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Warmistas Beffudled By 6000 Year Old Trees Found Under Melting Ice Bank in the High Mountains of Yellowstone

stock here: so this is very curious. They say the trees are well preserved, and they are all on the ground horizontal. So what “Noah Event” happened 6000 years ago, half of the major 12,000 year cycle. So it is likely that volcanoes caused the rapid cooling, but what caused them to all be knocked over, considering this species can live 1000 years.

https://www.msn.com/en-us/weather/topstories/melting-ice-reveals-remains-of-5900-year-old-trees-in-wyoming-uncovering-a-long-lost-forest/ar-BB1rob3c

A-Eye, did a quick estimate, 2F warmer at the time.

The discovery of 6,000-year-old trees found under melting ice at 10,140 feet above sea level, above the current tree line, suggests that the climate in that region was significantly warmer in the past. Let’s explore how much warmer it might have been based on the relationship between tree line elevation and temperature:

  1. Relationship Between Tree Line and Temperature

The tree line is largely determined by average summer temperatures. For trees to grow:

The mean summer temperature must typically be at least 10°C (50°F) or higher.

In high-elevation environments:

The tree line rises or falls by about 100 meters (328 feet) for every 0.6°C (1°F) change in mean annual temperature.
For this case: The ancient trees are 590 feet (approximately 180 meters) higher than the current tree line.
  1. Temperature Difference Estimate

Using the rule of thumb that the tree line changes by 0.6°C per 100 meters:

180 meters (590 feet) increase in tree line corresponds to:
ΔT=180 meters×0.6∘C100 meters=1.08∘C
ΔT=180meters×100meters0.6∘C​=1.08∘C
    This means the region was likely 1.0–1.1°C (1.8–2°F) warmer during the time these trees grew.
  1. What This Tells Us About the Past Climate The warmer conditions allowed trees to thrive at elevations that are now inhospitable due to colder temperatures.
    This aligns with the Holocene Climatic Optimum (roughly 9,000 to 5,000 years ago):
    A period when global temperatures were slightly warmer than today, especially in the Northern Hemisphere.
    Changes in Earth’s orbital patterns (Milankovitch cycles) and reduced ice cover likely contributed to these warmer conditions.
  2. Implications of This Discovery Localized Warming: While the global temperature difference during the Holocene Climatic Optimum is estimated to be only about 0.5–1°C, high-altitude regions like this one may have experienced more pronounced warming due to regional climate dynamics.
    Ecological Shifts: The higher tree line indicates a significant shift in ecosystems, suggesting that the region supported vegetation and perhaps wildlife that are now found at lower elevations.
  3. Could It Happen Again? If modern warming trends continue, the tree line is expected to rise again in many regions. However, the melting ice exposing these trees also indicates rapid glacial retreat, which has far-reaching consequences for water supplies and ecosystems.

Conclusion

Based on the elevation difference of 590 feet and the tree line-temperature relationship, the region was likely around 1°C warmer than today when the trees were alive. This aligns with the Holocene Climatic Optimum, when Earth’s climate was warmer due to natural factors.

Would you like to dive deeper into the factors behind the Holocene warming or modern tree line changes?

