logo
#

Latest news with #GRAIL

GRAIL Announces Inducement Grants Under NASDAQ Listing Rule 5635(c)(4)
GRAIL Announces Inducement Grants Under NASDAQ Listing Rule 5635(c)(4)

Yahoo

time6 days ago

  • Business
  • Yahoo

GRAIL Announces Inducement Grants Under NASDAQ Listing Rule 5635(c)(4)

MENLO PARK, Calif., May 30, 2025 /PRNewswire/ -- GRAIL, Inc. (Nasdaq: GRAL), a healthcare company whose mission is to detect cancer early when it can be cured, today announced that it has granted equity awards in the form of restricted stock units ("RSUs") underlying an aggregate of 77,350 shares of GRAIL's common stock to 38 recently hired non-executive employees as an inducement material to their acceptance of employment with GRAIL. The employment inducement awards were granted under GRAIL's Inducement Equity Incentive Plan and related form of restricted stock award agreement in accordance with Nasdaq Listing Rule 5635(c)(4). The inducement plan is used exclusively for the grant of equity awards to individuals who were not previously employees of GRAIL, or following a bona fide period of non-employment, as an inducement material to such individuals entering into employment with GRAIL, pursuant to Nasdaq Listing Rule 5635(c)(4). The RSUs vest over an approximately four year period, with 25% of the award vesting May 31, 2026, and on each one year anniversary of those respective dates thereafter, subject to continued employment with GRAIL (or any successor to or subsidiary of the Company) through the vesting dates. About GRAILGRAIL is a healthcare company whose mission is to detect cancer early, when it can be cured. GRAIL is focused on alleviating the global burden of cancer by using the power of next-generation sequencing, population-scale clinical studies, and state-of-the-art machine learning, software, and automation to detect and identify multiple deadly cancer types in earlier stages. GRAIL's targeted methylation-based platform can support the continuum of care for screening and precision oncology, including multi-cancer early detection in symptomatic patients, risk stratification, minimal residual disease detection, biomarker subtyping, treatment and recurrence monitoring. GRAIL is headquartered in Menlo Park, CA with locations in Washington, D.C., North Carolina, and the United Kingdom. For more information, visit View original content to download multimedia: SOURCE GRAIL, Inc.

Why do the two sides of the moon look different?
Why do the two sides of the moon look different?

The Hindu

time24-05-2025

  • Science
  • The Hindu

Why do the two sides of the moon look different?

The earth's moon is tidally locked: one side always faces the earth and the other side always faces away. So when scientists got their first look of the moon's far side, they were surprised to find it looked very different from the near side. NASA's GRAIL mission recently reported small month-on-month changes in the moon's gravity caused by tides on the earth. When mission scientists processed the data, they found evidence that the moon's interior is not uniform: the near side seemed to be warmer, softer, and slightly molten. The researchers predicted a temperature difference of 100-200° C between the hemispheres. Because warmer rock melts more easily, their models suggested there is still a partly molten layer of rock 800-1,250 km beneath the near side surface. Long ago, this layer could have risen to the surface and erupted to form dark lava plains that dominate the near side. As the interior slowly cooled, the eruptions would have faded 3-4 billion years ago. The moon's far side crust is thicker, so the magma may never have made it to the surface there. The findings join others — like meteorites being shielded by the earth on the near side, an uneven distribution of radioactive materials, and quirks in the moon's ancient formation event — to understand why the earth's closest cosmic companion is also Janus-faced.

