erosional and Depositional Landforms.
Geological action of river or Fluvial processes
The geological action of river is divided chiefly into three parts as Erosion, Transportation and Deposition.
Erosion: River erosion is mainly due to mechanical breaking down of rock fragment. The chemical action of
rivers is minimal. A wide variety of processes are involved in river erosion as follows;
a. Hydraulic action: It is the process of mechanical loosening or removal of the material by the action of the water
alone. The effectiveness of hydraulic action of a river is depends on gradient, velocity of the stream, width, depth
and shape of the channel and discharge.
b. Abrasion: The process of wearing-away of bed rock surfaces by mechanical processes such as rubbing, cutting,
scratching, grinding and polishing etc. is known as abrasion.
c. Attrition: The process of mechanical wearing and tearing of the transported rock fragments into smaller fragments
due to mutual impact and collision.
d. Cavitation: Highly turbulent rivers in rocky channels erode their beds by hydraulic plucking, in which pieces of
bed rocks are lifted out by strong eddies spiraling up around vertical axes. This sucking out of the rock pieces
produces cavities or depressions within the rock. This type of process is called cavitation.
e. Corrosion: The chemical processes of rock erosion by river water are known as corrosion or solution.
Important erosional features:
a. Potholes: These are cylindrical or bowl-like depressions in the rocky beds of streams, which are excavated in the
floors of the streams by extensive, localized abrasion. These are commonly found in softer bedrocks.
b. Water fall: These are defined as magnificent jumps made by stream or river water at certain specific parts of their
course where there is a sudden and considerable drop in the gradient of the channel.
c. River valleys: The river channel carved out by the flow of running water is commonly known as a river valley.
d. Gorges or canyons: During the river erosion, down cutting of its cannel gives rise to a deep narrow valley with
vertical or steep walls. Such a valley is termed as a gorge or canyons.
e. Escarpments: These are erosional land forms produces by rivers in regions composed of alternating beds of hard
and soft rocks. During river erosion soft rocks erode much faster than hard rocks, leaving behind steep slopes on
one side and a gentle slope on the other. The steep slope side is known as the escarpment.
Hog’s back: This is a sharp ridge like structure with high angle sides on two sides formed by harder rocks in an
inclined series of beds.
Mesa and butte: In regions of horizontal strata in which isolated portions of land is capped by a hard, erosion-
resistant bed, the erosional landforms produced will have an isolated flat-topped land area with seep sides,
commonly known as mesa. Isolated masses without flat tops are called buttes.
Transportation: A river is a most powerful agent of transportation. All the material being transported by a
GEOGRAPHY YEAR 10: RIVER LANDFORMS. Contains: river landforms, across the rivers, v-shapped valleys, waterfalls, formation of the waterfalls, meanders and ox-bow lakes, braiding and deltas, the formation of a delta.
WRI’s brand new “Food Service Playbook for Promoting Sustainable Food Choices” gives food service operators the very latest strategies for creating dining environments that empower consumers to choose sustainable, plant-rich dishes. This research builds off our first guide for food service, now with industry experience and insights from nearly 350 academic trials.
Top 8 Strategies for Effective Sustainable Waste Management.pdfJhon Wick
Discover top strategies for effective sustainable waste management, including product removal and product destruction. Learn how to reduce, reuse, recycle, compost, implement waste segregation, and explore innovative technologies for a greener future.
"Understanding the Carbon Cycle: Processes, Human Impacts, and Strategies for...MMariSelvam4
The carbon cycle is a critical component of Earth's environmental system, governing the movement and transformation of carbon through various reservoirs, including the atmosphere, oceans, soil, and living organisms. This complex cycle involves several key processes such as photosynthesis, respiration, decomposition, and carbon sequestration, each contributing to the regulation of carbon levels on the planet.
Human activities, particularly fossil fuel combustion and deforestation, have significantly altered the natural carbon cycle, leading to increased atmospheric carbon dioxide concentrations and driving climate change. Understanding the intricacies of the carbon cycle is essential for assessing the impacts of these changes and developing effective mitigation strategies.
By studying the carbon cycle, scientists can identify carbon sources and sinks, measure carbon fluxes, and predict future trends. This knowledge is crucial for crafting policies aimed at reducing carbon emissions, enhancing carbon storage, and promoting sustainable practices. The carbon cycle's interplay with climate systems, ecosystems, and human activities underscores its importance in maintaining a stable and healthy planet.
In-depth exploration of the carbon cycle reveals the delicate balance required to sustain life and the urgent need to address anthropogenic influences. Through research, education, and policy, we can work towards restoring equilibrium in the carbon cycle and ensuring a sustainable future for generations to come.
Altered Terrain: Colonial Encroachment and Environmental Changes in Cachar, A...PriyankaKilaniya
The beginning of colonial policy in the area was signaled by the British annexation of the Cachar district in southern Assam in 1832. The region became an alluring investment opportunity for Europeans after British rule over Cachar, especially after the accidental discovery of wild tea in 1855. Within this historical context, this study explores three major stages that characterize the evolution of nature. First, it examines the distribution and growth of tea plantations, examining their size and rate of expansion. The second aspect of the study examines the consequences of land concessions, which led to the initial loss of native forests. Finally, the study investigates the increased strain on forests caused by migrant workers' demands. It also highlights the crucial role that the Forest Department plays in protecting these natural habitats from the invasion of tea planters. This study aims to analyze the intricate relationship between colonialism and the altered landscape of Cachar, Assam, by means of a thorough investigation, shedding light on the environmental, economic, and societal aspects of this historical transformation.