—————————————————— A-Eye Volcanoes

  1. Kikai Caldera, Japan (circa 5350 BC) Eruption: Known as the Akahoya eruption, this event is estimated to have been a VEI-7, making it one of the largest eruptions in the Holocene. Impact: The eruption produced approximately 80–100 km³ of tephra, leading to significant climatic effects and contributing to the formation of the present-day Kikai Caldera.
  2. Mount Aniakchak, Alaska Peninsula (circa 5250 BC ±1000 years) Eruption: This eruption is classified as a VEI-6, indicating a colossal explosive event. Impact: It expelled between 10 to 50 km³ of tephra, significantly altering the local landscape and affecting regional climates.
  3. Cerro Hudson, Southern Chile (circa 4750 BC) Eruption: This event reached a VEI-6, marking it as a major volcanic eruption. Impact: The eruption released approximately 18 km³ of tephra, influencing both the environment and human populations in the region.
  4. Macauley Island, Kermadec Islands, New Zealand (circa 4360 BC ±200 years) Eruption: This eruption is estimated to have been a VEI-6, indicating a significant explosive event. Impact: It produced a substantial volume of tephra, estimated around 100 km³, affecting the surrounding marine and atmospheric environments.
  5. Masaya Volcano, Nicaragua (circa 4050 BC) Eruption: This event reached a VEI-6, signifying a major explosive eruption. Impact: The eruption released more than 13 km³ of tephra, impacting local ecosystems and human settlements.
  6. Pago, New Britain (circa 4000 BC ±200 years) Eruption: This eruption is estimated to have been a VEI-6, indicating a significant explosive event. Impact: It produced a substantial volume of tephra, estimated around 10 km³, affecting the local environment and climate.

These eruptions had profound impacts on the climate, environment, and human societies of their time. The large volumes of volcanic ash and gases released into the atmosphere could have led to short-term climatic cooling, known as volcanic winters, and widespread ecological disruptions.

Note: The dates and tephra volumes mentioned are based on geological estimates and may have uncertainties.

  1. Kikai Caldera, Japan (circa 5350 BC) Eruption: Known as the Akahoya eruption, this event is estimated to have been a VEI-7, making it one of the largest eruptions in the Holocene. Impact: The eruption produced approximately 80–100 km³ of tephra, leading to significant climatic effects and contributing to the formation of the present-day Kikai Caldera.
  2. Mount Aniakchak, Alaska Peninsula (circa 5250 BC ±1000 years) Eruption: This eruption is classified as a VEI-6, indicating a colossal explosive event. Impact: It expelled between 10 to 50 km³ of tephra, significantly altering the local landscape and affecting regional climates.
  3. Cerro Hudson, Southern Chile (circa 4750 BC) Eruption: This event reached a VEI-6, marking it as a major volcanic eruption. Impact: The eruption released approximately 18 km³ of tephra, influencing both the environment and human populations in the region.
  4. Macauley Island, Kermadec Islands, New Zealand (circa 4360 BC ±200 years) Eruption: This eruption is estimated to have been a VEI-6, indicating a significant explosive event. Impact: It produced a substantial volume of tephra, estimated around 100 km³, affecting the surrounding marine and atmospheric environments.
  5. Masaya Volcano, Nicaragua (circa 4050 BC) Eruption: This event reached a VEI-6, signifying a major explosive eruption. Impact: The eruption released more than 13 km³ of tephra, impacting local ecosystems and human settlements.
  6. Pago, New Britain (circa 4000 BC ±200 years) Eruption: This eruption is estimated to have been a VEI-6, indicating a significant explosive event. Impact: It produced a substantial volume of tephra, estimated around 10 km³, affecting the local environment and climate.

These eruptions had profound impacts on the climate, environment, and human societies of their time. The large volumes of volcanic ash and gases released into the atmosphere could have led to short-term climatic cooling, known as volcanic winters, and widespread ecological disruptions.

Note: The dates and tephra volumes mentioned are based on geological estimates and may have uncertainties.

One reply on “Warmistas Beffudled By 6000 Year Old Trees Found Under Melting Ice Bank in the High Mountains of Yellowstone”

The pole shift rap, the Noah Event,
etc.— Ben Davidson citing Velikovsky
and other data, says these forests were
at much different latitude than today.
Catastrophes from Solar Blasts caused
Instantaneously melted ice, tremendous
movements of seawater across continents, and then the yin-yang cycle
bringing the re-freezing, on top of them
Yellowstone trees. Too bad for us all,
that academic liars, working for the mob, will still push stupid dogmas.
So A-Eye needs some solar astronomy
and history and Velikovsky entered into
Its thinking, electric universe theory,
World cultures reporting their Real experiences without some gangster
Church repressing their truths.
Mark Biltz— El Shaddai on YouTube.
War with Amalek- written in the stars.

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