Stock Market News for May 23, 2025
Stock Market News for May 23, 2025

Yahoo

time23-05-2025

  • Business
  • Yahoo

Stock Market News for May 23, 2025

U.S. stocks markets closed mixed after a choppy session. Market participants remained concerned that the proposed tax-cut bill of President Trump will further worsen U.S. fiscal deficit. Spike in yields of long-dated U.S. sovereign bonds also unnerved investors. The Dow and the S&P 500 ended in negative territory while the Nasdaq Composite managed to finished in positive zone. The Dow Jones Industrial Average (DJI) fell 1.35 points to close at 41,859.09. Notably, 15 components of the 30-stock index ended in negative territory and 15 finished in positive zone. The tech-heavy Nasdaq Composite finished at 18,925.73, gaining 0.3% due to strong performance of technology bigwigs. However, the major gainer of the tech-laden index was GRAIL Inc. GRAL. The stock price of the biotech firm was up 3.5%. GRAIL currently carry a Zacks Rank #3 (Hold). You can see the complete list of today's Zacks #1 Rank (Strong Buy) stocks here. The S&P 500 was down 2.6 points to finish at 5,842.01. Nine broad sectors of the broad-market index ended in negative territory while two in positive zone. The Consumer Discretionary Select Sector SPDR (XLY) rose 0.4% while the Health Care Select Sector SPDR (XLV) fell 0.8%. The fear-gauge CBOE Volatility Index (VIX) was down 2.8% to 20.28. A total of 16.09 billion shares were traded on Thursday, lower than the last 20-session average of 17.56 billion. The S&P 500 posted four new 52-week highs and nine new 52-week lows while the Nasdaq Composite recorded 49 new 52-week highs and 109 new 52-week lows. Yields on long-dated U.S. government securities spiked after republican-controlled House passed the state and local taxes (SALT) bill of the Trump administration on a water-thin majority. The 2017 Republican tax bill capped SALT deductions at $10,000 and the current tax bill has raised the limit to $40,000. Earlier, House republicans from Democrat-controlled states raised questions on the tax deduction allowed for SALT on federal income tax returns. A rough estimate has shown that the proposed tax cut will generate around $3.8 trillion extra burden on the U.S. government exchequer. The United States is currently facing a gigantic $36.2 trillion fiscal deficit. Given the concerns of the U.S. fiscal prudence, on May 21, the auction for 20-Year U.S. Treasury Notes had a lackluster demand from investors. Market participants shorted long-dated government securities. As a result, yield on the 30-Year U.S. Treasury Note last traded around 5.161%, touching the highest level going back to October 2023. Similarly, the yield on the benchmark 10-Year U.S. Treasury Note spiked to 4.59%, its highest level since mid-February. On May 16, Moody's Investor Services downgraded the U.S. sovereign credit rating by one notch to Aa1 from Aaa. Moody's is the third major rating agency after the S&P 500 Global and Fitch to downgrade the U.S. sovereign credit rating. The rating agency cited the growing burden of financing the federal government's outstanding budget deficit of a mammoth $36.2 trillion and the rising cost of rolling over existing debt under the high-interest rate regime. The Department of Labor reported that initial claims decreased 2,000 to 227,000 for the week ended May 17, lower-than the consensus estimate of 230,000. Continuing claims (those who have already received government aids and reported a week behind) increased 36,000 to 1.903 million. Previous week's data was revised downward by 14,000 to 1.867 million. The National Association of REALTORS reported that existing home sales in April came in at 4 million units compared with the consensus estimate of 4.18 million and March's metric of 4.02 million units. Want the latest recommendations from Zacks Investment Research? Today, you can download 7 Best Stocks for the Next 30 Days. Click to get this free report GRAIL, Inc. (GRAL) : Free Stock Analysis Report This article originally published on Zacks Investment Research ( Zacks Investment Research

NASA study reveals why the moon look so different on each side
NASA study reveals why the moon look so different on each side