Climate Change All over the World .pptxsairaanwer024
Climate change refers to significant and lasting changes in the average weather patterns over periods ranging from decades to millions of years. It encompasses both global warming driven by human emissions of greenhouse gases and the resulting large-scale shifts in weather patterns. While climate change is a natural phenomenon, human activities, particularly since the Industrial Revolution, have accelerated its pace and intensity
Artificial Reefs by Kuddle Life Foundation - May 2024punit537210
Situated in Pondicherry, India, Kuddle Life Foundation is a charitable, non-profit and non-governmental organization (NGO) dedicated to improving the living standards of coastal communities and simultaneously placing a strong emphasis on the protection of marine ecosystems.
One of the key areas we work in is Artificial Reefs. This presentation captures our journey so far and our learnings. We hope you get as excited about marine conservation and artificial reefs as we are.
Please visit our website: https://kuddlelife.org
Our Instagram channel:
@kuddlelifefoundation
Our Linkedin Page:
https://www.linkedin.com/company/kuddlelifefoundation/
and write to us if you have any questions:
info@kuddlelife.org
Presented by The Global Peatlands Assessment: Mapping, Policy, and Action at GLF Peatlands 2024 - The Global Peatlands Assessment: Mapping, Policy, and Action
UNDERSTANDING WHAT GREEN WASHING IS!.pdfJulietMogola
Many companies today use green washing to lure the public into thinking they are conserving the environment but in real sense they are doing more harm. There have been such several cases from very big companies here in Kenya and also globally. This ranges from various sectors from manufacturing and goes to consumer products. Educating people on greenwashing will enable people to make better choices based on their analysis and not on what they see on marketing sites.
Epcon is One of the World's leading Manufacturing Companies.EpconLP
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Characterization and the Kinetics of drying at the drying oven and with micro...Open Access Research Paper
The objective of this work is to contribute to valorization de Nephelium lappaceum by the characterization of kinetics of drying of seeds of Nephelium lappaceum. The seeds were dehydrated until a constant mass respectively in a drying oven and a microwawe oven. The temperatures and the powers of drying are respectively: 50, 60 and 70°C and 140, 280 and 420 W. The results show that the curves of drying of seeds of Nephelium lappaceum do not present a phase of constant kinetics. The coefficients of diffusion vary between 2.09.10-8 to 2.98. 10-8m-2/s in the interval of 50°C at 70°C and between 4.83×10-07 at 9.04×10-07 m-8/s for the powers going of 140 W with 420 W the relation between Arrhenius and a value of energy of activation of 16.49 kJ. mol-1 expressed the effect of the temperature on effective diffusivity.
2. Discussion about the course of river
The general terminologies regarding river
Erosion and its result on the shape of river
The detail insight of the river pattern and its
final destination
Summary of the entire presentation
Question/Answer session
3. A river is a natural watercourse, usually
freshwater, flowing towards an ocean, lake,
sea or another river
Rivers can flow down mountains,
through valleys or along plains, and can
create canyons or gorges.
4. Source of river
Body of river
Confluence
Mouth of river
7. Origination from a mountain lake or a glacier
V-shaped valley
Water fall
Hydraulic action
Aberration
Attrition
Cascade
Interlocking spurs
Potholes
8.
9.
10.
11. The force of the water weakens and breaks up the
rocks
ABRASION, The material carried in the river wears
away the river bed
ATTRITION, As the pebbles carried by the river
crash into each other, they become smaller and
rounder
SOLUTION, The water in the river dissolves the
minerals in the rocks
12. Rolling stones along the river bed.(
needs lots of energy)
Traction Suspension
Clay sized particles are carried
along by the river flow
Saltation
Sand sized particles
bounce along the riverbed
Solution
Some minerals are dissolved
by the riverwater
river flow
13. Formation Of A Waterfall
Soft rock
Hard rock
Steep sides
( gorge )
Vertical erosion
Forms plunge pool
Undercutting
erodes the
softer rock
forming an overhang
The overhang
Eventually
collapses
The process
starts again
Eroded rock
Waterfall
Retreats upstream
16. MENDERS, Rivers snaking across and is
called mendering river or mender
Ox-bow lake, Cut of region of a river is
called ox-bow lake
FLOODED PLAINS, The area around a river
that is usually used for irrigation
CONFLUENCE, The point where the
tributary joins the river
20. LEVEES, Is the natural or artificial banking
of a river to prevent out flow or river usually
due to erosion on bed
DEPOSITION, The eroded material is
steadily washed into the ocean
MOUTH, The area where the river meets the
sea
21. DELTA, Is the area where the river splits into
a few portions and make a Δ shape
ESTUARY, An estuary is a partly enclosed
coastal body of brackish water with one or
more rivers or streams flowing into it, and
with a free connection to the open sea.
22. SWAMP, An area of low-lying, uncultivated
ground where water collects; a bog or marsh.
MANGROVE, A tree or shrub that grows in chiefly
tropical coastal swamps that are flooded at high
tide. Mangroves typically have numerous tangled
roots above ground and form dense thickets.
23. Characteristics Upper Course Middle Course Lower Course
Slope
Width
Depth
Straightness
Load
Main work
Valley width
Type of load
usually steep
narrow
shallow
winding
little
large/small
angular
erosion
transportation
steeper
wider
deeper
meandering
some
medium/small
rounded
Transportation
narrow
gentle
quite wide
wide
deep
big meanders
lots
small+
rounded
transportation
deposition
wide