Time of India

time16-05-2025

  • Science
  • Time of India

NASA study reveals why the moon look so different on each side

NASA study reveals why the moon look so different on each side The moon, Earth's only natural satellite, has been a source of fascination for centuries, not just for its mesmerizing phases but also for the stark differences between its two sides. While the side that faces Earth, known as the nearside, is characterized by vast, dark plains called "mare," the far side is marked by rugged, heavily cratered terrain. This striking asymmetry has puzzled scientists for decades. Now, an in-depth study using data from NASA 's Gravity Recovery and Interior Laboratory (GRAIL) mission is providing new clues about why the moon's two hemispheres look so different. The findings, published in the journal Nature, shed light on the moon's internal structure, revealing significant differences between its nearside and farside that are deeply linked to its volcanic past and gravitational interactions with Earth. Understanding the GRAIL mission and its significance NASA's GRAIL mission, launched in 2011, consisted of two robotic spacecraft, Ebb and Flow, which orbited the moon to create the most detailed gravitational map of the lunar surface to date. The mission's primary goal was to measure variations in the moon's gravitational field, providing critical insights into its internal structure and geological history. by Taboola by Taboola Sponsored Links Sponsored Links Promoted Links Promoted Links You May Like ثلاجات غير مباعة متاحة الآن – انقر وشاهد الأسعار! ثلاجات | إعلانات البحث ابحث الآن Undo The GRAIL mission achieved this by precisely measuring the distance between the two spacecraft as they orbited the moon. Even tiny changes in this distance, caused by variations in the moon's gravitational pull, provided data about the moon's interior composition, crust thickness, and subsurface anomalies. This approach has proven crucial for understanding the forces that shaped the moon's contrasting hemispheres. Why the two sides of the moon are so different 1. Tidal deformation and gravitational asymmetry One of the key findings from the GRAIL mission is that the moon's interior is not uniform. Researchers discovered that the lunar nearside flexes slightly more than the farside during its elliptical orbit around Earth, a phenomenon known as tidal deformation. This difference in flexibility is primarily driven by Earth's gravitational pull, which exerts a greater influence on the side facing our planet. Ryan Park, the study's lead author and supervisor of the Solar System Dynamics Group at NASA's Jet Propulsion Laboratory, explained, 'Our study shows that the moon's interior is not uniform: the side facing Earth - the nearside - is warmer and more geologically active deep down than the farside.' This increased flexibility suggests that the lunar nearside has a significantly different internal structure, which likely played a role in its distinct surface features. 2. Volcanic activity and heat distribution The study also confirmed a long-standing theory that the moon's nearside was once more volcanically active than the farside. Billions of years ago, intense volcanic activity on the nearside led to the formation of vast plains of basaltic rock, which are still visible today as the dark regions known as "mare." In contrast, the farside is covered with lighter, older crust that has remained largely untouched by large-scale volcanic processes. According to the research, this volcanic activity concentrated heat-producing, radioactive elements like thorium and titanium in the nearside mantle, resulting in a significant temperature difference between the two hemispheres. The nearside mantle is estimated to be about 180-360 degrees Fahrenheit (100-200 degrees Celsius) hotter than the farside mantle, creating a long-term thermal imbalance that has shaped the moon's geology over billions of years. 3. Crustal thickness and surface composition Another major factor contributing to the moon's asymmetry is the difference in crustal thickness between the two sides. The GRAIL data revealed that the nearside crust is significantly thinner than the farside crust, allowing magma from the moon's interior to more easily reach the surface in the past, leading to extensive lava flows. This difference in crustal thickness likely explains why the nearside has large, flat plains while the farside remains rugged and heavily cratered. The thinner nearside crust also contributed to the accumulation of radioactive, heat-producing elements, further enhancing the thermal imbalance between the two hemispheres. Implications for lunar exploration and future missions The findings from the GRAIL mission have far-reaching implications for future lunar exploration. Understanding the moon's internal structure is critical for developing accurate lunar positioning, navigation, and timing (PNT) systems, which will be essential for the success of future crewed missions to the moon and beyond. Additionally, the methods used in this study to map the moon's gravitational field could be applied to other celestial bodies, such as Saturn's moon Enceladus and Jupiter's moon Ganymede, both of which are considered potential candidates in the search for extraterrestrial life. Connecting lunar findings to Earth's stability Beyond its scientific interest, the moon plays a vital role in stabilizing Earth's rotation and generating ocean tides, which have shaped the evolution of life on our planet. Understanding the moon's internal dynamics and geological history not only deepens our knowledge of our closest neighbor but also provides insights into the early solar system and the forces that shaped it. As Park noted, 'Our knowledge of the moon has expanded through human and robotic missions that have revealed details about its surface and interior, yet many questions about its deep structure and history remain.' This continued exploration promises to uncover more secrets about the moon's complex geological past and its ongoing influence on Earth. Also read | NASA fired the employee they once celebrated, then tried to erase her story — here's who she is

Nasa study reveals deep-seated reason moon's two faces look so different
Nasa study reveals deep-seated reason moon's two faces look so different

Malay Mail

time15-05-2025

  • Science
  • Malay Mail

Nasa study reveals deep-seated reason moon's two faces look so different

WASHINGTON, May 16 — An exhaustive examination of lunar gravity using data obtained by two Nasa robotic spacecraft is offering new clues about why the two sides of the moon — the one perpetually facing Earth and the other always facing away — look so different. The data from the US space agency's Grail, or Gravity Recovery and Interior Laboratory, mission indicates that the moon's deep interior has an asymmetrical structure, apparently caused by intense volcanism on its nearside billions of years ago that helped shape its surface features. The researchers discovered that the lunar nearside flexes slightly more than the farside during its elliptical orbit around Earth thanks to our planet's gravitational influence — a process called tidal deformation. This indicates differences in the two sides of the lunar interior, they said, specifically in the geological layer called the mantle. 'Our study shows that the moon's interior is not uniform: the side facing Earth — the nearside — is warmer and more geologically active deep down than the farside,' said Ryan Park, supervisor of the Solar System Dynamics Group at Nasa's Jet Propulsion Laboratory in California and lead author of the study published on Wednesday in the journal Nature. The moon's nearside is covered by vast plains, called mare, formed from molten rock that cooled and solidified billions of years ago. Its farside has much more rugged terrain, with few plains. Some scientists have hypothesized that intense volcanism within the nearside that caused radioactive, heat-generating elements to accumulate on that side of the mantle drove the surface differences observed today. The new findings offer the strongest evidence yet to support this notion. The researchers estimated that the nearside mantle on average is about 100°-200°Celsius hotter than the farside, with the thermal difference perhaps sustained by radioactive decay of the elements thorium and titanium on the nearside. 'The moon's nearside and farside look very different, as shown by differences in topography, crustal thickness and the amount of heat-producing elements inside,' Park said. The moon's diameter of about 3,475 km is a bit more than a quarter of Earth's diameter. The lunar mantle is the layer located beneath the crust and above the core, spanning a depth about 35-1,400 km under the surface. The mantle makes up roughly 80 per cent of the moon's mass and volume and is composed mostly of the minerals olivine and pyroxene, similar to Earth's mantle. 'The fact that the detected asymmetry in the mantle matches the pattern of the surface geology — for instance, differences in the abundance of the approximately 3-4 billion-year-old mare basalts (volcanic rock) between the nearside and the farside — suggests that processes which drove ancient lunar volcanism are active today,' said Caltech computational planetary scientist and study co-author Alex Berne, affiliated with the Jet Propulsion Laboratory working on the design of gravity sensors for missions to the outer solar system. The researchers spent years analyzing data from Grail's Ebb and Flow spacecraft, which orbited the moon from December 2011 to December 2012. 'Our study delivers the most detailed and accurate gravitational map of the moon to date,' Park said. 'This enhanced gravity map is a critical foundation for developing lunar Positioning, Navigation and Timing (PNT) systems, which are essential for the success of future lunar exploration missions. By improving our understanding of the moon's gravity field, it contributes to establishing a precise lunar reference frame and time system, enabling safer and more reliable navigation for spacecraft and surface operations,' Park added. The same approach employed here using gravity data to assess the lunar interior, the researchers said, could be applied to other bodies in the solar system such as Saturn's moon Enceladus and Jupiter's moon Ganymede, two worlds of interest in the search for potential life beyond Earth. In the meantime, the new findings add to the understanding of Earth's eternal companion. 'The moon plays a vital role in stabilizing Earth's rotation and generating ocean tides, which influence natural systems and daily rhythms,' Park said. 'Our knowledge of the moon has expanded through human and robotic missions that have revealed details about its surface and interior, yet many questions about its deep structure and history remain. As our closest neighbor, the moon continues to be an important focus of scientific discovery.' — Reuters

DOWNLOAD THE APP

Get Started Now: Download the App

Ready to dive into the world of global news and events? Download our app today from your preferred app store and start exploring.
app-storeplay-store